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黄河流域地下水储量变化的时空动态。

Spatio-temporal dynamics of groundwater storage changes in the Yellow River Basin.

机构信息

Department of Natural Resources Sciences, McGill University, 21111, Lakeshore Road, Ste-Anne-de-Bellevue, QC, H9X 3V9, Canada.

School of Environmental Sciences, University of Guelph, 50 Stone Road East, Guelph, ON, N1G 2W1, Canada.

出版信息

J Environ Manage. 2019 Apr 1;235:84-95. doi: 10.1016/j.jenvman.2019.01.016. Epub 2019 Jan 21.

Abstract

Groundwater is an important source of water supply and ecosystem resilience. However, limited information on spatio-temporal dynamics makes a complete assessment of available groundwater resources difficult, impairing sustainable water management. The Gravity Recovery and Climate Experiment mission (GRACE) has recently made this possible. In this study, we used the Yellow River Basin (YRB) as a model system to explore the use of spatio-temporal dynamics information about groundwater change derived from the GRACE datasets for regional groundwater management. While there was an overall decreasing trend (R = 0.57) during the last 14 year, the groundwater storage over the whole basin decreased significantly (p < 0.0001, slope changed from -0.0137 cm/month to -0.0684 cm/month) since 2010 (2010-2016) and showed stronger fluctuations than the time before (2003-2009). The range and the standard deviation of groundwater storage change also increased in recent years especially after 2010. At the basin scale, locations which exhibited higher variabilities (large standard deviation) over time generally showed radical decrease of groundwater storage. The results indicated that groundwater depletion may reduce the aquifers' function for ecosystem resilience, thus posing risks to the ecosystem of the YRB and threatening its people to climate change and extreme events. Despite the overall trend, the changes were heterogeneous if looking at finer scales: spatially, there was a gradual decline of storage from west to east (e.g. the change in December 2016 was -3.6, -9.1 and -25.8 cm for the upper, middle and lower reach, respectively); and temporally, the timeseries among the reaches were significantly different (p = 0.023). Our hotspot analysis also indicated the heterogeneity in groundwater decline across the basin and through the time. Additionally, it showed that human factors (e.g. groundwater consumption) become dominant in determining the groundwater change pattern over climatic variations. We therefore call for more attention to groundwater in developing sustainable water management strategies and suggest a closer cooperation of neighboring provinces in the YRB to have a reciprocal strategic plan for water regulation, protection, and management.

摘要

地下水是供水和生态系统恢复的重要水源。然而,由于缺乏时空动态方面的信息,难以对现有地下水资源进行全面评估,从而影响可持续水资源管理。最近,“重力恢复与气候实验”(GRACE)任务使这成为可能。在这项研究中,我们以黄河流域(YRB)为模型系统,探索利用 GRACE 数据集提供的地下水变化时空动态信息进行区域地下水管理。尽管在过去 14 年中存在整体下降趋势(R=0.57),但整个流域的地下水储量自 2010 年以来显著减少(p<0.0001,斜率从-0.0137cm/月变为-0.0684cm/月),且波动幅度比之前更大(2003-2009 年)。近年来,地下水储量变化的范围和标准差也有所增加,尤其是 2010 年以后。在流域尺度上,随着时间的推移,表现出较高变异性(较大标准差)的位置通常会导致地下水储量的急剧减少。结果表明,地下水枯竭可能会降低含水层对生态系统恢复的功能,从而对黄河流域的生态系统构成威胁,并使其面临气候变化和极端事件的威胁。尽管存在总体趋势,但如果从更精细的尺度来看,变化是不均匀的:从空间上看,地下水储量从西向东逐渐减少(例如,2016 年 12 月,上游、中游和下游的变化分别为-3.6、-9.1 和-25.8cm);从时间上看,各河段之间的时间序列存在显著差异(p=0.023)。我们的热点分析还表明,整个流域和整个时间范围内的地下水下降存在不均匀性。此外,它还表明,在确定地下水变化模式时,人类因素(如地下水消耗)比气候变化更为重要。因此,我们呼吁在制定可持续水资源管理战略时更加关注地下水,并建议黄河流域各邻省加强合作,制定相互协调的水资源调控、保护和管理战略。

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