新疆孔雀河流域地下水演化及其生态效应

龙睿, 张俊, 余堃, 顾小凡, 李瑛, 董佳秋, 苏潇, 朱瑾. 新疆孔雀河流域地下水演化及其生态效应[J]. 水文地质工程地质, 2023, 50(6): 41-50. doi: 10.16030/j.cnki.issn.1000-3665.202305032
引用本文: 龙睿, 张俊, 余堃, 顾小凡, 李瑛, 董佳秋, 苏潇, 朱瑾. 新疆孔雀河流域地下水演化及其生态效应[J]. 水文地质工程地质, 2023, 50(6): 41-50. doi: 10.16030/j.cnki.issn.1000-3665.202305032
LONG Rui, ZHANG Jun, YU Kun, GU Xiaofan, LI Ying, DONG Jiaqiu, SU Xiao, ZHU Jin. Groundwater evolution and ecological effect in the Kongque River Basin, Xinjiang[J]. Hydrogeology & Engineering Geology, 2023, 50(6): 41-50. doi: 10.16030/j.cnki.issn.1000-3665.202305032
Citation: LONG Rui, ZHANG Jun, YU Kun, GU Xiaofan, LI Ying, DONG Jiaqiu, SU Xiao, ZHU Jin. Groundwater evolution and ecological effect in the Kongque River Basin, Xinjiang[J]. Hydrogeology & Engineering Geology, 2023, 50(6): 41-50. doi: 10.16030/j.cnki.issn.1000-3665.202305032

新疆孔雀河流域地下水演化及其生态效应

  • 基金项目: 第三次新疆综合科学考察项目(2022xjkk0300);陕西省创新能力支持计划项目(2019TD-040);陕西省自然科学基础研究计划项目(2022JQ-271;2022JQ-238);国家自然科学基金项目(41877199;42302301);陕西省重点研发计划项目(2021ZDLSF05-01;2022SF-327);中国地质调查局地质调查项目(DD20190351;DD20221751)
详细信息
    作者简介: 龙睿(1994 -),男,硕士,助理工程师,主要从事西北地区水文地质研究。E-mail:752194828@qq.com
    通讯作者: 张俊(1982 -),男,博士,正高级工程师,主要从事西北地区水文地质研究。E-mail:36170038@qq.com
  • 中图分类号: P641.8

Groundwater evolution and ecological effect in the Kongque River Basin, Xinjiang

More Information
  • 近50 a,西北干旱内陆河流域经历了历史时期的水土资源过度开发和近期的生态保护修复的不同阶段,对区域地下水和生态环境产生了重要影响,但地下水长期演化规律及其生态效应认识尚不清晰。以新疆孔雀河流域为典型研究区,基于最新地下水监测数据与历史数据对比,分析流域地下水流场时空演化规律以及流域地下水对河岸带胡杨林的影响作用,探讨地下水长期演化的生态效应。结果表明:1971—2021年,孔雀河流域因过量集中开采地下水引起区域地下水流动系统发生根本性变化,地下水水位整体呈下降趋势,流域内累计降幅大于40 m的面积达204.69 km2,累计降幅20~40 m的面积为1735.81 km2,累计降幅5~20 m的面积为1018.56 km2,并形成地下水降落漏斗;生态输水前,中下游河道长时间断流,河岸带地下水水位埋深累计降幅超过10 m,导致河岸带胡杨林退化萎缩,2016年实施生态输水工程以后,埋深逐渐上升2~4 m,上升至胡杨林生长临界水位以上,2014—2018年天然胡杨林植被覆盖率增大17%。本研究有助于认识西北干旱内陆河流域地下水和生态环境演化规律,为类似区域地下水可持续开发利用与生态保护提供科学参考。

  • 加载中
  • 图 1  研究区示意图及监测点、断面分布图

    Figure 1. 

    图 2  孔雀河流域 A - A′ 南北向水文地质剖面图

    Figure 2. 

    图 3  1971和2021年地下水水位等值线与埋深分区

    Figure 3. 

    图 4  1971—2021年地下水水位变幅

    Figure 4. 

    图 5  301、302、303和304监测孔地下水水位埋深年际变化

    Figure 5. 

    图 6  漏斗范围内典型监测孔2019年地下水埋深变化

    Figure 6. 

    图 7  孔雀河流域下游胡杨林分布区NDVI的变化特征(修改自Zhang等[36]

    Figure 7. 

    图 8  河流-地下水关系剖面

    Figure 8. 

    表 1  孔雀河流域下游胡杨林分布区NDVI的变化特征(修改自Zhang等[36]

    Table 1.  Variation characteristics of NDVI of the Populus euphratica forest in the lower reaches of the Kongque River Basin (modified from Zhang et al.[36])

    土地类型 INDVI变化范围 分布区域面积变化率/%
    2014年 2016年 2018年
    荒漠裸地
    INDVI≤0 77.87 75.94 61.41
    草地、灌木、低密度胡杨林
    0< INDVI≤0.05 19.47 19.73 35.57
    中等密度胡杨林
    0.05< INDVI≤0.1 2.10 3.21 2.65
    高密度胡杨林
    0.1< INDVI≤0.2 0.54 1.03 0.35
    耕地
    INDVI >0.2 0.02 0.09 0.02
    下载: 导出CSV
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出版历程
收稿日期:  2023-05-14
修回日期:  2023-07-17
刊出日期:  2023-11-15

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