the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
| 09 Sep 2025
Continuous in situ monitoring of the vertical and horizontal passage of a labeled-water pulse through a boreal Scots pine forest
Abstract. Water labeled with stable isotopes provides a conservative tracer, being neither produced nor consumed, for water flowpaths within soils and root systems. We added a strong, evenly distributed 2HHO label to one m2 of soil surface and continuously monitored its passage downward into the soil and upward into the stems of surrounding trees, with the objective of illuminating spatiotemporal lateral root water uptake and overlap. The study was conducted during the historic drought of 2018 in a mature Scots pine (Pinus sylvestris) forest growing on sandy soil in northern Sweden. Continuous in situ isotopic measurements of tree xylem water evidenced root system overlap of six trees within the labeled square meter. This result is consistent with previous estimates from labelled nutrient uptake measurements at this site. However, label uptake differed sharply among trees, even within the same radius; 90 % of the label was taken up by one of the two trees closest to the labelled plot. Horizontal transport rates in tree roots averaged 0.17 ± 0.05 m d-1, meaning that the arrival of label pulse in tree stems was delayed by 6–33 days from first tree to last. Root water uptake by trees appeared restricted to the upper 60 cm of mineral soil, even at the peak of the drought. Label intensity of the mineral soil weakened throughout the drought, consistent with the notion that the label was being dispersed or diluted. Labeled water recovery was low (3–4 %), and we hypothesize that this was due to a significant upward flux of water into the organic surface horizons. Our data provide a daily and three-dimensional description of the passage of a labeled water pulse, highlighting the heterogeneity in horizontal water transport flowpaths and the uneven partitioning of label among individual trees in a boreal forest.
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- CC1: 'Comment on egusphere-2025-3025', Richard Keim, 11 Sep 2025 reply
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- 1
This manuscript presents results of a field experiment to identify root water uptake using isotopically labelled irrigation. The measurement techniques are state of the art, which is to say that they are difficult to implement and interpret. The results are satisfyingly clear in terms of temporal behavior of isotopic composition of soil water and sap, and the experiment is thus a rare opportunity to quantify processes that are difficult to observe. The strength of the results lies in the spatial observations of tree water uptake, and the weakness is the mass conservation estimates. Some improvements in mass conservation estimation might reduce some of the considerable uncertainty that derives from recovering less than 5% of the tracer.
L162 “UD” does not appear in Eq 1, and is later defined as something else (L167). Please move L168 to L162.
L171 what is the exact scope of this non-evaporation assumption? For example, do the berry bushes count in the reported LAI or not? Also, mosses are a nontrivial pathway for E (e.g., Heijmans et al. Global Biogeochem Cycles 2004). Finally, Fig 4b, 5a pre-labeling lce<0 and vertical profiles of 2H both suggest soil evaporation (though there are also other possible explanations for these conditions). If the flux tower data and pre-labeling soil isotopic profiles are not sufficient to resolve the soil/moss/understory(?) E flux component, some rough, literature-based or isotope-based estimates would be helpful for estimating biases introduced by assuming it to be zero.
What is the likely magnitude of downward unsaturated flux—i.e., to a zone below the soil moisture sensors? If unaccounted for, this flux would give upward bias to estimates of water consumption in upper layers—more bias the shallower the layer.
Fig 1 shows 8 trees within 4 m of the injection. This is a tree-dense part of the forest. What does this mean for extrapolation of the results to the stand scale?
L198 the whole-tree-bore equilibration method causes samples to equilibrate with all water along the hole, whereas the tree water might be dominated by recent uptake only at the outer few mm of xylem. Just as Marshall et al (2000) addressed this, it would be helpful to add some discussion of the likely magnitude of this effect in this experiment.
I think the Label Recovery section of the discussion more properly belongs in the results. Also, what are the consequences for the soil depth uptake calculations of accepting some alternative hypotheses about the fate of the unrecovered 95%+ of tracer?
Fig 6 and its caption could be improved to explain the meaning of “days after labelling”—day of first observation? Also, isn’t it more logical to swap the axes?
Are there no measurements of the monitored trees available? I expect differences in rooting and uptake might be related to things like relative crown size and sapwood area.