Deep roots mitigate drought impacts on tropical trees despite limited quantitative contribution to transpiration
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Author
Kühnhammer, K.van Haren, J.
Kübert, A.
Bailey, K.
Dubbert, M.
Hu, J.
Ladd, S.N.
Meredith, L.K.
Werner, C.
Beyer, M.
Affiliation
Biosphere 2, University of ArizonaHonors College, University of Arizona
School of Natural Resources and the Environment, University of Arizona
Issue Date
2023-10-01Keywords
Biosphere 2Drought resistance
Plant-water relations
Root water uptake depth
Water content
Water stable isotopes
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Elsevier B.V.Citation
Kühnhammer, K., van Haren, J., Kübert, A., Bailey, K., Dubbert, M., Hu, J., ... & Beyer, M. (2023). Deep roots mitigate drought impacts on tropical trees despite limited quantitative contribution to transpiration. Science of the Total Environment, 893, 164763.Journal
Science of the Total EnvironmentRights
© 2023 The Author. Published by Elsevier B.V. This is an open access article under the CC BY-NC-ND license (https://creativecommons.org/licenses/by-nc-nd/4.0/).Collection Information
This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.Abstract
Deep rooting is considered a central drought-mitigation trait with vast impact on ecosystem water cycling. Despite its importance, little is known about the overall quantitative water use via deep roots and dynamic shifts of water uptake depths with changing ambient conditions. Knowledge is especially sparse for tropical trees. Therefore, we conducted a drought, deep soil water labeling and re-wetting experiment at Biosphere 2 Tropical Rainforest. We used in situ methods to determine water stable isotope values in soil and tree water in high temporal resolution. Complemented by soil and stem water content and sap flow measurements we determined percentages and quantities of deep-water in total root water uptake dynamics of different tree species. All canopy trees had access to deep-water (max. uptake depth 3.3 m), with contributions to transpiration ranging between 21 % and 90 % during drought, when surface soil water availability was limited. Our results suggest that deep soil is an essential water source for tropical trees that delays potentially detrimental drops in plant water potentials and stem water content when surface soil water is limited and could hence mitigate the impacts of increasing drought occurrence and intensity as a consequence of climate change. Quantitatively, however, the amount of deep-water uptake was low due to the trees' reduction of sap flow during drought. Total water uptake largely followed surface soil water availability and trees switched back their uptake depth dynamically, from deep to shallow soils, following rainfall. Total transpiration fluxes were hence largely driven by precipitation input. © 2023 The AuthorsNote
Open access articleISSN
0048-9697PubMed ID
37308023Version
Final Published Versionae974a485f413a2113503eed53cd6c53
10.1016/j.scitotenv.2023.164763
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Except where otherwise noted, this item's license is described as © 2023 The Author. Published by Elsevier B.V. This is an open access article under the CC BY-NC-ND license (https://creativecommons.org/licenses/by-nc-nd/4.0/).
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