都基众, 赵杰, 邢树文. 沈阳市城区地下水位的变化与控制[J]. 地质与资源, 2006, 15(1): 62-66. DOI: 10.13686/j.cnki.dzyzy.2006.01.011
    引用本文: 都基众, 赵杰, 邢树文. 沈阳市城区地下水位的变化与控制[J]. 地质与资源, 2006, 15(1): 62-66. DOI: 10.13686/j.cnki.dzyzy.2006.01.011
    DU Ji-zhong, ZHAO Jie, XING Shu-wen. GROUND WATER TABLE CHANGING AND CONTROL IN SHENYANG CITY[J]. Geology and Resources, 2006, 15(1): 62-66. DOI: 10.13686/j.cnki.dzyzy.2006.01.011
    Citation: DU Ji-zhong, ZHAO Jie, XING Shu-wen. GROUND WATER TABLE CHANGING AND CONTROL IN SHENYANG CITY[J]. Geology and Resources, 2006, 15(1): 62-66. DOI: 10.13686/j.cnki.dzyzy.2006.01.011

    沈阳市城区地下水位的变化与控制

    GROUND WATER TABLE CHANGING AND CONTROL IN SHENYANG CITY

    • 摘要: 沈阳是一个以地下水为主要供水水源的城市,区域地下水降落漏斗自上世纪60年代初形成,至1989年漏斗面积达225.79 km2.由于采取限制开采措施,90年代初开始,沈阳市降落漏斗逐步得到恢复.地下水位的升高带来地下建筑被淹等新的环境地质问题.应采取有效措施,将地下水位控制在适当的高度,在保护地质环境的同时,合理开发地下水资源.

       

      Abstract: The water supply in Shenyang City is mainly depended on groundwater. The groundwater depression was firstly appear in 1960s, and developed to an area of 225.79 km2 by 1989. Thanks to some measures such as the limitation to groundwater discharge, the depression has been reducing since 1990s. However, new problems occurred with the water table rising continuously, even to the extent that some underground buildings were flooded. Thus it is necessary to control the water table on a certain height, so as to utilize the groundwater and protect the environmental resources scientifically.

       

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