摘要
陕北地区生态环境脆弱,大规模的煤炭开采又加速了水资源流失,但是很难定量计算其影响程度。以陕北窟野河流域为例,通过机理分析创造性地提出了将煤炭开采对区域内水资源的影响分为三部分:地下水静储量破坏、地下水动储量破坏和采空区积水,分别计算了各部分的水量;并采用邻近流域进行了流量对比分析。结果表明:窟野河流域煤炭开采造成的地下水静储量破坏值为1.38×10~8m^3,采空区形成2.72×10~8m^3的积水,2011年地下水动储量破坏达到了0.62×10~8m^3。以秃尾河流域作为参证流域,计算出窟野河1999-2013年平均还原流量为13.22 m^3·s^(-1),比实测径流量大2.28×10~8m^3。为了减少煤炭开采过程中水资源的损耗量,窟野河流域必须加大对采空区积水和矿井排水的综合利用。
In northern Shaanxi Province,China,the ecological environment is poor and the water resource is inadequate. The large-scale coal mining accelerated the loss of water,but how to quantitatively calculate the influence degree is a research hotspot both at home and abroad. Taking the Kuye River basin in northern Shaanxi as an example,this paper creatively put forward that influences of coal mining on regional water resources can be divided into three parts：（1）Destruction of groundwater static reserves： because roof fall happened in the process of coal mining,the water originally stored in the aquifer was emptied in a short time,the destruction effects was permanent and irreversible.（2）Goaf water storage： after the aquifer was destructed,a large amount of surface water and aquifer water flowed into the goaf through cracks,some goaf water＇s storage time maybe long and some maybe short.（3）Destruction of groundwater dynamic reserves：part of the goaf water was expelled out well,and called as mine water gushing,which can not been drunk by human and animal because of pollution. In order to get the amount of the water damaged by coal mining in watershed,the three parts of water resources was calculated respectively and summed. Next,taking the nearby Tuwei River as compared basin,this paper further calculated the Kuye River natural flow in coal mining period by area ratio method and measured flow ratio in base periods method. The results show that：by 2011,Kuye River groundwater static reserves damaged by coal mining was 1.38 × 10~8m^3,goaf water storage was 2.72×10~8m^3,and groundwater dynamic reserves destruction（mine water gushing） in 2011 reached 0.62×10~8m^3,each unit coal consumed about 0.6 m3 water. Taking the nearby Tuwei River as Compared basin,Kuye River natural flow was 17.06 m^3·s^（-1）in 1980-1998,which was 0.44×10~8m^3higher than the measured runoff;and in 1999-2013 the natural flow was 13.22 m^3·s^（-1）,which is 2.28×10~8m^3higher than the measured runoff. This reduced runoff was mainly caused by soil and water conservation,coal mining,increased production and living water and other factors of Kuye River basin. Finally this paper put forward some measures that helped reduce water resources depletion caused by coal mining in Kuye River.Above all,coal mining is the main reason for water resources reduction in Kuye River basin,and the comprehensive utilization of goaf water and mine drainage must be enhance in future. The new method proposed in this paper,not only has sufficient theoretical basis,but also has simple calculation process,which can be quantitatively used to evaluate the influence of coal mining on water resources in most regions of China.
出处
《干旱区地理》
CSCD
北大核心
2016年第2期246-253,共8页
Arid Land Geography
基金
陕西省自然科学基金(2014JM2-5063)
西北旱区生态水利工程国家重点实验室开放基金(2013KFKT-3)
关键词
陕北地区
煤炭开采
水资源
地下水
定量识别
参证流域
northern Shaanxi
coal mining
water resources
groundwater
quantitative recognition
compared basin
作者简介
吴喜军（1979-），男，陕西榆林人，博士，副教授，主要从事矿区水资源保护和水污染控制方面的研究．Email：wxj0826@163．com
