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The impact of mining-related human activities on runoff in northern Shaanxi, China

机译:与采矿有关的人类活动对陕北地区径流的影响

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摘要

Northern Shaanxi, a major coal base in China, is facing water scarcity, soil erosion, and ecological deterioration. We chose the Kuye and Tuwei Rivers as the study area, in which many underground mining bases have operated in these catchments since the late 1980s. The objective of this study was to quantify the anthropogenic impacts of runoff on the main rivers in the mining region. First, trend analysis and change-point detection were used to examine changes in the magnitude of annual runoff. Then, the contributions of precipitation changes and human activities to runoff changes were distinguished. Linear regression and comparative analysis were used to quantify the extents of human impacts on the runoff in two representative catchments. The results showed that the annual runoff in both catchments decreased significantly at the 99 confidence level during 1960-2016. The significant change in the runoff occurred in 1997 in the Kuye River (KYH) catchment because of coal mining, while it occurred in 1980 in the Tuwei River (TWH) catchment due to soil and water conservation measures. The contribution of human activities to the runoff change was estimated to account for 91 and 42 in the KYH catchment and TWH catchment, respectively, whereas climate change accounted for 9 and 58, respectively. Moreover, by reconstructing the time series of runoff, we surmise that anthropogenic interventions lead to a decrease in the average annual runoff by 168-344 million m~3 (in the KYH catchment) and 152 million m~3 (in the TWH catchment), respectively, during the descending period (1997-2016).
机译:陕北是中国主要的煤炭基地,正面临缺水、水土流失和生态恶化的问题。我们选择库野河和土渭河作为研究区,自1980年代后期以来,许多地下采矿基地一直在这些集水区运营。本研究的目的是量化径流对矿区主要河流的人为影响。首先,采用趋势分析和变化点检测方法检验年径流量级变化;然后,区分了降水变化和人类活动对径流变化的贡献;采用线性回归和比较分析来量化人类对两个代表性集水区径流的影响程度。结果表明,1960—2016年,两个流域的年径流量均在99%置信水平下显著下降。1997年,由于煤矿开采,库野河(KYH)流域发生了径流的显著变化,而1980年,由于水土保持措施,土魏河(TWH)流域发生了径流的显著变化。据估计,人类活动对径流变化的贡献分别占KYH流域和TWH流域的91%和42%,而气候变化分别占9%和58%。此外,通过重建径流时间序列,我们推测在下降期(1997-2016年),人为干预导致年平均径流量分别减少168-3.44亿m~3(KYH流域)和1.52亿m~3(TWH流域)。

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