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https://doi.org/10.5194/egusphere-2023-1025
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/egusphere-2023-1025
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
28 Jun 2023
| 28 Jun 2023
Is transport of microplastics different from that of mineral dust? Results from idealized wind tunnel studies
Eike Maximilian Esders
CORRESPONDING AUTHOR
Micrometeorology Group, University of Bayreuth, Universitätsstraße 30, Bayreuth, Germany
Sebastian Sittl
Department of Physical Chemistry II, Universtiy of Bayreuth, Universitätsstraße 30, Bayreuth, Germany
Inka Krammel
Department of Physical Chemistry II, Universtiy of Bayreuth, Universitätsstraße 30, Bayreuth, Germany
Wolfgang Babel
Micrometeorology Group, University of Bayreuth, Universitätsstraße 30, Bayreuth, Germany
Bayreuth Center of Ecology and Environmental Research, Dr.Hans-Frisch-Str.1-3, Bayreuth, Germany
Georg Papastavrou
Department of Physical Chemistry II, Universtiy of Bayreuth, Universitätsstraße 30, Bayreuth, Germany
Christoph Karl Thomas
Micrometeorology Group, University of Bayreuth, Universitätsstraße 30, Bayreuth, Germany
Bayreuth Center of Ecology and Environmental Research, Dr.Hans-Frisch-Str.1-3, Bayreuth, Germany
Abstract. Atmospheric transport disperses microplastic particulate matter to virtually every environment on the planet. Despite the well-known long-range transport, only few studies have examined the fundamental transport mechanisms for microplastics and contrasted it with the existing body of knowledge accumulated for mineral dust over the past decades. Our study addresses this research gap and presents results from wind tunnel experiments, which examine the detachment behavior of microplastics ranging from 38 to 125 µm in diameter from idealized substrates. We here define 'detachment' as microspheres detaching from a substrate and leaving the field of observation, which includes several transport modes including creeping, rolling, directly lifting off. The detachment behavior of polyethylene microspheres (PE69) and borosilicate microspheres (GL69) of nominally the same physical diameter (63–75 µm) are contrasted across hydrophilic to hydrophobic substrates. We further examine the effect of microsphere-microsphere collisions on the detachment behavior of both polyethylene and borosilicate microspheres. Differentiating between collision independent microspheres and collisions dependent microspheres revealed that collisions impact detachment from enhancing to mitigating. Further, results indicate that GL69, as a hydrophilic particle, is highly dependent on substrate hydrophobicity and PE69 is less affected by it. A more detailed comparison between GL69 and PE69 regarding surface and substrate hydrophobicity is masked by the influence of capillary forces. Moreover, the smallest polyethylene microspheres behave similar to mineral microspheres. Results demonstrate that PE69 and GL69 as proxy for plastic and mineral dust, respectively, detach at u* between 0.1 to 0.3 ms-1 fitting to the prediction of the simple wind erosion model by Shao et al. (2000). In the observed range of rH, capillary forces can increase the median detachment by about 0.2 ms-1 for PE69 and GL69. Polyethylene microspheres, smaller than 70 µm in diameter, behave like borosilicate microspheres of the same size. For bigger microspheres, the lesser density of polyethylene drives their higher erodibility. We conclude that it is no surprise, that like mineral dust, plastic dust is found all around the globe, transported via the atmosphere.
How to cite. Esders, E. M., Sittl, S., Krammel, I., Babel, W., Papastavrou, G., and Thomas, C. K.: Is transport of microplastics different from that of mineral dust? Results from idealized wind tunnel studies, EGUsphere [preprint], https://doi.org/10.5194/egusphere-2023-1025, 2023.
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Eike Maximilian Esders et al.
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Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
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RC1: 'Comment on egusphere-2023-1025', Anonymous Referee #1, 20 Jul 2023
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2023/egusphere-2023-1025/egusphere-2023-1025-RC1-supplement.pdf
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RC2: 'Comment on egusphere-2023-1025', Anonymous Referee #2, 04 Aug 2023
Enders et al. investigate the wind movement of microplastics in the wind tunnel using different sized polyethylene (PE) and borosilicate (GL) microspheres, the latter as a reference mimicking dust (or maybe better sand) particles. The study is very timely: microplastics and their atmospheric transport have become a focus of research, yet the mechanism of their entrainment from a land/soil surface into the atmosphere is not yet well understood. By comparing the aeolian transport of microplastic with that of mineral dust – which, even though there are still important gaps in our understanding of dust emission as well, can build on a body of research of several decades – the authors take an important step in trying to advance the process understanding of microplastic emission.
The manuscript is well written overall and most results are well explained. However, I do see some conceptual and experimental design aspects, which need clarification. I detail those together with some other aspects in the following. I hope that my comments will help to further improve the study and make it even more relevant and insightful.
Major comments:
- Rather than placing the test microspheres, either PE or GL, on e.g. a soil substrate, the authors use a glass plate as a substrate. A glass plate, different to a “natural” surface (meaning a surface in the outside environment), is very smooth. While I understand that this eases implementation of the experiment, it has two important disadvantages: i) the microspheres will roll off the (very, very small) field of observation rather than lift off; ii) in the case of a soil surface, e.g. a desert, no interaction between microplastics and soil particles (sand/dust) can be considered. Point ii) may not be relevant for other surfaces, such as asphalt. Point i), however, is very important in my opinion, because the mechanism relevant for long-term atmospheric transport of microplastics is suspension and not creep. The authors touch upon this topic somewhat when discussing the expression for wind erosion threshold by Shao and Lu (2000) [I would like to add that this is not a wind erosion model, contrary to what is stated in the text], which is primarily addressing saltation (l. 212 – 225). I therefore wonder why the authors chose this experimental design, which does not address the target emission mechanism. Related to that, the primary emission mechanism of mineral dust is saltation bombardment (e.g. Shao et al., 1993; Shao, 2008; Kok et al., 2012). Is this also expected to be the main emission mechanism for microplastics (note that it requires microplastic particles to impact upon, hence for plastic/plastic collisions a relatively large abundance of microplastics on a surface is needed; less so for sand/plastic collisions) or – due to the lower density – maybe aerodynamic entrainment (e.g. Klose et al., 2014)? And what is the effect of the often very non-spherical shape of microplastics on their emission? Why did the authors choose to study the movement threshold of two spherical particle types with main difference being their density (which has been investigated in previous studies; e.g. Corn and Stein, 1965; Iversen and White, 1982; etc.) over the other questions? I believe this requires a more detailed conceptual discussion and justification. Also, previous experimental studies that investigated the wind transport of different-density particles should be discussed more.
- I find the terminology of individual critical friction velocity, critical friction velocity, and threshold friction velocity unfortunate, given that it does not seem to agree with that used in the wind erosion / aeolian research community. Also, the benefit of defining the critical friction velocity as that for 25% detached particles and threshold friction velocity as 50% detached particles is not clear to me. Please consider using a comparable terminology. Note also that the aeolian research community differentiates between the fluid and impact thresholds, the latter accounting for particle collisions (e.g. Kok et al., 2012) and that threshold friction velocity is primarily used in the context of saltation.
- Please add more detail on the experiments, e.g. how many experiments have been conducted in total, how many replicates for each substrate/microsphere type, etc. In line 145 it is only mentioned “over 30 runs”. Those should be defined exactly.
- It is noted that the substrate is placed on top of the roughness elements, which are ~1 cm (?) high and that the aerodynamic roughness length is 0.5 mm. From my perspective this means that the substrate and particles are not actually at the surface, but elevated? How does this impact the accuracy of the derived values of friction velocity for the height of the substrate?
- Generally, as commented upon above, the comparison with mineral dust throughout the manuscript is somehow problematic as only creep is considered in the experiments and not suspension, even though I understand that the ultimate ambition is to compare with mineral dust transport. Also, the size of the used mineral dust analogue, GL69, is not in the typical dust size range, but would be giant mineral dust or sand.
Technical comments:
- Title: Both the words “transport” and “mineral dust” are misleading, because they indicate long-term transport, whereas the processes considered experimentally in the present study are (short-term) creep of sand-sized particles.
- L 1 add “can” after “Atmospheric transport”
- L 2 Knowing all the challenges associated with mineral dust transport (e.g. related with particle shape), I would very much argue that long-range transport of microplastics is not at all well-known. The author in fact state the same in line 44.
- L 3 contrasted them
- L 10-11 The statement that collisions can both enhance and mitigate detachment needs more explanation, otherwise it is not understandable without context.
- L 14 borosilicate instead of mineral microspheres
- L 15 fitting to the prediction of the wind erosion threshold friction velocity (adapt to the terminology used in the paper; cf. comment (2)
- L 19-20 The conclusion made here is not justified by the paper’s results. Suggest removing.
- L 56 “driving the emission”
- L 65-66 I assume that rHc refers to the relative humidity in air. With “water accumulating”, do you mean that the water vapor condenses on the microspheres and substrates?
- L 76 define subscript i (if you stick to this terminology)
- L 78-79 The behavior of the microspheres would likely be quite different if they were “embedded” in a rough substrate, rather than resting on top of a smooth plate.
- L 83 collisions can lead (compare next sentence)
- L 86-88 check grammar for i) and ii) (To what extent do collisions influence …; Do the findings support …)
- L 88 Doesn’t the finding of a preferential support of microplastics explicitly relate to the concomitant entrainment of both sand/dust and microplastics (e.g. Bullard et el., 2021) rather than the density-dependent entrainment (here movement) friction velocity threshold? For the latter, as mentioned before, I strongly recommend to discuss more of the previous study on this topic.
- L 108 Where/which height is the free-stream velocity measured?
- L 112 10 s appear like a very long interval to track particle movement. Was a higher temporal frequency not possible or was this interval chosen on purpose? Please comment on this choice.
- Sec 2.2, line 1: Should the Fig. reference be to Fig. A3?
- L 120 Related to the previous comment, by counting only the remaining number of particles, it is impossible to know the detachment mechanism. Was the movement of the microspheres not observed/recorded in some way?
- Table 1: Please add substrate material
- Sec 2.5, line before second equation (the line numbering seems off here): The authors mention that a logistic function was fit to the experimental results, but – unless I overlooked it – it is never shown how well this fit matches the results. Please give more information so that the reader can understand the accuracy of the fit. On another note, it is not clear to me why A/2 in the equation is replaced by m, but I leave this to authors’ preference.
- L 153 Do I understand correctly that u*th is defined as the friction velocity at which – in one entire experiment – 50% of all particles have detached / are remaining? It is not determined as detachment of 50% of all microsphere at one given time/friction velocity interval, right? The wording is not entirely clear. Please also comment on how this definition relates to the threshold friction velocity used in wind erosion research. On another note, in line 182, the critical friction velocity is defined as that friction velocity at which 25% of the particles detached. Why are two different particle number threshold (25% and 50%) used? The purpose is not clear to me.
- L 155-157 See also Shao and Klose (2016, https://doi.org/10.1016/j.aeolia.2016.08.004)
- Sec 2.7, line 1: The critical friction velocity is here defined as for “multiple microspheres”, which I interpret as for a population of microspheres. I find this somehow misleading though and would argue that u*c, especially in the context of the estimate by Shao and Lu (2000) is the average critical (or threshold) friction velocity.
- Sec 2.7 lines 3-4: It is important to say, as also discussed by the authors later on, that Shao and Lu (2000) assume that particles are resting on top of each other, contrary to the monolayer of particles considered here. I suggest to rephrase the sentence “We assume that a glass plate … represents a simplified soil” accordingly.
- L 178-179 It is important to note here that both Ravi et al. and McKenna Neuman et al. determined this threshold for saltation as measured by, e.g. impact sensors.
- L 195 A smaller u*th for CIM at low u*th seems indeed only applicable for rolling and sliding motions, because then the fluid motion can be inhibited by blocking stationary particles. It does not apply to a hopping motion, because then the blocking does not apply and lifting is determined by the fluid forces alone.
- L 204 d < 100 um (70 um) < d is not a mathematically correct formulation, because d cannot at the same time be smaller and larger than a reference. Please revise.
- L 209 It is quite surprising that a lower threshold/critical friction velocity than estimated by Shao and Lu (2000) is only found for two types of microspheres, even though a lower threshold is expected for rolling compared to lifting. How do you explain that?
- L 212 I think a better formulation than “overpredicts u*c compared to our observations” would be “it is conceivable that we obtain lower u*c from our experiments than predicted by…”. “Overpredict” creates the notion that the estimate by Shao and Lu (2000) is wrong, whereas the difference here is at a first instance due to a different assumed setting.
- L 228 It seems that the effect of nano-scale surface roughness has received attention particularly in the context of capillary forces (e.g. Rabinovich et al, 2002; Kim et al., 2016). It is correct though that it is not considered in the Shao and Lu model. I think this topic is very interesting, however, I would argue that it is of second order importance compared to differences between the shape of “natural” compared to spherical particles, which may be even more important for microplastics compared to sand/dust.
- L 230-231 The last sentence is not clear. Suggest revising.
- Figures: Please explain how the error range has been calculated.
- L 246-248 It seems that the variability of u*th with rH is quite diverse. How do the authors explain that u*th is not always increasing with rH? Is there any further insight from the experiments on the cause of this? I believe a somewhat more detailed discussion would be insightful.
- Please list references in a systematic order, e.g. chronological (recommended) or alphabetical.
- Fig. 5 Please add explanation for the circles and triangles in all figures / figure captions.
- L 262 decreases with increasing theta_s
- L 268-269 Would an indication for the occurrence of capillary forces be meant to be due to a variation in rH? The context of this statement is not quite clear.
- L 270 which showed instead of showing
- L 276 particle surface roughness
- L 274 – 277 Please see my initial comments on aspects which from my perspective are more pressing and more tailored to advancing understanding of the entrainment of microplastics.
- L 278-280 I find that this passage does not summarize the results very precisely. I strongly recommend to be more specific on the achievements made in this study, in particular define what is meant by detachment behavior.
- L 282 I would not agree that the agreement confirms that a glass plate equipped with a monolayer of microspheres represents a simplified soil. Please see my earlier similar comment and rephrase the sentence accordingly.
- L 283-285 As mentioned in my comment 1, mineral dust is entrained either through saltation as intermediate mechanism or directly aerodynamically by wind. What is studied here for microplastics is the initiation of creep, which does not yet allow to conclude that the behavior of microplastics is similar to that of dust, in particular considering that saltation (to entrain dust) is driven by sand grains which are (not exactly, but somewhat) spherical. This may not apply in the same way to microplastics, or does it? The smaller density of microplastics compared to dust may certainly play a role, but without knowing the emission mechanism, its roll cannot be conclusively determined (e.g. spherical microplastics may entrain smaller particles less efficiently through saltation than sand does, do to the lower density).
- L 285 Similarly as in the abstract, the last sentence is not supported by the study results as suspension is not (yet) investigated.
- A3: should “(see A3)” be “(see Fig. A3)“?; also lines 329-330 are the same as in the main text.
- A4: I suggest to place all four panels side-by-side such that the magnitudes can be compared more easily. It seems that there is enough space for that.
- There is no reference to Appendices A5 to A7 in the main text.
- L 333 There is no pseudocode in this section. Suggest calling it procedure instead.
- A6: This section is not understandable for someone who has not used this technique before. Please add some more detail, also to Figs. A7 and A8.
Citation: https://doi.org/10.5194/egusphere-2023-1025-RC2 - AC1: 'Comment on egusphere-2023-1025', Eike Esders, 20 Oct 2023
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
| : Report abuse
-
RC1: 'Comment on egusphere-2023-1025', Anonymous Referee #1, 20 Jul 2023
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2023/egusphere-2023-1025/egusphere-2023-1025-RC1-supplement.pdf
-
RC2: 'Comment on egusphere-2023-1025', Anonymous Referee #2, 04 Aug 2023
Enders et al. investigate the wind movement of microplastics in the wind tunnel using different sized polyethylene (PE) and borosilicate (GL) microspheres, the latter as a reference mimicking dust (or maybe better sand) particles. The study is very timely: microplastics and their atmospheric transport have become a focus of research, yet the mechanism of their entrainment from a land/soil surface into the atmosphere is not yet well understood. By comparing the aeolian transport of microplastic with that of mineral dust – which, even though there are still important gaps in our understanding of dust emission as well, can build on a body of research of several decades – the authors take an important step in trying to advance the process understanding of microplastic emission.
The manuscript is well written overall and most results are well explained. However, I do see some conceptual and experimental design aspects, which need clarification. I detail those together with some other aspects in the following. I hope that my comments will help to further improve the study and make it even more relevant and insightful.
Major comments:
- Rather than placing the test microspheres, either PE or GL, on e.g. a soil substrate, the authors use a glass plate as a substrate. A glass plate, different to a “natural” surface (meaning a surface in the outside environment), is very smooth. While I understand that this eases implementation of the experiment, it has two important disadvantages: i) the microspheres will roll off the (very, very small) field of observation rather than lift off; ii) in the case of a soil surface, e.g. a desert, no interaction between microplastics and soil particles (sand/dust) can be considered. Point ii) may not be relevant for other surfaces, such as asphalt. Point i), however, is very important in my opinion, because the mechanism relevant for long-term atmospheric transport of microplastics is suspension and not creep. The authors touch upon this topic somewhat when discussing the expression for wind erosion threshold by Shao and Lu (2000) [I would like to add that this is not a wind erosion model, contrary to what is stated in the text], which is primarily addressing saltation (l. 212 – 225). I therefore wonder why the authors chose this experimental design, which does not address the target emission mechanism. Related to that, the primary emission mechanism of mineral dust is saltation bombardment (e.g. Shao et al., 1993; Shao, 2008; Kok et al., 2012). Is this also expected to be the main emission mechanism for microplastics (note that it requires microplastic particles to impact upon, hence for plastic/plastic collisions a relatively large abundance of microplastics on a surface is needed; less so for sand/plastic collisions) or – due to the lower density – maybe aerodynamic entrainment (e.g. Klose et al., 2014)? And what is the effect of the often very non-spherical shape of microplastics on their emission? Why did the authors choose to study the movement threshold of two spherical particle types with main difference being their density (which has been investigated in previous studies; e.g. Corn and Stein, 1965; Iversen and White, 1982; etc.) over the other questions? I believe this requires a more detailed conceptual discussion and justification. Also, previous experimental studies that investigated the wind transport of different-density particles should be discussed more.
- I find the terminology of individual critical friction velocity, critical friction velocity, and threshold friction velocity unfortunate, given that it does not seem to agree with that used in the wind erosion / aeolian research community. Also, the benefit of defining the critical friction velocity as that for 25% detached particles and threshold friction velocity as 50% detached particles is not clear to me. Please consider using a comparable terminology. Note also that the aeolian research community differentiates between the fluid and impact thresholds, the latter accounting for particle collisions (e.g. Kok et al., 2012) and that threshold friction velocity is primarily used in the context of saltation.
- Please add more detail on the experiments, e.g. how many experiments have been conducted in total, how many replicates for each substrate/microsphere type, etc. In line 145 it is only mentioned “over 30 runs”. Those should be defined exactly.
- It is noted that the substrate is placed on top of the roughness elements, which are ~1 cm (?) high and that the aerodynamic roughness length is 0.5 mm. From my perspective this means that the substrate and particles are not actually at the surface, but elevated? How does this impact the accuracy of the derived values of friction velocity for the height of the substrate?
- Generally, as commented upon above, the comparison with mineral dust throughout the manuscript is somehow problematic as only creep is considered in the experiments and not suspension, even though I understand that the ultimate ambition is to compare with mineral dust transport. Also, the size of the used mineral dust analogue, GL69, is not in the typical dust size range, but would be giant mineral dust or sand.
Technical comments:
- Title: Both the words “transport” and “mineral dust” are misleading, because they indicate long-term transport, whereas the processes considered experimentally in the present study are (short-term) creep of sand-sized particles.
- L 1 add “can” after “Atmospheric transport”
- L 2 Knowing all the challenges associated with mineral dust transport (e.g. related with particle shape), I would very much argue that long-range transport of microplastics is not at all well-known. The author in fact state the same in line 44.
- L 3 contrasted them
- L 10-11 The statement that collisions can both enhance and mitigate detachment needs more explanation, otherwise it is not understandable without context.
- L 14 borosilicate instead of mineral microspheres
- L 15 fitting to the prediction of the wind erosion threshold friction velocity (adapt to the terminology used in the paper; cf. comment (2)
- L 19-20 The conclusion made here is not justified by the paper’s results. Suggest removing.
- L 56 “driving the emission”
- L 65-66 I assume that rHc refers to the relative humidity in air. With “water accumulating”, do you mean that the water vapor condenses on the microspheres and substrates?
- L 76 define subscript i (if you stick to this terminology)
- L 78-79 The behavior of the microspheres would likely be quite different if they were “embedded” in a rough substrate, rather than resting on top of a smooth plate.
- L 83 collisions can lead (compare next sentence)
- L 86-88 check grammar for i) and ii) (To what extent do collisions influence …; Do the findings support …)
- L 88 Doesn’t the finding of a preferential support of microplastics explicitly relate to the concomitant entrainment of both sand/dust and microplastics (e.g. Bullard et el., 2021) rather than the density-dependent entrainment (here movement) friction velocity threshold? For the latter, as mentioned before, I strongly recommend to discuss more of the previous study on this topic.
- L 108 Where/which height is the free-stream velocity measured?
- L 112 10 s appear like a very long interval to track particle movement. Was a higher temporal frequency not possible or was this interval chosen on purpose? Please comment on this choice.
- Sec 2.2, line 1: Should the Fig. reference be to Fig. A3?
- L 120 Related to the previous comment, by counting only the remaining number of particles, it is impossible to know the detachment mechanism. Was the movement of the microspheres not observed/recorded in some way?
- Table 1: Please add substrate material
- Sec 2.5, line before second equation (the line numbering seems off here): The authors mention that a logistic function was fit to the experimental results, but – unless I overlooked it – it is never shown how well this fit matches the results. Please give more information so that the reader can understand the accuracy of the fit. On another note, it is not clear to me why A/2 in the equation is replaced by m, but I leave this to authors’ preference.
- L 153 Do I understand correctly that u*th is defined as the friction velocity at which – in one entire experiment – 50% of all particles have detached / are remaining? It is not determined as detachment of 50% of all microsphere at one given time/friction velocity interval, right? The wording is not entirely clear. Please also comment on how this definition relates to the threshold friction velocity used in wind erosion research. On another note, in line 182, the critical friction velocity is defined as that friction velocity at which 25% of the particles detached. Why are two different particle number threshold (25% and 50%) used? The purpose is not clear to me.
- L 155-157 See also Shao and Klose (2016, https://doi.org/10.1016/j.aeolia.2016.08.004)
- Sec 2.7, line 1: The critical friction velocity is here defined as for “multiple microspheres”, which I interpret as for a population of microspheres. I find this somehow misleading though and would argue that u*c, especially in the context of the estimate by Shao and Lu (2000) is the average critical (or threshold) friction velocity.
- Sec 2.7 lines 3-4: It is important to say, as also discussed by the authors later on, that Shao and Lu (2000) assume that particles are resting on top of each other, contrary to the monolayer of particles considered here. I suggest to rephrase the sentence “We assume that a glass plate … represents a simplified soil” accordingly.
- L 178-179 It is important to note here that both Ravi et al. and McKenna Neuman et al. determined this threshold for saltation as measured by, e.g. impact sensors.
- L 195 A smaller u*th for CIM at low u*th seems indeed only applicable for rolling and sliding motions, because then the fluid motion can be inhibited by blocking stationary particles. It does not apply to a hopping motion, because then the blocking does not apply and lifting is determined by the fluid forces alone.
- L 204 d < 100 um (70 um) < d is not a mathematically correct formulation, because d cannot at the same time be smaller and larger than a reference. Please revise.
- L 209 It is quite surprising that a lower threshold/critical friction velocity than estimated by Shao and Lu (2000) is only found for two types of microspheres, even though a lower threshold is expected for rolling compared to lifting. How do you explain that?
- L 212 I think a better formulation than “overpredicts u*c compared to our observations” would be “it is conceivable that we obtain lower u*c from our experiments than predicted by…”. “Overpredict” creates the notion that the estimate by Shao and Lu (2000) is wrong, whereas the difference here is at a first instance due to a different assumed setting.
- L 228 It seems that the effect of nano-scale surface roughness has received attention particularly in the context of capillary forces (e.g. Rabinovich et al, 2002; Kim et al., 2016). It is correct though that it is not considered in the Shao and Lu model. I think this topic is very interesting, however, I would argue that it is of second order importance compared to differences between the shape of “natural” compared to spherical particles, which may be even more important for microplastics compared to sand/dust.
- L 230-231 The last sentence is not clear. Suggest revising.
- Figures: Please explain how the error range has been calculated.
- L 246-248 It seems that the variability of u*th with rH is quite diverse. How do the authors explain that u*th is not always increasing with rH? Is there any further insight from the experiments on the cause of this? I believe a somewhat more detailed discussion would be insightful.
- Please list references in a systematic order, e.g. chronological (recommended) or alphabetical.
- Fig. 5 Please add explanation for the circles and triangles in all figures / figure captions.
- L 262 decreases with increasing theta_s
- L 268-269 Would an indication for the occurrence of capillary forces be meant to be due to a variation in rH? The context of this statement is not quite clear.
- L 270 which showed instead of showing
- L 276 particle surface roughness
- L 274 – 277 Please see my initial comments on aspects which from my perspective are more pressing and more tailored to advancing understanding of the entrainment of microplastics.
- L 278-280 I find that this passage does not summarize the results very precisely. I strongly recommend to be more specific on the achievements made in this study, in particular define what is meant by detachment behavior.
- L 282 I would not agree that the agreement confirms that a glass plate equipped with a monolayer of microspheres represents a simplified soil. Please see my earlier similar comment and rephrase the sentence accordingly.
- L 283-285 As mentioned in my comment 1, mineral dust is entrained either through saltation as intermediate mechanism or directly aerodynamically by wind. What is studied here for microplastics is the initiation of creep, which does not yet allow to conclude that the behavior of microplastics is similar to that of dust, in particular considering that saltation (to entrain dust) is driven by sand grains which are (not exactly, but somewhat) spherical. This may not apply in the same way to microplastics, or does it? The smaller density of microplastics compared to dust may certainly play a role, but without knowing the emission mechanism, its roll cannot be conclusively determined (e.g. spherical microplastics may entrain smaller particles less efficiently through saltation than sand does, do to the lower density).
- L 285 Similarly as in the abstract, the last sentence is not supported by the study results as suspension is not (yet) investigated.
- A3: should “(see A3)” be “(see Fig. A3)“?; also lines 329-330 are the same as in the main text.
- A4: I suggest to place all four panels side-by-side such that the magnitudes can be compared more easily. It seems that there is enough space for that.
- There is no reference to Appendices A5 to A7 in the main text.
- L 333 There is no pseudocode in this section. Suggest calling it procedure instead.
- A6: This section is not understandable for someone who has not used this technique before. Please add some more detail, also to Figs. A7 and A8.
Citation: https://doi.org/10.5194/egusphere-2023-1025-RC2 - AC1: 'Comment on egusphere-2023-1025', Eike Esders, 20 Oct 2023
Eike Maximilian Esders et al.
Eike Maximilian Esders et al.
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Latest update: 01 Dec 2023
Short summary
We asked, Is the transport of plastic dust via air different from mineral dust? We observed plastic and mineral particles in a wind tunnel and measured at what wind speeds the particles start to move. The results show that plastic and mineral particles smaller than 70 µm behave similarly. For bigger particles, plastic particles move more easily, as they weigh less. We conclude that it is no surprise, that like mineral dust, plastic dust is found all around the globe, transported via air.
We asked, Is the transport of plastic dust via air different from mineral dust? We observed...