Quantifying river water contributions to the transpiration of riparian trees along a losing river: lessons from stable isotopes and an iteration method
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Published:2023-09-26
Issue:18
Volume:27
Page:3405-3425
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ISSN:1607-7938
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Container-title:Hydrology and Earth System Sciences
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language:en
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Short-container-title:Hydrol. Earth Syst. Sci.
Author:
Li Yue, Ma Ying, Song Xianfang, Zhang Qian, Wang LixinORCID
Abstract
Abstract. River water plays a critical role in riparian
plant water use and riparian ecosystem restoration along losing rivers
(i.e., river water recharging underlying groundwater). How to quantify the
contributions of river water to the transpiration of riparian plants under
different groundwater levels and the related responses of plant water use
efficiency is a great challenge. In this study, observations of stable isotopes of water (δ2H and δ18O), 222Rn, and leaf
δ13C were conducted for the deep-rooted riparian weeping willow
(Salix babylonica L.) in 2019 (dry year) and 2021 (wet year) along the Chaobai River in
Beijing, China. We proposed an iteration method in combination with the
MixSIAR model to quantify the river water contribution to the transpiration
of riparian S. babylonica and its correlations with the water table depth and leaf
δ13C. Our results demonstrated that riparian S. babylonica took up deep
water (in the 80–170 cm soil layer and groundwater) by 56.5 % ± 10.8 %. River water recharging riparian deep water was an indirect water
source and contributed 20.3 % of water to the transpiration of riparian
trees near the losing river. Significantly increasing river water uptake (by
7.0 %) and decreasing leaf δ13C (by
−2.0 ‰) of riparian trees were observed as the water
table depth changed from 2.7 m in the dry year of 2019 to 1.7 m in the wet
year of 2021 (p<0.05). The higher water availability probably
promoted stomatal opening and thus increased transpiration water loss,
leading to the decreasing leaf δ13C in the wet year compared to
the dry year. The river water contribution to the transpiration of riparian
S. babylonica was found to be negatively linearly correlated with the water table depth
and leaf δ13C (p<0.01). The rising groundwater level
may increase the water extraction from the groundwater and/or river and produce a
consumptive river-water-use pattern of riparian trees, which can have an
adverse impact on the conservation of both river flow and riparian
vegetation. This study provides new insights into understanding the
mechanisms of the water cycle in a groundwater–soil–plant–atmosphere
continuum and managing water resources and riparian afforestation along
losing rivers.
Funder
National Natural Science Foundation of China National Key Research and Development Program of China
Publisher
Copernicus GmbH
Subject
General Earth and Planetary Sciences,General Engineering,General Environmental Science
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