不同地表水流频率对塔克拉玛干沙漠腹地柽柳用水特性的影响

IF 5.9 1区 地球科学 Q1 ENGINEERING, CIVIL
Tingting Zhang , Yue Dai , Anwar Abdureyim , Jiabing Kang
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引用次数: 0

摘要

柽柳(Tamarix ramosissima)是沙漠生态系统中的优势物种,也是干旱地区的生态屏障物种,在稳定沙丘和防止荒漠化方面发挥着至关重要的作用。本研究于 2023 年 7 月和 10 月在位于塔克拉玛干沙漠腹地克里雅河尾部的达利亚博依绿洲的三个地点采集了河水、地下水、土壤水和柽柳个体样本。这三个地点分别称为达利亚博依绿洲的中部(SE)、西部(SW)和北部(SN),每个地点都经历了不同频率的洪水。东南部站点在七月和十月经历了洪水,西南部站点仅在七月经历了洪水,而北部站点在七月和十月没有经历洪水。分析了水样和植物样本中氢、氧稳定同位素和线条件过量(lc-excess)的时空变化,并通过氢、氧稳定同位素和 MixSIAR 模型分析了 T. ramosissima 水利用的潜在变化。结果表明,东南部、西南部和西南部地点的 SWL 斜率在 7 月份(分别为 6.77、6.42 和 3.05)高于 10 月份(分别为 7.37、3.30 和 2.14)。东南部站点的 lc-excess 值未出现季节性变化;只有西南部和西南部站点的土壤水 lc-excess 值出现了季节性变化。MixSIAR 结果表明,东南部地点洪水事件频繁,7 月和 10 月 T. ramosissima 对水源的利用比例相对稳定。此外,浅层土壤水(0-60 厘米)和深层土壤水(60-80 厘米)是东南部 ramosissima 的主要水源。在 SN 地点,由于受到地表水的轻微影响,T. ramosissima 对水源利用的变化在统计学上并不显著。事实上,深层土壤水(60-200 厘米)和地下水是该地点 T. ramosissima 的水源。与 10 月份不同的是,西南部地点在 7 月份发生了洪水事件,导致苎麻在 7 月份和 10 月份分别利用了浅层土壤水(0-60 厘米)和深层土壤水(60-280 厘米)。不同的地表水流模式导致苎麻不同的水分利用特征,这进一步证明了苎麻具有较强的恢复能力和生态可塑性。这项工作为在达利亚博伊绿洲及类似干旱生境实施有效的生态水运输措施提供了有益的参考。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Effects of different surface water flow frequencies on water use characteristics of Tamarix ramosissima in the hinterland of the Taklamakan Desert
Tamarix ramosissima is a dominant species in desert ecosystems and an ecological barrier species in arid areas, playing a crucial role in stabilizing dunes and preventing desertification. In this study, river water, groundwater, soil water, and T. ramosissima individual samples were collected from three sites in July and October 2023 at the Daliyaboyi Oasis located at the tail of the Kriya River in the hinterland of the Taklamakan Desert. The three sites are referred to as the center (SE), west (SW), and north (SN) sites within the Daliyaboyi Oasis, and each experienced different flood frequencies. The SE site experienced flooding in July and October, the SW site experienced flooding only in July, and the SN site experienced no flooding in July or October. The spatial and temporal variation in hydrogen and oxygen stable isotopes and line-conditional excess (lc-excess) in water and plant samples were analyzed, and the potential changes in water use of T. ramosissima were analyzed by the hydrogen and oxygen stable isotope and MixSIAR model. The findings indicated that the slope of SWL at the SE, SW, and SN sites was higher in July (6.77, 6.42, and 3.05, respectively) than in October (7.37, 3.30, and 2.14, respectively). The lc-excess value of the SE site did not exhibit seasonal changes; only the lc-excess values of soil water in SW and SN sites showed seasonal changes. MixSIAR results indicated frequent flood events at the SE site, with relatively constant proportions of water source utilization by T. ramosissima in July and October. In addition, shallow soil water (0–60 cm) and deeper soil water (60–80 cm) were the main water sources of T. ramosissima at SE. The SN site was slightly influenced by surface water, resulting in statistically non-significant changes in the water source utilization by T. ramosissima. Indeed, deep soil water (60–200 cm) and groundwater were the sources of water for T. ramosissima at this site. In contrast with October, the SW site experienced flood events in July, resulting in the utilization of water by T. ramosissima from the shallow soil (0–60 cm) and deep soil (60–280 cm) in July and October, respectively. Different surface water flow patterns led to different water use characteristics of T. ramosissima, which further demonstrated that T. ramosissima has high resilience and ecological plasticity. This work provides a useful reference for the implementation of effective ecological water transport measures in the Daliyaboyi Oasis and similar arid habitats.
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来源期刊
Journal of Hydrology
Journal of Hydrology 地学-地球科学综合
CiteScore
11.00
自引率
12.50%
发文量
1309
审稿时长
7.5 months
期刊介绍: The Journal of Hydrology publishes original research papers and comprehensive reviews in all the subfields of the hydrological sciences including water based management and policy issues that impact on economics and society. These comprise, but are not limited to the physical, chemical, biogeochemical, stochastic and systems aspects of surface and groundwater hydrology, hydrometeorology and hydrogeology. Relevant topics incorporating the insights and methodologies of disciplines such as climatology, water resource systems, hydraulics, agrohydrology, geomorphology, soil science, instrumentation and remote sensing, civil and environmental engineering are included. Social science perspectives on hydrological problems such as resource and ecological economics, environmental sociology, psychology and behavioural science, management and policy analysis are also invited. Multi-and interdisciplinary analyses of hydrological problems are within scope. The science published in the Journal of Hydrology is relevant to catchment scales rather than exclusively to a local scale or site.
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