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白宜斐, 王 弋, 陈亚宁, 梁建辉, 向燕芸.叶尔羌河流域灌区地下水埋深变化及影响因素分析水资源与水工程学报[J].,2019,30(6):242-249
叶尔羌河流域灌区地下水埋深变化及影响因素分析
Variation of groundwater depth and its influencing factors in the irrigated area of the Yarkant River Basin
  
DOI:10.11705/j.issn.1672-643X.2019.06.37
中文关键词:  地下水埋深  影响因子  敏感系数  相对贡献率  叶尔羌河流域灌区
英文关键词:groundwater depth  influencing factor  sensitivity coefficient  ralative contribution rate  irrigation area of Yarkant River Basin
基金项目:国家自然科学基金项目(Y771071001)
作者单位
白宜斐1,2, 王 弋1, 陈亚宁1, 梁建辉3, 向燕芸1,2 (1.中国科学院 新疆生态与地理研究所, 荒漠与绿洲生态国家重点实验室, 新疆 乌鲁木齐 8300112.中国科学院大学, 北京 100049 3.喀什水文勘测局 新疆 喀什 844000) 
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中文摘要:
      选取叶尔羌河灌区中3个子灌区(莎车、巴楚和麦盖提灌区)的35眼地下水位观测井的月观测数据以及径流量、降水量、实际蒸散发、地表水灌溉用水量和地下水开采量等数据,基于敏感性分析和相对贡献率研究灌区2006-2017年地下水埋深变化及导致其变化的主导因子。结果表明:在3个子灌区中,地下水埋深变化最大的为巴楚灌区,莎车子和麦盖提灌区的地下水埋深波动较小;相比莎车子灌区,巴楚和麦盖提灌区地下水埋深受农业生产季节的影响更为显著;叶尔羌河灌区地下水埋深加深的主导因子是地下水的超采,且与灌区的地理位置有关。
英文摘要:
      This study selected the monthly data of thirty-five groundwater observation wells located in three representative sub-irrigation areas (Shache, Bachu and Maigaiti irrigation areas), and used five influencing factors, including runoff, precipitation, actual evapotranspiration, irrigation water amount, groundwater exploitation. The variations of groundwater depth (GWD) in the irrigated area from 2006 to 2017 and its leading factors were studied based on sensitivity analysis and relative contribution rate. The results showed that the variation of GWD of Bachu sub-irrigated area was the biggest compared to the two other sub-irrigated areas. The GWD of Bachu and Maigaiti sub-irrigated areas were susceptible to the season changes than Shache sub-irrigated area. The main influencing factor of groundwater depth change in the Yarkant River irrigation area is over-exploitation of groundwater, and is also related to the geographical location of the sub-irrigation area.
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