CAJ | 학술논문

本文在分析降水与地下水埋深关系的基础上，采用地下水位波动法研究兴隆庄采煤塌陷区蓄水与地下水的补给规律，得出研究区地下水补给量的变化规律为从东北向西南递减，与地下水流向基本一致；补给量随降水量增大而增大，但在降水量增大到一定程度后变化趋于平稳，与地下水埋深的关系则为先增后减；将塌陷前后地下水补给量进行对比，表明塌陷后地下水对塌陷区蓄水有较大补给作用。此研究成果可为塌陷区蓄水与地下水的综合开发利用提供重要参考。
본문재분석강수여지하수매심관계적기출상，채용지하수위파동법연구흥륭장채매탑함구축수여지하수적보급규률，득출연구구지하수보급량적변화규률위종동북향서남체감，여지하수류향기본일치；보급량수강수량증대이증대，단재강수량증대도일정정도후변화추우평은，여지하수매심적관계칙위선증후감；장탑함전후지하수보급량진행대비，표명탑함후지하수대탑함구축수유교대보급작용。차연구성과가위탑함구축수여지하수적종합개발이용제공중요삼고。
Based on the analysis of the relationship between the rainfall and groundwater depth on the groundwater recharge, the water-table fluctuation method was adopted in this paper to estimate the groundwater recharge around Xinglongzhuang coal mining subsidence area. This paper reached a conclusion that the changes of groundwater recharge amount decreased from northeast to southwest, and basically the same as the groundwater flow. The groundwater recharge generally increased with rainfall, however, as the rainfall increases to a certain extent, the change trend will not increase obviously, but the relationship with the buried depth of groundwater is first increased and then decreased. Meanwhile, the comparison of groundwater recharge before and after the collapse shows that the subsidence area will be recharged by groundwater after the collapse. The research results can provide an important reference for the comprehensive development and utilization of water in the subsidence area.