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在水分限制的干旱荒漠生态系统中,旱生灌木林冠层将总降雨量分为穿透雨和树干流时,降雨量的同位素组成会发生变化。

Alteration in isotopic composition of gross rainfall as it is being partitioned into throughfall and stemflow by xerophytic shrub canopies within water-limited arid desert ecosystems.

机构信息

Shapotou Desert Research and Experiment Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 320 Donggang West Road, Lanzhou 730000, China.

Shapotou Desert Research and Experiment Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 320 Donggang West Road, Lanzhou 730000, China.

出版信息

Sci Total Environ. 2019 Nov 20;692:631-639. doi: 10.1016/j.scitotenv.2019.07.294. Epub 2019 Jul 19.

Abstract

Isotopic composition of gross rainfall has been extensively used as a conservative tracer to track water movement and other hydrological processes in vegetated ecosystems. Recent studies from forest ecosystems, however, demonstrated that vegetation canopies can alter the isotopic composition of rainwater during rainfall partitioning into throughfall and stemflow, likely leading to errors and biases in aforementioned studies. No known studies, to date, had investigated this topic in shrub-dominated arid and semi-arid ecosystems where water is typically the driving factor in ecological, hydrological and biogeochemical processes. In this study, event-based gross rainfall, the throughfall and stemflow induced by shrubs of Caragana korshinskii were measured and samples were collected within a water-limited arid desert ecosystem of northern China, and their water stable isotopes (O and H) were also analyzed in the laboratory. We mainly aimed to investigate whether there is an isotopic enrichment or depletion in stemflow and throughfall in comparison to gross rainfall, and to evaluate the possible underlying mechanisms. Our results indicated an enrichment of both isotopes in stemflow, while a general more depletion in throughfall than in gross rainfall, which is presumably affected by a combinative effects of canopy evaporation, isotopic exchange, and selective canopy storage. Deuterium excess of stemflow were found to be significantly higher (P < 0.05) than that of gross rainfall and throughfall. Moreover, we detected the pronounced "amount effect", with a significant (P < 0.05) negative relationship between isotopic composition and the amount of gross rainfall, throughfall, and stemflow, respectively. Our study is expected to contribute to an improved understanding of physical processes and water routing in shrub canopies within vast arid desert ecosystems.

摘要

总降雨量的同位素组成已被广泛用作示踪剂,以追踪植被生态系统中的水分运移和其他水文过程。然而,最近来自森林生态系统的研究表明,在降雨分配为穿透雨和茎流的过程中,植被冠层可以改变雨水的同位素组成,这可能导致上述研究中的误差和偏差。迄今为止,尚无已知研究调查过在以灌木为主的干旱和半干旱生态系统中这一主题,在这些生态系统中,水通常是生态、水文和生物地球化学过程的驱动因素。在这项研究中,我们在一个受水资源限制的中国北方干旱荒漠生态系统中,测量了基于事件的总降雨量、沙拐枣灌木引起的穿透雨和茎流,并收集了样本,同时在实验室中分析了它们的稳定同位素(O 和 H)。我们主要旨在研究与总降雨量相比,茎流和穿透雨是否存在同位素富集或贫化,并评估可能的潜在机制。我们的研究结果表明,同位素在茎流中都有富集,而穿透雨则普遍比总降雨量更贫化,这可能是受冠层蒸发、同位素交换和选择性冠层储存的综合影响。我们发现茎流的氘过剩值明显高于(P < 0.05)总降雨量和穿透雨。此外,我们检测到明显的“数量效应”,即同位素组成与总降雨量、穿透雨和茎流的数量之间存在显著的(P < 0.05)负相关关系。我们的研究有望有助于更好地理解广阔干旱荒漠生态系统中灌木冠层的物理过程和水分运移。

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