院报 ›› 2019, Vol. 36 ›› Issue (9): 46-50,63.DOI: 10.11988/ckyyb.20180225

• 水资源与环境 • 上一篇    下一篇

高开采强度下库尔勒市地下水位埋深动态与影响因素浅析

魏兴1,2,周金龙1,2,曾妍妍1,2,冯书同3,王燕3   

  1. 1.新疆农业大学 水利与土木工程学院,乌鲁木齐 830052;
    2.新疆水文水资源工程技术研究中心,乌鲁木齐 830052;
    3.新疆巴音郭楞蒙古自治州国土资源局,新疆 库尔勒 841000
  • 收稿日期:2018-03-12 修回日期:2018-04-27 出版日期:2019-09-01 发布日期:2019-09-12
  • 通讯作者: 周金龙(1964-),男,浙江龙游人,教授,博士,博士生导师,主要从事干旱区地下水利用与保护、灌区土壤水-盐运移监测与模拟等研究。E-mail:zjzhoujl@163.com
  • 作者简介:魏 兴(1993-),男,安徽阜阳人,博士研究生,主要从事干旱区地下水资源评价方面的研究。E-mail:1035027480@qq.com
  • 基金资助:
    国家自然科学基金-新疆联合基金重点支持项目(U1403282);新疆自治区“十三五”重点学科建设高峰学科-水利工程学科基金项目(xjslgcgfxk20161103)

Dynamics and Influence Factors of Groundwater Depth in Korla with Intensive Exploitation

WEI Xing1,2,ZHOU Jin-long1,2,ZENG Yan-yan1,2,FENG Shu-tong3,WANG Yan3   

  1. 1.College of Water Conservancy and Civil Engineering, Xinjiang Agricultural University, Urumqi 830052, China;
    2.Xinjiang Hydrology and Water Resources Engineering Research Center, Urumqi 830052, China;
    3.Land Resource Bureau of Bayingol Mongolian Autonomous Prefecture, Korla 841000, China
  • Received:2018-03-12 Revised:2018-04-27 Online:2019-09-01 Published:2019-09-12

摘要: 库尔勒市社会经济快速发展对水资源的需求使其地下水开发经历了临界超采期(2000—2006年)、超采增长期(2007—2011年)和高位超采稳定期(2012—2015年)过程。为探究高开采强度下的地下水位埋深动态特征,以库尔勒市地下水监测网覆盖区作为研究区,对以上3个开采强度时段地下水位埋深进行线性趋势分析。所有监测井地下水位埋深均呈持续增大趋势,研究区2000—2011年地下水位埋深总体呈“加速”增大状态;2012—2015年转变为“减速”增大状态。地下水长期超采已使山前倾斜平原地下水位埋深累计增大4.10~12.67 m,冲积平原累计增大9.07~22.26 m,天然生态受到威胁。逐步回归分析表明,研究区监测井地下水位埋深与径流量呈负相关关系,与地下水开采量呈正相关关系,径流量、开采量实质是研究区地下水补给项与排泄项的综合反映。地下水位埋深持续增大是地下水补给量减少、地下水开采强度增大共同作用的结果。研究成果可为库尔勒市水资源开发利用与保护提供一定的参考。

关键词: 地下水位埋深, 地下水高开采强度, 线性趋势分析, 径流量, 开采量, 库尔勒市

Abstract: Due to high demand of water resources posed by rapid socio-economic development, the exploitation of groundwater depth experienced periods of critical overexploitation (2000 to 2006), intensifying overexploitation (2007 to 2011), and stable high overexploitation (2012 to 2015). Linear trend analysis of groundwater depth during the aforementioned three periods elucidated that the groundwater depth of all monitoring wells continued to decline. From 2000 to 2011, the drawdown of groundwater level in the study area accelerated in general, and from 2012 to 2015, the decline attenuated. The long-term overexploitation of groundwater had made groundwater depth in piedmont sloping plain declined by 4.10-12.67 m, and in alluvial plain declined by 9.07-22.26 m, threatening the natural ecology. Stepwise regression analysis showed that the groundwater depth was negatively correlated with runoff and positively correlated with groundwater exploitation, and both were the comprehensive reflection of groundwater recharge and discharge in the study area. The continuous drawdown of groundwater level was caused by the joint action of the reduction of groundwater recharge and the increase of groundwater exploitation intensity.

Key words: groundwater depth, high intensity of groundwater exploitation, linear trend analysis, runoff, exploitation amount, Korla

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