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首页> 外文期刊>Journal of Hydrology: Regional Studies >Bi-decadal groundwater level trends in a semi-arid south indian region: Declines, causes and management
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Bi-decadal groundwater level trends in a semi-arid south indian region: Declines, causes and management

机译:半干旱南印度地区双年代际地下水位趋势:下降,成因与管理

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Study region Three districts in crystalline aquifer region of semi-arid south India. Study focus India, world’s largest groundwater user (250 billion m 3 yr ?1 ) has been reported to experience declining groundwater levels. However, the statistical significance of the decline has not been analyzed to separate human effects from natural variability. Trends in groundwater levels in three administrative districts of south India were analyzed and explained through changes in irrigation, rainfall, and agricultural power subsidy. New hydrological insights for the region Contrary to common perception of widespread groundwater declines only 22–36% of the wells showed statistically significant declines. The use of well depth during dry well periods may slightly underestimate the number of declining wells (by 1%) and rate of decline. Increase in groundwater irrigated area combined with rainfall and power subsidy policy, were the main causative factors for the decline. Groundwater decline after implementation of free-electricity policy in 2004 confirmed the nexus between power subsidy and groundwater. These declines are likely to worsen due to future well drillings. Trends in other regions with similar hydro-geologic conditions need to be analyzed to verify groundwater declines and its linkages with power subsidy. Once established, reforms in power subsidy and well permit policy along with conversion to efficient micro–irrigation may be needed to maintain or enhance groundwater availability in the crystalline aquifer region of India (240 million ha).
机译:研究区域印度南部半干旱的结晶含水层区域中的三个地区。研究重点据报道,印度是世界上最大的地下水消费国(2500亿立方米yr 3年),其地下水位正在下降。但是,尚未对下降的统计意义进行分析以将人类影响与自然变异性区分开。通过灌溉,降雨和农业电力补贴的变化,对印度南部三个行政区的地下水位趋势进行了分析和解释。该地区的新水文见解与普遍认为的地下水广泛下降相反,只有22–36%的井显示出统计上的显着下降。在干井期使用井深度可能会略微低估下降井的数量(下降1%)和下降速度。地下水灌溉面积增加,加上降雨和电力补贴政策,是造成灌溉面积减少的主要原因。 2004年实施免费电力政策后,地下水的下降证实了电力补贴与地下水之间的联系。由于未来的钻井作业,这些下降可能会加剧。需要分析其他具有类似水文地质条件的地区的趋势,以验证地下水的下降及其与电力补贴的联系。一旦建立,可能需要进行电力补贴和许可政策的改革,以及转换为有效的微灌,以维持或提高印度结晶含水层地区(2.4亿公顷)的地下水供应。

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