the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
| 04 Jun 2025
Detecting the occurrence of preferential flow in soils with stable water isotopes
Abstract. Subsurface flow in preferential pathways in soils may transport water more rapidly than the soil matrix, which may be quickly activated during precipitation events and enhancing infiltration or interflow. Vertical pathways are particularly important for runoff generation. However, identifying these pathways is challenging because traditional methods such as piezometers, soil moisture sensors, or hillslope trenches do not adequately capture the spatial scale and frequency of prefer ential flow features, while other experimental techniques like dye tracing are labor-intensive and invasive. In this study, we introduce a novel method to identify the locations of preferential flow by analysing vertical soil profiles of stable water isotope. Across four catchments, we drilled 100 soil cores (1–3 m deep) per catchment and analyzed the stable isotope composition of the soil water in 10–20 cm depth intervals to construct depth profiles. We employed clustering techniques to group soil-water isotope profiles and selecting those that match to a seasonal sampling date to establish a reference profile for each catchment using LOESS regression, representing profiles influenced solely by matrix infiltration. Deviations from these reference profiles were then used as indicators of being influenced by vertical or lateral preferential flow. Our results revealed evidence of preferential flow in all studied catchments. Especially in the alpine catchment with highly heterogeneous soils many profiles showed distinct preferential flow features, including multiple, vertically independent pathways occurring at variable depths, even among adjacent profiles. These findings demonstrate the feasibility of using soil water isotope profiles to assess preferential flow pathways highlighting the substantial spatial and vertical variability of preferential flowpaths at hillslope and catchment scale.
Competing interests: At least one of the (co-)authors is a member of the editorial board of Hydrology and Earth System Sciences.
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- CC1: 'Comment on egusphere-2025-2411', Ryan Stewart, 09 Jul 2025
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RC1: 'Comment on egusphere-2025-2411', Ryan Stewart, 09 Jul 2025
General comments:
This manuscript describes the results of using stable water isotopes extracted from different soil depths to detect incidence of preferential flow, using data collected seasonally from four catchments in Europe. The manuscript is well-written save for some editorial suggestions listed below, and the approach is an interesting contribution. The manuscript focuses a bit more on the validation and assumptions of the approach than on the scientific contribution itself, so having a better balance with the actually scientific contribution of the work would be something to consider during the revision process.
In terms of results and interpretations, the approach appears to work best in areas with distinct seasonality in the isotopic signature of precipitation (e.g., the Alpine catchment) and operates under the assumption that water moving via preferential flow has the same isotopic signature as the topsoil. This assumption does not cover all instances of preferential flow, as discussed starting around Line 310.
The approach also relies on the assumption that there is isotopic exchange/equilibrium between mobile and bulk matrix water (Lines 321-328). Another possibility is that mobile water could still be present (but not equilibrated) within the soil at the time of sampling. Water content at the time of sampling could be a way to distinguish between these possibilities, and it could be generally instructive to present the water content data if those are available.
Another assumption (which I don’t think was discussed) is that the reference profiles were not affected by preferential flow. The authors constrain what they consider to be reference profiles based on presumed seasonality in the isotopic signature of input precipitation, but it might also be possible to use a simple plug flow calculation or something similar to perform a back-of-the-envelope verification of the approximate depths those seasonal inputs would move given an assumption of effective porosity and rainfall depth (the latter perhaps minus ET).
The manuscript also does not discuss situations in which the water at depth has a depleted isotopic signature relative to the reference profiles, even though such scenarios 1) exist in the dataset, and 2) may reveal interesting behaviors about subsurface flow.
With some revision the paper is a good candidate for publication in HESS.
Specific comments:
Line 2-16: Some minor grammatical issues here: 1) “may be quickly activated” sounds like it is referring to the soil matrix, 2) “and enhance infiltration or interflow”; 3) “profiles of stable water isotopes”; 4) “and selected those that matched…” 5) “heterogenous soils, many profiles”; 6) “flow pathways and highlight the…”; 7) “hillslope and catchment scales”.
Line 19: “water flows through… rather than the surrounding…”
Line 22: This range of preferential flow (16-27%) seems very specific. Either provide the context or consider not putting these numbers.
Line 25: “understanding” may not be needed twice.
Line 38: “soil-layer, which”.
Line 46: “formed”.
Line 47: Check your references that “Glenn V.” is needed for Wilson.
Line 53: 190 m is another number that seems very specific and context-specific. Can you at least express on a relative basis or something? Otherwise it doesn’t seem transferrable.
Line 58: Why is SSF only limited to 1/3 of events? Another specific rather than universal number.
Line 60: Velocities have already been discussed in L27-28.
Line 61-65: This section could be written more concisely.
Line 85: GPR can also be used in a timelapse manner to visualize changes in water content during discrete flow events.
Line 102: no dash is needed between continent and effect.
Line 111: “making them an ideal”.
Line 130: “and reach deeper”.
Line 132: “the signatures shift”.
Line 140: This could be a place to elaborate on the validity/assumptions of deriving reference profiles from the dataset itself.
Line 163: add “for delta18O” after 1.7 per mille. Same for Line 166.
Line 216: It seems you could solve this equation explicitly for f, which may not be that important but would better illustrate the analysis.
Line 272: Interesting interpretation/context.
Figure 4: The shading for SD is faint (didn’t show up in the printed copy I made) and would benefit from lines as in Figure 6.
Line 285: Might indicate that 65 and 35% are approximate values.
Line 284: Suggest calling the variable “aspect”, not “Aspectcos”, and it indicates the direction (not just northerly).
Line 305: Seems like these two sentences could be combined. Somewhat redundant currently.
Line 317: “in both cases.”
Figure 9: Did you consider/try fitting logistic models to the individual sites? The response appears to be driven primarily by the Alps site, which makes sense as the one showing the most preferential flow, but also it is hard to see the different catchments with the points overlaid on each other.
Line 318: “thus”.
Line 334-336: The comparison of the two stable isotopes is an important point, but one that wasn’t emphasized until here near the end of the paper. It would be good to make this point early on.
Line 354-360: This paragraph is choppy in its structure and logic. I suggest rewriting.
Citation: https://doi.org/10.5194/egusphere-2025-2411-RC1 -
AC2: 'Reply on RC1', Jonas Pyschik, 25 Jul 2025
Authors’ responses to the comments of Ryan Stewart
We appreciate your review and comments on our manuscript, “Detecting the occurrence of preferential flow in soils with stable water isotopes”. Your feedback is valuable to us, and we will make the recommended revisions accordingly. We provide detailed responses to each of your comments below.
General comments:
This manuscript describes the results of using stable water isotopes extracted from different soil depths to detect incidence of preferential flow, using data collected seasonally from four catchments in Europe. The manuscript is well-written save for some editorial suggestions listed below, and the approach is an interesting contribution. The manuscript focuses a bit more on the validation and assumptions of the approach than on the scientific contribution itself, so having a better balance with the actually scientific contribution of the work would be something to consider during the revision process.
In terms of results and interpretations, the approach appears to work best in areas with distinct seasonality in the isotopic signature of precipitation (e.g., the Alpine catchment) and operates under the assumption that water moving via preferential flow has the same isotopic signature as the topsoil. This assumption does not cover all instances of preferential flow, as discussed starting around Line 310.
The approach also relies on the assumption that there is isotopic exchange/equilibrium between mobile and bulk matrix water (Lines 321-328). Another possibility is that mobile water could still be present (but not equilibrated) within the soil at the time of sampling. Water content at the time of sampling could be a way to distinguish between these possibilities, and it could be generally instructive to present the water content data if those are available.
Thank you for this suggestion. We will further discuss this in the revision, however we do not have water content data.
Another assumption (which I don’t think was discussed) is that the reference profiles were not affected by preferential flow. The authors constrain what they consider to be reference profiles based on presumed seasonality in the isotopic signature of input precipitation, but it might also be possible to use a simple plug flow calculation or something similar to perform a back-of-the-envelope verification of the approximate depths those seasonal inputs would move given an assumption of effective porosity and rainfall depth (the latter perhaps minus ET).
Unfortunately, we lack the precipitation data of the year previous to drilling at those locations. Our approach aimed at filling this data gap with the reference profiles. We will make this clearer in the revision, that the reference profile creation was due to lacking isotope values in the rainfall.
The manuscript also does not discuss situations in which the water at depth has a depleted isotopic signature relative to the reference profiles, even though such scenarios 1) exist in the dataset, and 2) may reveal interesting behaviors about subsurface flow.
Yes, those instances are sometimes found in the data, however this was a really minor case. It might be that “older” winter water was transported there, but since we are not able to assess the origin of the signature (as it is not within the topsoil reference profile), we are unable to say which flow process transported it there.
With some revision the paper is a good candidate for publication in HESS.
Specific comments:
Line 2-16: Some minor grammatical issues here: 1) “may be quickly activated” sounds like it is referring to the soil matrix, 2) “and enhance infiltration or interflow”; 3) “profiles of stable water isotopes”; 4) “and selected those that matched…” 5) “heterogenous soils, many profiles”; 6) “flow pathways and highlight the…”; 7) “hillslope and catchment scales”.
We will fix that
Line 19: “water flows through… rather than the surrounding…”
We will change this
Line 22: This range of preferential flow (16-27%) seems very specific. Either provide the context or consider not putting these numbers.
It was stated in the publication but is indeed very specific, therefore we will remove the numbers in the revision
Line 25: “understanding” may not be needed twice.
We will rephrase
Line 38: “soil-layer, which”.
We will change that
Line 46: “formed”.
We will update the sentence
Line 47: Check your references that “Glenn V.” is needed for Wilson.
We will revise the citation to leave out the surname.
Line 53: 190 m is another number that seems very specific and context-specific. Can you at least express on a relative basis or something? Otherwise it doesn’t seem transferrable.
It was also stated in that publication but is also very specific, therefore we will remove the number in the revision
Line 58: Why is SSF only limited to 1/3 of events? Another specific rather than universal number.
We will also remove this number
Line 60: Velocities have already been discussed in L27-28.
We will remove this in the revision
Line 61-65: This section could be written more concisely.
We will try to make this more concise.
Line 85: GPR can also be used in a timelapse manner to visualize changes in water content during discrete flow events.
Thank you, we will add that
Line 102: no dash is needed between continent and effect.
We will remove this
Line 111: “making them an ideal”.
We will update the wording
Line 130: “and reach deeper”.
We will change this
Line 132: “the signatures shift”.
We will revise this
Line 140: This could be a place to elaborate on the validity/assumptions of deriving reference profiles from the dataset itself.
We will include a few sentences in the revisions where we elaborate on the validity
Line 163: add “for delta18O” after 1.7 per mille. Same for Line 166.
Yes, we missed that and will add it
Line 216: It seems you could solve this equation explicitly for f, which may not be that important but would better illustrate the analysis.
True, we will change it so it gets clearer what we are actually solving
Line 272: Interesting interpretation/context.
Thank you!
Figure 4: The shading for SD is faint (didn’t show up in the printed copy I made) and would benefit from lines as in Figure 6.
We will change it to the same style as in Figure 6
Line 285: Might indicate that 65 and 35% are approximate values.
Yes, we will add that
Line 284: Suggest calling the variable “aspect”, not “Aspectcos”, and it indicates the direction (not just northerly).
We also calculated this for Aspect (Range 0-360 degree) which discerns between east and west facing slopes, where we found no effect, and used the cos of aspect to gain a metric to discern between north and south, therefore we will keep the name but also add some explanation on this
Line 305: Seems like these two sentences could be combined. Somewhat redundant currently.
We will write this more concisely
Line 317: “in both cases.”
We will change the wording
Figure 9: Did you consider/try fitting logistic models to the individual sites? The response appears to be driven primarily by the Alps site, which makes sense as the one showing the most preferential flow, but also it is hard to see the different catchments with the points overlaid on each other.
Yes, we tried and still saw the effect, but stronger in the alps. We will add that to the revision
Line 318: “thus”.
We will change this
Line 334-336: The comparison of the two stable isotopes is an important point, but one that wasn’t emphasized until here near the end of the paper. It would be good to make this point early on.
We will shift this further up
Line 354-360: This paragraph is choppy in its structure and logic. I suggest rewriting.
We will rewrite it ensure more structure and logic.
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AC2: 'Reply on RC1', Jonas Pyschik, 25 Jul 2025
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RC2: 'Comment on egusphere-2025-2411', Inge Wiekenkamp, 13 Jul 2025
I have read the manuscript entitled “Detecting the occurrence of preferential flow in soils with stable water isotopes” written by Jonas Pyschik and Markus Weiler. In this work, they introduce a new method to identify locations where preferential flow occurs (both lateral and vertical), based on stable water isotope profiles in the soil. The core idea is to use deviations from reference profiles in the isotope signature as an indication of preferential flow occurrence.
I am confident that this paper is highly relevant and fits well within the scope of HESS, as it introduces a new method to identify preferential flow using stable water isotopes in soil profiles. It highlights the potential of isotopes as a novel tool to trace subsurface processes. Although the scientific method is clearly described, the assumptions and limitations could be discussed in more detail (see, for example, general comment B).
The paper is well-structured and demonstrates the authors’ strong expertise in both hydrological processes and isotope applications, here specifically focusing on subsurface flow. Figures are informative and visually appealing, and the dataset compiled is impressively broad. With some targeted refinements, the manuscript can be further strengthened and made even more accessible to a broader readership.
General comments:
A) Reference profile: I really like your approach, but was wondering about the following limitation. In your clustering and reference profile determination, you assume that no preferential flow is present. I can imagine that this is not always the case, because there might be particular features in some of these soils that can always facilitate preferential flow. In a way this approach means that more permanent features (facilitating preferential flow) that could be present in a lot of profiles are not indicated and present in this case. However, I can understand also that based on this average cluster profile that you create, in a way, such feature would need to be present in all the clustered profiles and at the same depth (which might be unlikely if you include a lot of different profiles and use a small number of clusters). Perhaps one could elaborate on this.
B) Discussion (1): While the discussion already touches on important opportunities and limitations, I believe it could benefit from further elaboration on a few points:
(1) Are there particular profiles, landscape types, or environmental conditions where this method is less applicable or might fail?
(2) Although the method is insightful, it still requires soil sampling, meaning that it provides a snapshot in time. How representative is this snapshot for a full season or hydrological cycle?
(3) Regarding the 2*std criterion for detecting deviations from the reference profile: could the threshold be sensitive to sampling design or the number of samples? Are the chosen limits potentially too conservative, and how might this influence the risk of false positives or false negatives?
Some of these suggestions are further elaborated in the detailed comments.C) Discussion (2) – add more on Novelty and Contribution: The manuscript presents an innovative and promising approach to identifying preferential flow in soils using stable water isotopes, which is a valuable addition to the “hydrological toolbox for preferential flow identification”. However, it would be helpful if the authors could explicitly position their method with respect to other common approaches (e.g., dye tracer studies, hydrometric techniques, geophysical methods). This contextualization could be more clearly revisited in the discussion to clarify the unique contributions and potential complementarities of this isotope-based approach.
D) Accessibility and Reproducibility: Given the method involves data clustering and isotope profile analysis, some information on data availability, reproducibility, or whether the authors will provide scripts/code for other researchers to apply this method could be valuable. Encouraging open science practices would enhance the method’s uptake and usability by the community.
E) Spatial Drivers: The spatial analysis section appears relatively brief and less extensive compared to other parts of the manuscript. This is likely constrained by the limited number of profiles where preferential flow (PF) was detected, which reduces the ability to identify clear spatial drivers. It might be helpful for the authors to acknowledge this limitation explicitly and, if possible, consider expanding the spatial analysis or discussing potential ways to improve it in future work.
Detailed comments:- Citation Wilson: For the citation of Wilson et al. (2013), the first name is included in the text and in the reference list (located in the list of authors with a G). If I see this correctly, it is even the same Wilson as the one cited for 2016 (Wilson et al., 2016). As there is no other reference to Wilson, please consider adjusting this accordingly: Glenn V. Wilson, John L. Nieber, Roy C. Sidle, and Garey A. Fox: Internal Erosion during Soil Pipeflow: State of the Science for Experimental and Numerical Analysis, Transactions of the ASABE, 56, 465–478, https://doi.org/10.13031/2013.42667, 2013.
- Citation style: I noticed that references often end with a double “))” at the end, for example here: “(Thomas et al., 2013; Demand et al., 2019a))”. Is this the style the citations are supposed to have? If not, please consider updating this accordingly.
- Introduction, Lines 51–53: “During water flow in macropores, they are typically not filled entirely with water but a water film forms along the wall if the pore, leaving the central part of the pore empty.” I think the “if the pore” sounds incorrect. Should “if” be replaced by “in”?
- Introduction: I was just curious about the connection between the following two sentences:
In Lines 21–22, authors refer to the flow in the soil:
“Preferential flow does not occur during every rainfall or infiltration event, but when it is activated, it can account for a significant proportion of annual flow through the soil, ranging from 16–27% (Eguchi and Hasegawa, 2008).”
Later, they refer to the contribution of preferential flow to discharge:
“The complex network of macropores, particularly soil pipes in hillslopes, can extend up to 190 m and can contribute up to 50% to overall discharge in streams (Jones, 2010; Wilson et al., 2016).”
I was wondering if these statements fit together or if they might mismatch. If you could also give a range for the second statement (“up to 50%”), this would maybe give a better feeling of the general importance and variability in preferential flow importance. - Introduction, statement on Ground Penetrating Radar (GPR): A period is missing at the end of the sentence. This was present for the other sentences. Also, I assume that another problem of these geophysical methods is the non-unique solution of the inversion results (imaging). This could be added and stated as a limitation of the method. Perhaps you could in this section rather refer more generally to geophysical methods that are able to characterize PF (ERT – Electrical Resistivity Tomography – is, for example, also used in multiple cases to visualize preferential flow paths), and include the limitation of non-uniqueness (underdetermined system)?
- Introduction, Lines 132–134: “Over time, however, the signatures shifts towards those of pre-event water (Leaney et al., 1993; Gehrels et al., 1998; Kelln et al., 2007) due to lateral infiltration and exchange processes between the preferential pathways and the surrounding matrix.” Please replace “shifts” with “shift”.
- Figure 1: It would be great if you could add (either in the figure or the caption) that the soil profiles are stable water isotope profiles. Perhaps the authors could also add the number of profiles to each catchment (to get a feeling for the number of points – vertical profiles – in each area). Is this always 100? Then this could also just be mentioned in the caption to give a direct feeling of the magnitude.
- Methods, 2.3, Line 197: “from the R caret package Kuhn (2008).” Probably this should be: “from the R caret package by Kuhn, 2008” (or use the bracket version: “(Kuhn, 2008)”).
- Figure 2: I like the schematic representation of the method, but I think it would help if the figure had x and y axis descriptions (not ranges, just an explanation of variables – depth on the y-axis, x-axis labeling δ²H / scaled δ¹⁸O (‰)). In the second sub-figure, the line borders of x and y axes are missing. I suggest implementing these as well.
- Methods, section 2.3: “Only depths where both δ²H and scaled 18 O values exceeded the reference range were considered for potential preferential flow (Figure 2.4).” Should “scaled 18 O” not be replaced by δ¹⁸O? Also, when referring to Figure 2.4, one could state the color of the points that are considered indicative of preferential flow (orange points, right?).
- Methods, 2.4 Mixing models: “By solving this equation, the proportion of preferential flow (f) at the identified depths was determined.” Before this sentence, a description is provided about the proportion of preferential flow. Does this implicitly mean that one could not indicate preferential flow in the topsoil with this method? Also, how would this equation work if the delta values of the topsoil and reference are very similar (could for example happen at the second sampling depth, I imagine)?
- 1 Reference profiles: In the results, the sampling periods for each region are also mentioned. This could possibly be moved to the methods section to keep more focus on the results here. I think the results are very descriptive. It would be quite nice if there was more comparison between the results. For example, to more easily compare results from different areas, one could also describe all summer results together and position the plots in Figure 3 accordingly. For instance, blue and yellow curve SL summer and BF summer curve seem to have very similar features and could be connected nicely.
- Table 1: First of all, it’s really impressive how many samples and profiles have been measured for this effort. I would suggest adjusting “Profiles with multiple PF” to “Profiles with PF at multiple depths.” I also think that the number of profiles showing PF is probably highly influenced by how you set the detection boundaries for PF. You used 2 times the standard deviation, which is a sound statistical concept, but I wonder how this connects to the process/physics – i.e., the occurrence of preferential flow in general. Keep in mind that these limits (2* std) do affect the number of locations where you will detect preferential flow heavily.
I also think the way the data is clustered can affect the outcome of your analysis substantially. I assume that if your clustered pool is larger and has more isotopic variability (at different depths), the chance that a particular profile pops up as PF will be smaller, as compared to a small group of clustered profiles with lower general variability. This means that the sampling locations chosen and the number of locations sampled might affect the output. It also means that for reference profiles with small standard deviations, smaller deviations from the mean might already lead to PF detection, whereas in the case of large variability, it might not. Perhaps this should be discussed in the discussion section as something important to keep in mind. - Figure 4: The difference between the two PF classes here is not clearly visible color-wise. If you want to distinguish them, it would probably be better to give them more distinct colors (currently both look reddish/orange). The grey background is not very visible and could be made a bit darker to more clearly show the region where samples are considered “piston flow.”
- Figure 6: Although I really like the figure, I did not find a clear reference to it in the main text. I was also not sure what the authors want to say with this plot. Why are fall plots from the TA location shown? What is the reasoning behind this arrangement? It would be great if the figure could be better integrated into the manuscript. In the caption, I also miss what the figure is trying to convey. To guide the reader more, I suggest clearly stating the purpose of the figure in the caption.
- Figure 7: I generally like the figure, but I think it’s unclear what is on the x-axis. One could choose to depict a numerical value here (e.g., number of PF profiles) or a more meaningful variable. In the text, you write: “Most samples identified as preferential flow exhibited a mixture of 65% new event water and 35% older pre-event water.” Perhaps you could show this in the graph as well (as a dotted line, for example).
- Discussion, Line 314: “However, this is not always the case.“ Remove the second period (“.”).
- Discussion, Line 302: “One disadvantage is that a sufficient number of samples are required , with more samples improving analysis quality.” Remove the space before the comma here. Regarding the number of samples: I think it is not only about the number of samples. The representativeness of the samples also really matters, especially if you generate a reference profile. What would happen if you over-sample one location and under-sample another? How would the sampling design affect the reference profile and clusters that are built?
- Figure 9: I would rephrase the caption to explain more clearly the intent. Also consider not using “Aspectcos” as a term here, but rather describing it in terms of slope direction. I’m not 100% sure about the absolute magnitude of the regression slope in the graph (as it does not reach “Flowpaths identified,” but rather stays close to “No Flowpaths”). I assume it relates to the probability of PF (between 0 and 1)? Does this not mean that, in general, the probability of detecting PF is lower than not detecting it—which may also be related to the fact that your sampling design includes many more “no PF” samples? How does your sampling distribution here affect your analysis?
- Discussion Section 3.4: I think this section could benefit from more detailed interpretation. I found it quite short and was thinking that some things could be explained (e.g., more on preferential flow from a catchment perspective). In general, I also wondered whether one could really draw strong conclusions about site-specific characteristics, given that the number of profiles where PF was detected was generally quite small. In TA, there are many detections, but in some other catchments, only 2 or 6 cases. This also relates to Figure 8 and 9.
- Connection between Introduction (Lines 64–68), Introduction and Discussion: In the introduction, the authors mention that one of the complications of preferential flow detection is that field observations are just a snapshot:
“Also, field surveys are only a snapshot of an environmental system, but flowpath arrangements can change completely within one year (Wessolek et al., 2009; Beven, 2019). Additionally, even when preferential flow features are successfully identified at the plot scale, these findings cannot be easily extrapolated to the whole catchment.”
To what degree do you think this applies to your newly proposed method? Are the profiles you take not also a snapshot of the preferential flow pathways? What kind of temporal sampling or general sampling design would be needed to get a statistically sound idea of preferential flow occurrence at a particular site, rather than just a snapshot. - Conclusion: I think the conclusion in this case would particularly benefit from a clear summary of pros and cons of this new methods. Currently the summary might not be fully accessible to people that have not read other parts of the manuscript. I always think it is a good opportunity to do this, as this would help to also guide readers that might just look at the conclusions really quick – this is helping readers quickly grasp the method’s utility and potential challenges.
Citation: https://doi.org/10.5194/egusphere-2025-2411-RC2 -
AC1: 'Reply on RC2', Jonas Pyschik, 25 Jul 2025
Authors’ responses to the comments of Inge Wiekenkamp
We appreciate your review and comments on our manuscript, “Detecting the occurrence of preferential flow in soils with stable water isotopes”. Your feedback is valuable to us, and we will make the recommended revisions accordingly. We provide detailed responses to each of your comments below.
I have read the manuscript entitled “Detecting the occurrence of preferential flow in soils with stable water isotopes” written by Jonas Pyschik and Markus Weiler. In this work, they introduce a new method to identify locations where preferential flow occurs (both lateral and vertical), based on stable water isotope profiles in the soil. The core idea is to use deviations from reference profiles in the isotope signature as an indication of preferential flow occurrence.
I am confident that this paper is highly relevant and fits well within the scope of HESS, as it introduces a new method to identify preferential flow using stable water isotopes in soil profiles. It highlights the potential of isotopes as a novel tool to trace subsurface processes. Although the scientific method is clearly described, the assumptions and limitations could be discussed in more detail (see, for example, general comment B).
The paper is well-structured and demonstrates the authors’ strong expertise in both hydrological processes and isotope applications, here specifically focusing on subsurface flow. Figures are informative and visually appealing, and the dataset compiled is impressively broad. With some targeted refinements, the manuscript can be further strengthened and made even more accessible to a broader readership.
Thank you!
General comments:
A) Reference profile: I really like your approach, but was wondering about the following limitation. In your clustering and reference profile determination, you assume that no preferential flow is present. I can imagine that this is not always the case, because there might be particular features in some of these soils that can always facilitate preferential flow. In a way this approach means that more permanent features (facilitating preferential flow) that could be present in a lot of profiles are not indicated and present in this case. However, I can understand also that based on this average cluster profile that you create, in a way, such feature would need to be present in all the clustered profiles and at the same depth (which might be unlikely if you include a lot of different profiles and use a small number of clusters). Perhaps one could elaborate on this.
This is partially correct and we can further elaborate on this in the revision. There may be preferential flow features persistent in many profiles. However, our first step in defining reference profiles is fitting a 3rd order polynomial function through the points, which discards single outliers which are typical for preferential flow effects. However, if for instance all hillslope would laterally transports water preferentially and similar depths are influenced, then even the polynomial lines would be skewed. However, we consider this highly unlikely. But we can certainly provide some more background on our assumptions.
B) Discussion (1): While the discussion already touches on important opportunities and limitations, I believe it could benefit from further elaboration on a few points:
(1) Are there particular profiles, landscape types, or environmental conditions where this method is less applicable or might fail?We will add something on that in the revision
(2) Although the method is insightful, it still requires soil sampling, meaning that it provides a snapshot in time. How representative is this snapshot for a full season or hydrological cycle?True, it is only a snapshot. We will elaborate on this in the revision. As preferential flow features are not always active, this can definitely only be seen as a short time assessment. However, some features, like the ones shown in the alpine hillslope which seem to be interconnected are probably more persistent. In future studies, multiple sampling at different times in the year could help to tackle the questions.
(3) Regarding the 2*std criterion for detecting deviations from the reference profile: could the threshold be sensitive to sampling design or the number of samples? Are the chosen limits potentially too conservative, and how might this influence the risk of false positives or false negatives?The limits are really strict and using for instance only 1*sd we get way more preferential flowpaths identified, but also a higher probability for false positives. We will include this in the discussion.
Some of these suggestions are further elaborated in the detailed comments.- C) Discussion (2) – add more on Novelty and Contribution: The manuscript presents an innovative and promising approach to identifying preferential flow in soils using stable water isotopes, which is a valuable addition to the “hydrological toolbox for preferential flow identification”. However, it would be helpful if the authors could explicitly position their method with respect to other common approaches (e.g., dye tracer studies, hydrometric techniques, geophysical methods). This contextualization could be more clearly revisited in the discussion to clarify the unique contributions and potential complementarities of this isotope-based approach.
We will clarify the unique contributions and potential complementarities of our approach in the discussion.
D) Accessibility and Reproducibility: Given the method involves data clustering and isotope profile analysis, some information on data availability, reproducibility, or whether the authors will provide scripts/code for other researchers to apply this method could be valuable. Encouraging open science practices would enhance the method’s uptake and usability by the community.
We will add the code to reproduce the findings. The data will be made available in a separate data paper including a wider variety of isotope data of the catchment in the following months.
E) Spatial Drivers: The spatial analysis section appears relatively brief and less extensive compared to other parts of the manuscript. This is likely constrained by the limited number of profiles where preferential flow (PF) was detected, which reduces the ability to identify clear spatial drivers. It might be helpful for the authors to acknowledge this limitation explicitly and, if possible, consider expanding the spatial analysis or discussing potential ways to improve it in future work.
We will elaborate on the limited spatial analysis due to limited identified preferential flow profiles
Detailed comments:
- Citation Wilson: For the citation of Wilson et al. (2013), the first name is included in the text and in the reference list (located in the list of authors with a G). If I see this correctly, it is even the same Wilson as the one cited for 2016 (Wilson et al., 2016). As there is no other reference to Wilson, please consider adjusting this accordingly: Glenn V. Wilson, John L. Nieber, Roy C. Sidle, and Garey A. Fox: Internal Erosion during Soil Pipeflow: State of the Science for Experimental and Numerical Analysis, Transactions of the ASABE, 56, 465–478, https://doi.org/10.13031/2013.42667, 2013.
We will fix the citation - Citation style: I noticed that references often end with a double “))” at the end, for example here: “(Thomas et al., 2013; Demand et al., 2019a))”. Is this the style the citations are supposed to have? If not, please consider updating this accordingly.
We will correct that error - Introduction, Lines 51–53: “During water flow in macropores, they are typically not filled entirely with water but a water film forms along the wall if the pore, leaving the central part of the pore empty.” I think the “if the pore” sounds incorrect. Should “if” be replaced by “in”?
We will change the wording - Introduction: I was just curious about the connection between the following two sentences:
In Lines 21–22, authors refer to the flow in the soil:
“Preferential flow does not occur during every rainfall or infiltration event, but when it is activated, it can account for a significant proportion of annual flow through the soil, ranging from 16–27% (Eguchi and Hasegawa, 2008).”
Later, they refer to the contribution of preferential flow to discharge:
“The complex network of macropores, particularly soil pipes in hillslopes, can extend up to 190 m and can contribute up to 50% to overall discharge in streams (Jones, 2010; Wilson et al., 2016).”
I was wondering if these statements fit together or if they might mismatch. If you could also give a range for the second statement (“up to 50%”), this would maybe give a better feeling of the general importance and variability in preferential flow importance.
In line with the Review by Ryan Stewart we will fully remove these numbers. - Introduction, statement on Ground Penetrating Radar (GPR): A period is missing at the end of the sentence. This was present for the other sentences. Also, I assume that another problem of these geophysical methods is the non-unique solution of the inversion results (imaging). This could be added and stated as a limitation of the method. Perhaps you could in this section rather refer more generally to geophysical methods that are able to characterize PF (ERT – Electrical Resistivity Tomography – is, for example, also used in multiple cases to visualize preferential flow paths), and include the limitation of non-uniqueness (underdetermined system)?
We will fix the period errors and state this limitation - Introduction, Lines 132–134: “Over time, however, the signatures shifts towards those of pre-event water (Leaney et al., 1993; Gehrels et al., 1998; Kelln et al., 2007) due to lateral infiltration and exchange processes between the preferential pathways and the surrounding matrix.” Please replace “shifts” with “shift”.
We will fix that - Figure 1: It would be great if you could add (either in the figure or the caption) that the soil profiles are stable water isotope profiles. Perhaps the authors could also add the number of profiles to each catchment (to get a feeling for the number of points – vertical profiles – in each area). Is this always 100? Then this could also just be mentioned in the caption to give a direct feeling of the magnitude.
We will add that to the figure caption and map - Methods, 2.3, Line 197: “from the R caret package Kuhn (2008).” Probably this should be: “from the R caret package by Kuhn, 2008” (or use the bracket version: “(Kuhn, 2008)”).
We will change that - Figure 2: I like the schematic representation of the method, but I think it would help if the figure had x and y axis descriptions (not ranges, just an explanation of variables – depth on the y-axis, x-axis labeling δ²H / scaled δ¹⁸O (‰)). In the second sub-figure, the line borders of x and y axes are missing. I suggest implementing these as well.
We will try to include this while still keeping the graphic concise - Methods, section 2.3: “Only depths where both δ²H and scaled 18 O values exceeded the reference range were considered for potential preferential flow (Figure 2.4).” Should “scaled 18 O” not be replaced by δ¹⁸O? Also, when referring to Figure 2.4, one could state the color of the points that are considered indicative of preferential flow (orange points, right?).
We will add that and revise - Methods, 2.4 Mixing models: “By solving this equation, the proportion of preferential flow (f) at the identified depths was determined.” Before this sentence, a description is provided about the proportion of preferential flow. Does this implicitly mean that one could not indicate preferential flow in the topsoil with this method? Also, how would this equation work if the delta values of the topsoil and reference are very similar (could for example happen at the second sampling depth, I imagine)?
We always exclude the two topsoil signatures as these data ranges are what we use to identify preferential flow. We would always get 100% event water in those zones. - 1 Reference profiles: In the results, the sampling periods for each region are also mentioned. This could possibly be moved to the methods section to keep more focus on the results here. I think the results are very descriptive. It would be quite nice if there was more comparison between the results. For example, to more easily compare results from different areas, one could also describe all summer results together and position the plots in Figure 3 accordingly. For instance, blue and yellow curve SL summer and BF summer curve seem to have very similar features and could be connected nicely.
We will try to find a way to arrange the graphics this differently and also add some comparative sentences - Table 1: First of all, it’s really impressive how many samples and profiles have been measured for this effort. I would suggest adjusting “Profiles with multiple PF” to “Profiles with PF at multiple depths.” I also think that the number of profiles showing PF is probably highly influenced by how you set the detection boundaries for PF. You used 2 times the standard deviation, which is a sound statistical concept, but I wonder how this connects to the process/physics – i.e., the occurrence of preferential flow in general. Keep in mind that these limits (2* std) do affect the number of locations where you will detect preferential flow heavily.
As commented above, we will add some sentences concerning the standard deviation range chosen
I also think the way the data is clustered can affect the outcome of your analysis substantially. I assume that if your clustered pool is larger and has more isotopic variability (at different depths), the chance that a particular profile pops up as PF will be smaller, as compared to a small group of clustered profiles with lower general variability. This means that the sampling locations chosen and the number of locations sampled might affect the output. It also means that for reference profiles with small standard deviations, smaller deviations from the mean might already lead to PF detection, whereas in the case of large variability, it might not. Perhaps this should be discussed in the discussion section as something important to keep in mind.
We can add this to the discussion, but basically the most important driver is the intra-catchment variability of stable water isotopes in the soil. If the variability is low, reference profiles are narrow. If it is large, so will be the profile ranges- Figure 4: The difference between the two PF classes here is not clearly visible color-wise. If you want to distinguish them, it would probably be better to give them more distinct colors (currently both look reddish/orange). The grey background is not very visible and could be made a bit darker to more clearly show the region where samples are considered “piston flow.”
We chose the same color for both, as only if both are outliers, they get classified - Figure 6: Although I really like the figure, I did not find a clear reference to it in the main text. I was also not sure what the authors want to say with this plot. Why are fall plots from the TA location shown? What is the reasoning behind this arrangement? It would be great if the figure could be better integrated into the manuscript. In the caption, I also miss what the figure is trying to convey. To guide the reader more, I suggest clearly stating the purpose of the figure in the caption.
We can state more clearly that the aim of this plot was to visualize profiles on a single hillslope in near vicinity. The profiles in the lowest row are at the hill-foot and each row goes 10-20m upslope. Since most profiles were drilled throughout the catchment, this gridded design is present on 3 hillslopes per catchment and allows for analyzing plot scale variability on a hillslope - Figure 7: I generally like the figure, but I think it’s unclear what is on the x-axis. One could choose to depict a numerical value here (e.g., number of PF profiles) or a more meaningful variable. In the text, you write: “Most samples identified as preferential flow exhibited a mixture of 65% new event water and 35% older pre-event water.” Perhaps you could show this in the graph as well (as a dotted line, for example).
We will adapt the graphic - Discussion, Line 314: “However, this is not always the case.“ Remove the second period (“.”).
We will revise this - Discussion, Line 302: “One disadvantage is that a sufficient number of samples are required , with more samples improving analysis quality.” Remove the space before the comma here. Regarding the number of samples: I think it is not only about the number of samples. The representativeness of the samples also really matters, especially if you generate a reference profile. What would happen if you over-sample one location and under-sample another? How would the sampling design affect the reference profile and clusters that are built?
We will change this and also include something on the representativeness of our sampling locations and the effect of them - Figure 9: I would rephrase the caption to explain more clearly the intent. Also consider not using “Aspectcos” as a term here, but rather describing it in terms of slope direction. I’m not 100% sure about the absolute magnitude of the regression slope in the graph (as it does not reach “Flowpaths identified,” but rather stays close to “No Flowpaths”). I assume it relates to the probability of PF (between 0 and 1)? Does this not mean that, in general, the probability of detecting PF is lower than not detecting it—which may also be related to the fact that your sampling design includes many more “no PF” samples? How does your sampling distribution here affect your analysis?
As stated in the answer to Ryan Stewart, we will elaborate on that name. And yes, it is still more probable to find a profile without preferential flow on north facing slopes than it is to find one with one, however the chance of finding a PF Profile is highest on north facing slopes. - Discussion Section 3.4: I think this section could benefit from more detailed interpretation. I found it quite short and was thinking that some things could be explained (e.g., more on preferential flow from a catchment perspective). In general, I also wondered whether one could really draw strong conclusions about site-specific characteristics, given that the number of profiles where PF was detected was generally quite small. In TA, there are many detections, but in some other catchments, only 2 or 6 cases. This also relates to Figure 8 and 9.
We will further elaborate the validity of the conclusions drawn from the results and also write more on the number of profiles identified - Connection between Introduction (Lines 64–68), Introduction and Discussion: In the introduction, the authors mention that one of the complications of preferential flow detection is that field observations are just a snapshot:
“Also, field surveys are only a snapshot of an environmental system, but flowpath arrangements can change completely within one year (Wessolek et al., 2009; Beven, 2019). Additionally, even when preferential flow features are successfully identified at the plot scale, these findings cannot be easily extrapolated to the whole catchment.”
To what degree do you think this applies to your newly proposed method? Are the profiles you take not also a snapshot of the preferential flow pathways? What kind of temporal sampling or general sampling design would be needed to get a statistically sound idea of preferential flow occurrence at a particular site, rather than just a snapshot.
As stated in the beginning, it depends on the feature, but yes, it is definitely a snapshot, and it will always be as soil cores are highly invasive and once sampled may alter the flow mechanisms surrounding the sample location - Conclusion: I think the conclusion in this case would particularly benefit from a clear summary of pros and cons of this new methods. Currently the summary might not be fully accessible to people that have not read other parts of the manuscript. I always think it is a good opportunity to do this, as this would help to also guide readers that might just look at the conclusions really quick – this is helping readers quickly grasp the method’s utility and potential challenges.
We will add more pro/con to the conclusion
- C) Discussion (2) – add more on Novelty and Contribution: The manuscript presents an innovative and promising approach to identifying preferential flow in soils using stable water isotopes, which is a valuable addition to the “hydrological toolbox for preferential flow identification”. However, it would be helpful if the authors could explicitly position their method with respect to other common approaches (e.g., dye tracer studies, hydrometric techniques, geophysical methods). This contextualization could be more clearly revisited in the discussion to clarify the unique contributions and potential complementarities of this isotope-based approach.
- Citation Wilson: For the citation of Wilson et al. (2013), the first name is included in the text and in the reference list (located in the list of authors with a G). If I see this correctly, it is even the same Wilson as the one cited for 2016 (Wilson et al., 2016). As there is no other reference to Wilson, please consider adjusting this accordingly: Glenn V. Wilson, John L. Nieber, Roy C. Sidle, and Garey A. Fox: Internal Erosion during Soil Pipeflow: State of the Science for Experimental and Numerical Analysis, Transactions of the ASABE, 56, 465–478, https://doi.org/10.13031/2013.42667, 2013.
Interactive discussion
Status: closed
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CC1: 'Comment on egusphere-2025-2411', Ryan Stewart, 09 Jul 2025
Publisher’s note: this comment is a copy of RC1 and its content was therefore removed on 9 July 2025.
Citation: https://doi.org/10.5194/egusphere-2025-2411-CC1 -
RC1: 'Comment on egusphere-2025-2411', Ryan Stewart, 09 Jul 2025
General comments:
This manuscript describes the results of using stable water isotopes extracted from different soil depths to detect incidence of preferential flow, using data collected seasonally from four catchments in Europe. The manuscript is well-written save for some editorial suggestions listed below, and the approach is an interesting contribution. The manuscript focuses a bit more on the validation and assumptions of the approach than on the scientific contribution itself, so having a better balance with the actually scientific contribution of the work would be something to consider during the revision process.
In terms of results and interpretations, the approach appears to work best in areas with distinct seasonality in the isotopic signature of precipitation (e.g., the Alpine catchment) and operates under the assumption that water moving via preferential flow has the same isotopic signature as the topsoil. This assumption does not cover all instances of preferential flow, as discussed starting around Line 310.
The approach also relies on the assumption that there is isotopic exchange/equilibrium between mobile and bulk matrix water (Lines 321-328). Another possibility is that mobile water could still be present (but not equilibrated) within the soil at the time of sampling. Water content at the time of sampling could be a way to distinguish between these possibilities, and it could be generally instructive to present the water content data if those are available.
Another assumption (which I don’t think was discussed) is that the reference profiles were not affected by preferential flow. The authors constrain what they consider to be reference profiles based on presumed seasonality in the isotopic signature of input precipitation, but it might also be possible to use a simple plug flow calculation or something similar to perform a back-of-the-envelope verification of the approximate depths those seasonal inputs would move given an assumption of effective porosity and rainfall depth (the latter perhaps minus ET).
The manuscript also does not discuss situations in which the water at depth has a depleted isotopic signature relative to the reference profiles, even though such scenarios 1) exist in the dataset, and 2) may reveal interesting behaviors about subsurface flow.
With some revision the paper is a good candidate for publication in HESS.
Specific comments:
Line 2-16: Some minor grammatical issues here: 1) “may be quickly activated” sounds like it is referring to the soil matrix, 2) “and enhance infiltration or interflow”; 3) “profiles of stable water isotopes”; 4) “and selected those that matched…” 5) “heterogenous soils, many profiles”; 6) “flow pathways and highlight the…”; 7) “hillslope and catchment scales”.
Line 19: “water flows through… rather than the surrounding…”
Line 22: This range of preferential flow (16-27%) seems very specific. Either provide the context or consider not putting these numbers.
Line 25: “understanding” may not be needed twice.
Line 38: “soil-layer, which”.
Line 46: “formed”.
Line 47: Check your references that “Glenn V.” is needed for Wilson.
Line 53: 190 m is another number that seems very specific and context-specific. Can you at least express on a relative basis or something? Otherwise it doesn’t seem transferrable.
Line 58: Why is SSF only limited to 1/3 of events? Another specific rather than universal number.
Line 60: Velocities have already been discussed in L27-28.
Line 61-65: This section could be written more concisely.
Line 85: GPR can also be used in a timelapse manner to visualize changes in water content during discrete flow events.
Line 102: no dash is needed between continent and effect.
Line 111: “making them an ideal”.
Line 130: “and reach deeper”.
Line 132: “the signatures shift”.
Line 140: This could be a place to elaborate on the validity/assumptions of deriving reference profiles from the dataset itself.
Line 163: add “for delta18O” after 1.7 per mille. Same for Line 166.
Line 216: It seems you could solve this equation explicitly for f, which may not be that important but would better illustrate the analysis.
Line 272: Interesting interpretation/context.
Figure 4: The shading for SD is faint (didn’t show up in the printed copy I made) and would benefit from lines as in Figure 6.
Line 285: Might indicate that 65 and 35% are approximate values.
Line 284: Suggest calling the variable “aspect”, not “Aspectcos”, and it indicates the direction (not just northerly).
Line 305: Seems like these two sentences could be combined. Somewhat redundant currently.
Line 317: “in both cases.”
Figure 9: Did you consider/try fitting logistic models to the individual sites? The response appears to be driven primarily by the Alps site, which makes sense as the one showing the most preferential flow, but also it is hard to see the different catchments with the points overlaid on each other.
Line 318: “thus”.
Line 334-336: The comparison of the two stable isotopes is an important point, but one that wasn’t emphasized until here near the end of the paper. It would be good to make this point early on.
Line 354-360: This paragraph is choppy in its structure and logic. I suggest rewriting.
Citation: https://doi.org/10.5194/egusphere-2025-2411-RC1 -
AC2: 'Reply on RC1', Jonas Pyschik, 25 Jul 2025
Authors’ responses to the comments of Ryan Stewart
We appreciate your review and comments on our manuscript, “Detecting the occurrence of preferential flow in soils with stable water isotopes”. Your feedback is valuable to us, and we will make the recommended revisions accordingly. We provide detailed responses to each of your comments below.
General comments:
This manuscript describes the results of using stable water isotopes extracted from different soil depths to detect incidence of preferential flow, using data collected seasonally from four catchments in Europe. The manuscript is well-written save for some editorial suggestions listed below, and the approach is an interesting contribution. The manuscript focuses a bit more on the validation and assumptions of the approach than on the scientific contribution itself, so having a better balance with the actually scientific contribution of the work would be something to consider during the revision process.
In terms of results and interpretations, the approach appears to work best in areas with distinct seasonality in the isotopic signature of precipitation (e.g., the Alpine catchment) and operates under the assumption that water moving via preferential flow has the same isotopic signature as the topsoil. This assumption does not cover all instances of preferential flow, as discussed starting around Line 310.
The approach also relies on the assumption that there is isotopic exchange/equilibrium between mobile and bulk matrix water (Lines 321-328). Another possibility is that mobile water could still be present (but not equilibrated) within the soil at the time of sampling. Water content at the time of sampling could be a way to distinguish between these possibilities, and it could be generally instructive to present the water content data if those are available.
Thank you for this suggestion. We will further discuss this in the revision, however we do not have water content data.
Another assumption (which I don’t think was discussed) is that the reference profiles were not affected by preferential flow. The authors constrain what they consider to be reference profiles based on presumed seasonality in the isotopic signature of input precipitation, but it might also be possible to use a simple plug flow calculation or something similar to perform a back-of-the-envelope verification of the approximate depths those seasonal inputs would move given an assumption of effective porosity and rainfall depth (the latter perhaps minus ET).
Unfortunately, we lack the precipitation data of the year previous to drilling at those locations. Our approach aimed at filling this data gap with the reference profiles. We will make this clearer in the revision, that the reference profile creation was due to lacking isotope values in the rainfall.
The manuscript also does not discuss situations in which the water at depth has a depleted isotopic signature relative to the reference profiles, even though such scenarios 1) exist in the dataset, and 2) may reveal interesting behaviors about subsurface flow.
Yes, those instances are sometimes found in the data, however this was a really minor case. It might be that “older” winter water was transported there, but since we are not able to assess the origin of the signature (as it is not within the topsoil reference profile), we are unable to say which flow process transported it there.
With some revision the paper is a good candidate for publication in HESS.
Specific comments:
Line 2-16: Some minor grammatical issues here: 1) “may be quickly activated” sounds like it is referring to the soil matrix, 2) “and enhance infiltration or interflow”; 3) “profiles of stable water isotopes”; 4) “and selected those that matched…” 5) “heterogenous soils, many profiles”; 6) “flow pathways and highlight the…”; 7) “hillslope and catchment scales”.
We will fix that
Line 19: “water flows through… rather than the surrounding…”
We will change this
Line 22: This range of preferential flow (16-27%) seems very specific. Either provide the context or consider not putting these numbers.
It was stated in the publication but is indeed very specific, therefore we will remove the numbers in the revision
Line 25: “understanding” may not be needed twice.
We will rephrase
Line 38: “soil-layer, which”.
We will change that
Line 46: “formed”.
We will update the sentence
Line 47: Check your references that “Glenn V.” is needed for Wilson.
We will revise the citation to leave out the surname.
Line 53: 190 m is another number that seems very specific and context-specific. Can you at least express on a relative basis or something? Otherwise it doesn’t seem transferrable.
It was also stated in that publication but is also very specific, therefore we will remove the number in the revision
Line 58: Why is SSF only limited to 1/3 of events? Another specific rather than universal number.
We will also remove this number
Line 60: Velocities have already been discussed in L27-28.
We will remove this in the revision
Line 61-65: This section could be written more concisely.
We will try to make this more concise.
Line 85: GPR can also be used in a timelapse manner to visualize changes in water content during discrete flow events.
Thank you, we will add that
Line 102: no dash is needed between continent and effect.
We will remove this
Line 111: “making them an ideal”.
We will update the wording
Line 130: “and reach deeper”.
We will change this
Line 132: “the signatures shift”.
We will revise this
Line 140: This could be a place to elaborate on the validity/assumptions of deriving reference profiles from the dataset itself.
We will include a few sentences in the revisions where we elaborate on the validity
Line 163: add “for delta18O” after 1.7 per mille. Same for Line 166.
Yes, we missed that and will add it
Line 216: It seems you could solve this equation explicitly for f, which may not be that important but would better illustrate the analysis.
True, we will change it so it gets clearer what we are actually solving
Line 272: Interesting interpretation/context.
Thank you!
Figure 4: The shading for SD is faint (didn’t show up in the printed copy I made) and would benefit from lines as in Figure 6.
We will change it to the same style as in Figure 6
Line 285: Might indicate that 65 and 35% are approximate values.
Yes, we will add that
Line 284: Suggest calling the variable “aspect”, not “Aspectcos”, and it indicates the direction (not just northerly).
We also calculated this for Aspect (Range 0-360 degree) which discerns between east and west facing slopes, where we found no effect, and used the cos of aspect to gain a metric to discern between north and south, therefore we will keep the name but also add some explanation on this
Line 305: Seems like these two sentences could be combined. Somewhat redundant currently.
We will write this more concisely
Line 317: “in both cases.”
We will change the wording
Figure 9: Did you consider/try fitting logistic models to the individual sites? The response appears to be driven primarily by the Alps site, which makes sense as the one showing the most preferential flow, but also it is hard to see the different catchments with the points overlaid on each other.
Yes, we tried and still saw the effect, but stronger in the alps. We will add that to the revision
Line 318: “thus”.
We will change this
Line 334-336: The comparison of the two stable isotopes is an important point, but one that wasn’t emphasized until here near the end of the paper. It would be good to make this point early on.
We will shift this further up
Line 354-360: This paragraph is choppy in its structure and logic. I suggest rewriting.
We will rewrite it ensure more structure and logic.
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AC2: 'Reply on RC1', Jonas Pyschik, 25 Jul 2025
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RC2: 'Comment on egusphere-2025-2411', Inge Wiekenkamp, 13 Jul 2025
I have read the manuscript entitled “Detecting the occurrence of preferential flow in soils with stable water isotopes” written by Jonas Pyschik and Markus Weiler. In this work, they introduce a new method to identify locations where preferential flow occurs (both lateral and vertical), based on stable water isotope profiles in the soil. The core idea is to use deviations from reference profiles in the isotope signature as an indication of preferential flow occurrence.
I am confident that this paper is highly relevant and fits well within the scope of HESS, as it introduces a new method to identify preferential flow using stable water isotopes in soil profiles. It highlights the potential of isotopes as a novel tool to trace subsurface processes. Although the scientific method is clearly described, the assumptions and limitations could be discussed in more detail (see, for example, general comment B).
The paper is well-structured and demonstrates the authors’ strong expertise in both hydrological processes and isotope applications, here specifically focusing on subsurface flow. Figures are informative and visually appealing, and the dataset compiled is impressively broad. With some targeted refinements, the manuscript can be further strengthened and made even more accessible to a broader readership.
General comments:
A) Reference profile: I really like your approach, but was wondering about the following limitation. In your clustering and reference profile determination, you assume that no preferential flow is present. I can imagine that this is not always the case, because there might be particular features in some of these soils that can always facilitate preferential flow. In a way this approach means that more permanent features (facilitating preferential flow) that could be present in a lot of profiles are not indicated and present in this case. However, I can understand also that based on this average cluster profile that you create, in a way, such feature would need to be present in all the clustered profiles and at the same depth (which might be unlikely if you include a lot of different profiles and use a small number of clusters). Perhaps one could elaborate on this.
B) Discussion (1): While the discussion already touches on important opportunities and limitations, I believe it could benefit from further elaboration on a few points:
(1) Are there particular profiles, landscape types, or environmental conditions where this method is less applicable or might fail?
(2) Although the method is insightful, it still requires soil sampling, meaning that it provides a snapshot in time. How representative is this snapshot for a full season or hydrological cycle?
(3) Regarding the 2*std criterion for detecting deviations from the reference profile: could the threshold be sensitive to sampling design or the number of samples? Are the chosen limits potentially too conservative, and how might this influence the risk of false positives or false negatives?
Some of these suggestions are further elaborated in the detailed comments.C) Discussion (2) – add more on Novelty and Contribution: The manuscript presents an innovative and promising approach to identifying preferential flow in soils using stable water isotopes, which is a valuable addition to the “hydrological toolbox for preferential flow identification”. However, it would be helpful if the authors could explicitly position their method with respect to other common approaches (e.g., dye tracer studies, hydrometric techniques, geophysical methods). This contextualization could be more clearly revisited in the discussion to clarify the unique contributions and potential complementarities of this isotope-based approach.
D) Accessibility and Reproducibility: Given the method involves data clustering and isotope profile analysis, some information on data availability, reproducibility, or whether the authors will provide scripts/code for other researchers to apply this method could be valuable. Encouraging open science practices would enhance the method’s uptake and usability by the community.
E) Spatial Drivers: The spatial analysis section appears relatively brief and less extensive compared to other parts of the manuscript. This is likely constrained by the limited number of profiles where preferential flow (PF) was detected, which reduces the ability to identify clear spatial drivers. It might be helpful for the authors to acknowledge this limitation explicitly and, if possible, consider expanding the spatial analysis or discussing potential ways to improve it in future work.
Detailed comments:- Citation Wilson: For the citation of Wilson et al. (2013), the first name is included in the text and in the reference list (located in the list of authors with a G). If I see this correctly, it is even the same Wilson as the one cited for 2016 (Wilson et al., 2016). As there is no other reference to Wilson, please consider adjusting this accordingly: Glenn V. Wilson, John L. Nieber, Roy C. Sidle, and Garey A. Fox: Internal Erosion during Soil Pipeflow: State of the Science for Experimental and Numerical Analysis, Transactions of the ASABE, 56, 465–478, https://doi.org/10.13031/2013.42667, 2013.
- Citation style: I noticed that references often end with a double “))” at the end, for example here: “(Thomas et al., 2013; Demand et al., 2019a))”. Is this the style the citations are supposed to have? If not, please consider updating this accordingly.
- Introduction, Lines 51–53: “During water flow in macropores, they are typically not filled entirely with water but a water film forms along the wall if the pore, leaving the central part of the pore empty.” I think the “if the pore” sounds incorrect. Should “if” be replaced by “in”?
- Introduction: I was just curious about the connection between the following two sentences:
In Lines 21–22, authors refer to the flow in the soil:
“Preferential flow does not occur during every rainfall or infiltration event, but when it is activated, it can account for a significant proportion of annual flow through the soil, ranging from 16–27% (Eguchi and Hasegawa, 2008).”
Later, they refer to the contribution of preferential flow to discharge:
“The complex network of macropores, particularly soil pipes in hillslopes, can extend up to 190 m and can contribute up to 50% to overall discharge in streams (Jones, 2010; Wilson et al., 2016).”
I was wondering if these statements fit together or if they might mismatch. If you could also give a range for the second statement (“up to 50%”), this would maybe give a better feeling of the general importance and variability in preferential flow importance. - Introduction, statement on Ground Penetrating Radar (GPR): A period is missing at the end of the sentence. This was present for the other sentences. Also, I assume that another problem of these geophysical methods is the non-unique solution of the inversion results (imaging). This could be added and stated as a limitation of the method. Perhaps you could in this section rather refer more generally to geophysical methods that are able to characterize PF (ERT – Electrical Resistivity Tomography – is, for example, also used in multiple cases to visualize preferential flow paths), and include the limitation of non-uniqueness (underdetermined system)?
- Introduction, Lines 132–134: “Over time, however, the signatures shifts towards those of pre-event water (Leaney et al., 1993; Gehrels et al., 1998; Kelln et al., 2007) due to lateral infiltration and exchange processes between the preferential pathways and the surrounding matrix.” Please replace “shifts” with “shift”.
- Figure 1: It would be great if you could add (either in the figure or the caption) that the soil profiles are stable water isotope profiles. Perhaps the authors could also add the number of profiles to each catchment (to get a feeling for the number of points – vertical profiles – in each area). Is this always 100? Then this could also just be mentioned in the caption to give a direct feeling of the magnitude.
- Methods, 2.3, Line 197: “from the R caret package Kuhn (2008).” Probably this should be: “from the R caret package by Kuhn, 2008” (or use the bracket version: “(Kuhn, 2008)”).
- Figure 2: I like the schematic representation of the method, but I think it would help if the figure had x and y axis descriptions (not ranges, just an explanation of variables – depth on the y-axis, x-axis labeling δ²H / scaled δ¹⁸O (‰)). In the second sub-figure, the line borders of x and y axes are missing. I suggest implementing these as well.
- Methods, section 2.3: “Only depths where both δ²H and scaled 18 O values exceeded the reference range were considered for potential preferential flow (Figure 2.4).” Should “scaled 18 O” not be replaced by δ¹⁸O? Also, when referring to Figure 2.4, one could state the color of the points that are considered indicative of preferential flow (orange points, right?).
- Methods, 2.4 Mixing models: “By solving this equation, the proportion of preferential flow (f) at the identified depths was determined.” Before this sentence, a description is provided about the proportion of preferential flow. Does this implicitly mean that one could not indicate preferential flow in the topsoil with this method? Also, how would this equation work if the delta values of the topsoil and reference are very similar (could for example happen at the second sampling depth, I imagine)?
- 1 Reference profiles: In the results, the sampling periods for each region are also mentioned. This could possibly be moved to the methods section to keep more focus on the results here. I think the results are very descriptive. It would be quite nice if there was more comparison between the results. For example, to more easily compare results from different areas, one could also describe all summer results together and position the plots in Figure 3 accordingly. For instance, blue and yellow curve SL summer and BF summer curve seem to have very similar features and could be connected nicely.
- Table 1: First of all, it’s really impressive how many samples and profiles have been measured for this effort. I would suggest adjusting “Profiles with multiple PF” to “Profiles with PF at multiple depths.” I also think that the number of profiles showing PF is probably highly influenced by how you set the detection boundaries for PF. You used 2 times the standard deviation, which is a sound statistical concept, but I wonder how this connects to the process/physics – i.e., the occurrence of preferential flow in general. Keep in mind that these limits (2* std) do affect the number of locations where you will detect preferential flow heavily.
I also think the way the data is clustered can affect the outcome of your analysis substantially. I assume that if your clustered pool is larger and has more isotopic variability (at different depths), the chance that a particular profile pops up as PF will be smaller, as compared to a small group of clustered profiles with lower general variability. This means that the sampling locations chosen and the number of locations sampled might affect the output. It also means that for reference profiles with small standard deviations, smaller deviations from the mean might already lead to PF detection, whereas in the case of large variability, it might not. Perhaps this should be discussed in the discussion section as something important to keep in mind. - Figure 4: The difference between the two PF classes here is not clearly visible color-wise. If you want to distinguish them, it would probably be better to give them more distinct colors (currently both look reddish/orange). The grey background is not very visible and could be made a bit darker to more clearly show the region where samples are considered “piston flow.”
- Figure 6: Although I really like the figure, I did not find a clear reference to it in the main text. I was also not sure what the authors want to say with this plot. Why are fall plots from the TA location shown? What is the reasoning behind this arrangement? It would be great if the figure could be better integrated into the manuscript. In the caption, I also miss what the figure is trying to convey. To guide the reader more, I suggest clearly stating the purpose of the figure in the caption.
- Figure 7: I generally like the figure, but I think it’s unclear what is on the x-axis. One could choose to depict a numerical value here (e.g., number of PF profiles) or a more meaningful variable. In the text, you write: “Most samples identified as preferential flow exhibited a mixture of 65% new event water and 35% older pre-event water.” Perhaps you could show this in the graph as well (as a dotted line, for example).
- Discussion, Line 314: “However, this is not always the case.“ Remove the second period (“.”).
- Discussion, Line 302: “One disadvantage is that a sufficient number of samples are required , with more samples improving analysis quality.” Remove the space before the comma here. Regarding the number of samples: I think it is not only about the number of samples. The representativeness of the samples also really matters, especially if you generate a reference profile. What would happen if you over-sample one location and under-sample another? How would the sampling design affect the reference profile and clusters that are built?
- Figure 9: I would rephrase the caption to explain more clearly the intent. Also consider not using “Aspectcos” as a term here, but rather describing it in terms of slope direction. I’m not 100% sure about the absolute magnitude of the regression slope in the graph (as it does not reach “Flowpaths identified,” but rather stays close to “No Flowpaths”). I assume it relates to the probability of PF (between 0 and 1)? Does this not mean that, in general, the probability of detecting PF is lower than not detecting it—which may also be related to the fact that your sampling design includes many more “no PF” samples? How does your sampling distribution here affect your analysis?
- Discussion Section 3.4: I think this section could benefit from more detailed interpretation. I found it quite short and was thinking that some things could be explained (e.g., more on preferential flow from a catchment perspective). In general, I also wondered whether one could really draw strong conclusions about site-specific characteristics, given that the number of profiles where PF was detected was generally quite small. In TA, there are many detections, but in some other catchments, only 2 or 6 cases. This also relates to Figure 8 and 9.
- Connection between Introduction (Lines 64–68), Introduction and Discussion: In the introduction, the authors mention that one of the complications of preferential flow detection is that field observations are just a snapshot:
“Also, field surveys are only a snapshot of an environmental system, but flowpath arrangements can change completely within one year (Wessolek et al., 2009; Beven, 2019). Additionally, even when preferential flow features are successfully identified at the plot scale, these findings cannot be easily extrapolated to the whole catchment.”
To what degree do you think this applies to your newly proposed method? Are the profiles you take not also a snapshot of the preferential flow pathways? What kind of temporal sampling or general sampling design would be needed to get a statistically sound idea of preferential flow occurrence at a particular site, rather than just a snapshot. - Conclusion: I think the conclusion in this case would particularly benefit from a clear summary of pros and cons of this new methods. Currently the summary might not be fully accessible to people that have not read other parts of the manuscript. I always think it is a good opportunity to do this, as this would help to also guide readers that might just look at the conclusions really quick – this is helping readers quickly grasp the method’s utility and potential challenges.
Citation: https://doi.org/10.5194/egusphere-2025-2411-RC2 -
AC1: 'Reply on RC2', Jonas Pyschik, 25 Jul 2025
Authors’ responses to the comments of Inge Wiekenkamp
We appreciate your review and comments on our manuscript, “Detecting the occurrence of preferential flow in soils with stable water isotopes”. Your feedback is valuable to us, and we will make the recommended revisions accordingly. We provide detailed responses to each of your comments below.
I have read the manuscript entitled “Detecting the occurrence of preferential flow in soils with stable water isotopes” written by Jonas Pyschik and Markus Weiler. In this work, they introduce a new method to identify locations where preferential flow occurs (both lateral and vertical), based on stable water isotope profiles in the soil. The core idea is to use deviations from reference profiles in the isotope signature as an indication of preferential flow occurrence.
I am confident that this paper is highly relevant and fits well within the scope of HESS, as it introduces a new method to identify preferential flow using stable water isotopes in soil profiles. It highlights the potential of isotopes as a novel tool to trace subsurface processes. Although the scientific method is clearly described, the assumptions and limitations could be discussed in more detail (see, for example, general comment B).
The paper is well-structured and demonstrates the authors’ strong expertise in both hydrological processes and isotope applications, here specifically focusing on subsurface flow. Figures are informative and visually appealing, and the dataset compiled is impressively broad. With some targeted refinements, the manuscript can be further strengthened and made even more accessible to a broader readership.
Thank you!
General comments:
A) Reference profile: I really like your approach, but was wondering about the following limitation. In your clustering and reference profile determination, you assume that no preferential flow is present. I can imagine that this is not always the case, because there might be particular features in some of these soils that can always facilitate preferential flow. In a way this approach means that more permanent features (facilitating preferential flow) that could be present in a lot of profiles are not indicated and present in this case. However, I can understand also that based on this average cluster profile that you create, in a way, such feature would need to be present in all the clustered profiles and at the same depth (which might be unlikely if you include a lot of different profiles and use a small number of clusters). Perhaps one could elaborate on this.
This is partially correct and we can further elaborate on this in the revision. There may be preferential flow features persistent in many profiles. However, our first step in defining reference profiles is fitting a 3rd order polynomial function through the points, which discards single outliers which are typical for preferential flow effects. However, if for instance all hillslope would laterally transports water preferentially and similar depths are influenced, then even the polynomial lines would be skewed. However, we consider this highly unlikely. But we can certainly provide some more background on our assumptions.
B) Discussion (1): While the discussion already touches on important opportunities and limitations, I believe it could benefit from further elaboration on a few points:
(1) Are there particular profiles, landscape types, or environmental conditions where this method is less applicable or might fail?We will add something on that in the revision
(2) Although the method is insightful, it still requires soil sampling, meaning that it provides a snapshot in time. How representative is this snapshot for a full season or hydrological cycle?True, it is only a snapshot. We will elaborate on this in the revision. As preferential flow features are not always active, this can definitely only be seen as a short time assessment. However, some features, like the ones shown in the alpine hillslope which seem to be interconnected are probably more persistent. In future studies, multiple sampling at different times in the year could help to tackle the questions.
(3) Regarding the 2*std criterion for detecting deviations from the reference profile: could the threshold be sensitive to sampling design or the number of samples? Are the chosen limits potentially too conservative, and how might this influence the risk of false positives or false negatives?The limits are really strict and using for instance only 1*sd we get way more preferential flowpaths identified, but also a higher probability for false positives. We will include this in the discussion.
Some of these suggestions are further elaborated in the detailed comments.- C) Discussion (2) – add more on Novelty and Contribution: The manuscript presents an innovative and promising approach to identifying preferential flow in soils using stable water isotopes, which is a valuable addition to the “hydrological toolbox for preferential flow identification”. However, it would be helpful if the authors could explicitly position their method with respect to other common approaches (e.g., dye tracer studies, hydrometric techniques, geophysical methods). This contextualization could be more clearly revisited in the discussion to clarify the unique contributions and potential complementarities of this isotope-based approach.
We will clarify the unique contributions and potential complementarities of our approach in the discussion.
D) Accessibility and Reproducibility: Given the method involves data clustering and isotope profile analysis, some information on data availability, reproducibility, or whether the authors will provide scripts/code for other researchers to apply this method could be valuable. Encouraging open science practices would enhance the method’s uptake and usability by the community.
We will add the code to reproduce the findings. The data will be made available in a separate data paper including a wider variety of isotope data of the catchment in the following months.
E) Spatial Drivers: The spatial analysis section appears relatively brief and less extensive compared to other parts of the manuscript. This is likely constrained by the limited number of profiles where preferential flow (PF) was detected, which reduces the ability to identify clear spatial drivers. It might be helpful for the authors to acknowledge this limitation explicitly and, if possible, consider expanding the spatial analysis or discussing potential ways to improve it in future work.
We will elaborate on the limited spatial analysis due to limited identified preferential flow profiles
Detailed comments:
- Citation Wilson: For the citation of Wilson et al. (2013), the first name is included in the text and in the reference list (located in the list of authors with a G). If I see this correctly, it is even the same Wilson as the one cited for 2016 (Wilson et al., 2016). As there is no other reference to Wilson, please consider adjusting this accordingly: Glenn V. Wilson, John L. Nieber, Roy C. Sidle, and Garey A. Fox: Internal Erosion during Soil Pipeflow: State of the Science for Experimental and Numerical Analysis, Transactions of the ASABE, 56, 465–478, https://doi.org/10.13031/2013.42667, 2013.
We will fix the citation - Citation style: I noticed that references often end with a double “))” at the end, for example here: “(Thomas et al., 2013; Demand et al., 2019a))”. Is this the style the citations are supposed to have? If not, please consider updating this accordingly.
We will correct that error - Introduction, Lines 51–53: “During water flow in macropores, they are typically not filled entirely with water but a water film forms along the wall if the pore, leaving the central part of the pore empty.” I think the “if the pore” sounds incorrect. Should “if” be replaced by “in”?
We will change the wording - Introduction: I was just curious about the connection between the following two sentences:
In Lines 21–22, authors refer to the flow in the soil:
“Preferential flow does not occur during every rainfall or infiltration event, but when it is activated, it can account for a significant proportion of annual flow through the soil, ranging from 16–27% (Eguchi and Hasegawa, 2008).”
Later, they refer to the contribution of preferential flow to discharge:
“The complex network of macropores, particularly soil pipes in hillslopes, can extend up to 190 m and can contribute up to 50% to overall discharge in streams (Jones, 2010; Wilson et al., 2016).”
I was wondering if these statements fit together or if they might mismatch. If you could also give a range for the second statement (“up to 50%”), this would maybe give a better feeling of the general importance and variability in preferential flow importance.
In line with the Review by Ryan Stewart we will fully remove these numbers. - Introduction, statement on Ground Penetrating Radar (GPR): A period is missing at the end of the sentence. This was present for the other sentences. Also, I assume that another problem of these geophysical methods is the non-unique solution of the inversion results (imaging). This could be added and stated as a limitation of the method. Perhaps you could in this section rather refer more generally to geophysical methods that are able to characterize PF (ERT – Electrical Resistivity Tomography – is, for example, also used in multiple cases to visualize preferential flow paths), and include the limitation of non-uniqueness (underdetermined system)?
We will fix the period errors and state this limitation - Introduction, Lines 132–134: “Over time, however, the signatures shifts towards those of pre-event water (Leaney et al., 1993; Gehrels et al., 1998; Kelln et al., 2007) due to lateral infiltration and exchange processes between the preferential pathways and the surrounding matrix.” Please replace “shifts” with “shift”.
We will fix that - Figure 1: It would be great if you could add (either in the figure or the caption) that the soil profiles are stable water isotope profiles. Perhaps the authors could also add the number of profiles to each catchment (to get a feeling for the number of points – vertical profiles – in each area). Is this always 100? Then this could also just be mentioned in the caption to give a direct feeling of the magnitude.
We will add that to the figure caption and map - Methods, 2.3, Line 197: “from the R caret package Kuhn (2008).” Probably this should be: “from the R caret package by Kuhn, 2008” (or use the bracket version: “(Kuhn, 2008)”).
We will change that - Figure 2: I like the schematic representation of the method, but I think it would help if the figure had x and y axis descriptions (not ranges, just an explanation of variables – depth on the y-axis, x-axis labeling δ²H / scaled δ¹⁸O (‰)). In the second sub-figure, the line borders of x and y axes are missing. I suggest implementing these as well.
We will try to include this while still keeping the graphic concise - Methods, section 2.3: “Only depths where both δ²H and scaled 18 O values exceeded the reference range were considered for potential preferential flow (Figure 2.4).” Should “scaled 18 O” not be replaced by δ¹⁸O? Also, when referring to Figure 2.4, one could state the color of the points that are considered indicative of preferential flow (orange points, right?).
We will add that and revise - Methods, 2.4 Mixing models: “By solving this equation, the proportion of preferential flow (f) at the identified depths was determined.” Before this sentence, a description is provided about the proportion of preferential flow. Does this implicitly mean that one could not indicate preferential flow in the topsoil with this method? Also, how would this equation work if the delta values of the topsoil and reference are very similar (could for example happen at the second sampling depth, I imagine)?
We always exclude the two topsoil signatures as these data ranges are what we use to identify preferential flow. We would always get 100% event water in those zones. - 1 Reference profiles: In the results, the sampling periods for each region are also mentioned. This could possibly be moved to the methods section to keep more focus on the results here. I think the results are very descriptive. It would be quite nice if there was more comparison between the results. For example, to more easily compare results from different areas, one could also describe all summer results together and position the plots in Figure 3 accordingly. For instance, blue and yellow curve SL summer and BF summer curve seem to have very similar features and could be connected nicely.
We will try to find a way to arrange the graphics this differently and also add some comparative sentences - Table 1: First of all, it’s really impressive how many samples and profiles have been measured for this effort. I would suggest adjusting “Profiles with multiple PF” to “Profiles with PF at multiple depths.” I also think that the number of profiles showing PF is probably highly influenced by how you set the detection boundaries for PF. You used 2 times the standard deviation, which is a sound statistical concept, but I wonder how this connects to the process/physics – i.e., the occurrence of preferential flow in general. Keep in mind that these limits (2* std) do affect the number of locations where you will detect preferential flow heavily.
As commented above, we will add some sentences concerning the standard deviation range chosen
I also think the way the data is clustered can affect the outcome of your analysis substantially. I assume that if your clustered pool is larger and has more isotopic variability (at different depths), the chance that a particular profile pops up as PF will be smaller, as compared to a small group of clustered profiles with lower general variability. This means that the sampling locations chosen and the number of locations sampled might affect the output. It also means that for reference profiles with small standard deviations, smaller deviations from the mean might already lead to PF detection, whereas in the case of large variability, it might not. Perhaps this should be discussed in the discussion section as something important to keep in mind.
We can add this to the discussion, but basically the most important driver is the intra-catchment variability of stable water isotopes in the soil. If the variability is low, reference profiles are narrow. If it is large, so will be the profile ranges- Figure 4: The difference between the two PF classes here is not clearly visible color-wise. If you want to distinguish them, it would probably be better to give them more distinct colors (currently both look reddish/orange). The grey background is not very visible and could be made a bit darker to more clearly show the region where samples are considered “piston flow.”
We chose the same color for both, as only if both are outliers, they get classified - Figure 6: Although I really like the figure, I did not find a clear reference to it in the main text. I was also not sure what the authors want to say with this plot. Why are fall plots from the TA location shown? What is the reasoning behind this arrangement? It would be great if the figure could be better integrated into the manuscript. In the caption, I also miss what the figure is trying to convey. To guide the reader more, I suggest clearly stating the purpose of the figure in the caption.
We can state more clearly that the aim of this plot was to visualize profiles on a single hillslope in near vicinity. The profiles in the lowest row are at the hill-foot and each row goes 10-20m upslope. Since most profiles were drilled throughout the catchment, this gridded design is present on 3 hillslopes per catchment and allows for analyzing plot scale variability on a hillslope - Figure 7: I generally like the figure, but I think it’s unclear what is on the x-axis. One could choose to depict a numerical value here (e.g., number of PF profiles) or a more meaningful variable. In the text, you write: “Most samples identified as preferential flow exhibited a mixture of 65% new event water and 35% older pre-event water.” Perhaps you could show this in the graph as well (as a dotted line, for example).
We will adapt the graphic - Discussion, Line 314: “However, this is not always the case.“ Remove the second period (“.”).
We will revise this - Discussion, Line 302: “One disadvantage is that a sufficient number of samples are required , with more samples improving analysis quality.” Remove the space before the comma here. Regarding the number of samples: I think it is not only about the number of samples. The representativeness of the samples also really matters, especially if you generate a reference profile. What would happen if you over-sample one location and under-sample another? How would the sampling design affect the reference profile and clusters that are built?
We will change this and also include something on the representativeness of our sampling locations and the effect of them - Figure 9: I would rephrase the caption to explain more clearly the intent. Also consider not using “Aspectcos” as a term here, but rather describing it in terms of slope direction. I’m not 100% sure about the absolute magnitude of the regression slope in the graph (as it does not reach “Flowpaths identified,” but rather stays close to “No Flowpaths”). I assume it relates to the probability of PF (between 0 and 1)? Does this not mean that, in general, the probability of detecting PF is lower than not detecting it—which may also be related to the fact that your sampling design includes many more “no PF” samples? How does your sampling distribution here affect your analysis?
As stated in the answer to Ryan Stewart, we will elaborate on that name. And yes, it is still more probable to find a profile without preferential flow on north facing slopes than it is to find one with one, however the chance of finding a PF Profile is highest on north facing slopes. - Discussion Section 3.4: I think this section could benefit from more detailed interpretation. I found it quite short and was thinking that some things could be explained (e.g., more on preferential flow from a catchment perspective). In general, I also wondered whether one could really draw strong conclusions about site-specific characteristics, given that the number of profiles where PF was detected was generally quite small. In TA, there are many detections, but in some other catchments, only 2 or 6 cases. This also relates to Figure 8 and 9.
We will further elaborate the validity of the conclusions drawn from the results and also write more on the number of profiles identified - Connection between Introduction (Lines 64–68), Introduction and Discussion: In the introduction, the authors mention that one of the complications of preferential flow detection is that field observations are just a snapshot:
“Also, field surveys are only a snapshot of an environmental system, but flowpath arrangements can change completely within one year (Wessolek et al., 2009; Beven, 2019). Additionally, even when preferential flow features are successfully identified at the plot scale, these findings cannot be easily extrapolated to the whole catchment.”
To what degree do you think this applies to your newly proposed method? Are the profiles you take not also a snapshot of the preferential flow pathways? What kind of temporal sampling or general sampling design would be needed to get a statistically sound idea of preferential flow occurrence at a particular site, rather than just a snapshot.
As stated in the beginning, it depends on the feature, but yes, it is definitely a snapshot, and it will always be as soil cores are highly invasive and once sampled may alter the flow mechanisms surrounding the sample location - Conclusion: I think the conclusion in this case would particularly benefit from a clear summary of pros and cons of this new methods. Currently the summary might not be fully accessible to people that have not read other parts of the manuscript. I always think it is a good opportunity to do this, as this would help to also guide readers that might just look at the conclusions really quick – this is helping readers quickly grasp the method’s utility and potential challenges.
We will add more pro/con to the conclusion
- C) Discussion (2) – add more on Novelty and Contribution: The manuscript presents an innovative and promising approach to identifying preferential flow in soils using stable water isotopes, which is a valuable addition to the “hydrological toolbox for preferential flow identification”. However, it would be helpful if the authors could explicitly position their method with respect to other common approaches (e.g., dye tracer studies, hydrometric techniques, geophysical methods). This contextualization could be more clearly revisited in the discussion to clarify the unique contributions and potential complementarities of this isotope-based approach.
- Citation Wilson: For the citation of Wilson et al. (2013), the first name is included in the text and in the reference list (located in the list of authors with a G). If I see this correctly, it is even the same Wilson as the one cited for 2016 (Wilson et al., 2016). As there is no other reference to Wilson, please consider adjusting this accordingly: Glenn V. Wilson, John L. Nieber, Roy C. Sidle, and Garey A. Fox: Internal Erosion during Soil Pipeflow: State of the Science for Experimental and Numerical Analysis, Transactions of the ASABE, 56, 465–478, https://doi.org/10.13031/2013.42667, 2013.
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Jonas Pyschik
Markus Weiler
The requested preprint has a corresponding peer-reviewed final revised paper. You are encouraged to refer to the final revised version.
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Publisher’s note: this comment is a copy of RC1 and its content was therefore removed on 9 July 2025.