Water sources of major plant species along a strong climatic gradient in the inland Heihe River Basin-Reference-Cited by-同舟云学术

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Water sources of major plant species along a strong climatic gradient in the inland Heihe River Basin

Published:2020-09-01 Issue:1-2 Volume:455 Page:439-466
ISSN:0032-079X
Container-title:Plant and Soil
language:en
Short-container-title:Plant Soil

Author:

Zhao Liangju,Xie Cong,Liu Xiaohong,Wang Ninglian,Yu Zhang,Dong Xiying,Wang Lixin

Funder

National Natural Science Foundation of China

National Key Research and Development Program of China

Opening Foundation of State Key Laboratory of Continental Dynamics, Northwest University

Division of Earth Sciences of National Science Foundation

President’s International Research Awards from Indiana University

Publisher

Springer Science and Business Media LLC

Subject

Plant Science,Soil Science

Link

https://link.springer.com/content/pdf/10.1007/s11104-020-04639-5.pdf

Reference51 articles.

1. Allison GB, Hughes MW (1983) The use of natural tracers as indicators of soil-water movement in a temperate semi-arid region. J Hydrol 60:157–173. https://doi.org/10.1016/0022-1694(83)90019-7

2. Barbeta A, Jones SP, Clavé L, Wingate L, Gimeno TE, Fréjaville B, Wohl S, Ogée J (2019) Unexplained hydrogen isotope offsets complicate the identification and quantification of tree water sources in a riparian forest. Hydrol Earth Syst Sci 23:2129–2146. https://doi.org/10.5194/hess-23-2129-2019

3. Barnes CJ, Allison GB (1988) Tracing of water movement in the unsaturated zone using stable isotopes of hydrogen and oxygen. J Hydrol 100:143–176

4. Bowen GJ, Putman A, Brooks JR, Bowling DR, Oerter EJ, Good SP (2018) Inferring the source of evaporated waters using stable H and O isotopes. Oecologia 187:1025–1039. https://doi.org/10.1007/s00442-018-4192-5

5. Brooks JR, Barnard HR, Coulombe R, McDonnell JJ, Renée Brooks J, Barnard HR, Coulombe R, McDonnell JJ (2010) Ecohydrologic separation of water between trees and streams in a Mediterranean climate. Nat Geosci 3:100–104. https://doi.org/10.1038/ngeo722

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