Quantifying river water contributions to the transpiration of riparian trees along a losing river: lessons from stable isotopes and an iteration method

IF 5.7 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Hydrology and Earth System Sciences Pub Date : 2023-09-26 DOI:10.5194/hess-27-3405-2023
Yue Li, Ying Ma, Xianfang Song, Qian Zhang, Lixin Wang
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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.
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量化河流水对失去河流沿岸树木蒸腾的贡献:来自稳定同位素和迭代方法的经验教训
摘要河流水在丧失河流的河岸植物用水和河岸生态系统恢复(即河流水补给地下地下水)中起着至关重要的作用。如何量化不同地下水位下河流水对河岸植物蒸腾的贡献以及植物水分利用效率的相关响应是一个巨大的挑战。本研究对北京潮白河流域深根滨水垂柳(Salix babylonica L.)在2019年(旱年)和2021年(丰水年)进行了水(δ2H和δ18O)、222Rn和叶片δ13C的稳定同位素观测。我们提出了一种结合MixSIAR模型的迭代方法,量化了河川水对巴比伦河蒿蒸腾的贡献及其与地下水位深度和叶片δ13C的相关性。结果表明,滨水巴比伦螺对深层(80 ~ 170 cm土层和地下水)的吸收量为56.5%±10.8%。补给河岸深水的河水为间接水源,对失去河流附近的河岸树木蒸腾贡献了20.3%的水分。当地下水位从2019年干旱年的2.7 m增加到2021年湿润年的1.7 m时,河岸树木的河流吸水量显著增加(7.0%),叶片δ13C显著降低(- 2.0‰)(p<0.05)。较高的水分有效度可能促进了气孔的开放,从而增加了蒸腾水分的损失,导致叶片δ13C在湿润年比干燥年降低。河水对河滨巴比伦杉蒸腾的贡献与地下水位深度和叶片δ13C呈负线性相关(p<0.01)。不断上升的地下水位可能会增加从地下水和/或河流中提取的水量,并产生一种消耗河岸树木的河流用水模式,这可能对河流流量和河岸植被的保护产生不利影响。该研究为理解地下水-土壤-植物-大气连续体中的水循环机制以及管理水资源和沿河流的河岸造林提供了新的见解。
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来源期刊
Hydrology and Earth System Sciences
Hydrology and Earth System Sciences 地学-地球科学综合
CiteScore
10.10
自引率
7.90%
发文量
273
审稿时长
15 months
期刊介绍: Hydrology and Earth System Sciences (HESS) is a not-for-profit international two-stage open-access journal for the publication of original research in hydrology. HESS encourages and supports fundamental and applied research that advances the understanding of hydrological systems, their role in providing water for ecosystems and society, and the role of the water cycle in the functioning of the Earth system. A multi-disciplinary approach is encouraged that broadens the hydrological perspective and the advancement of hydrological science through integration with other cognate sciences and cross-fertilization across disciplinary boundaries.
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