CAJ | 학술논문

地下水是指储存在地面以下饱和岩土孔隙、裂隙及溶洞的水。地下水资源量是指某时段内地下含水层接收降水、地表水体、侧向径流及人工回灌等项渗透补给量的总和。其中，地表水体渗透补给量由湖泊（水库、坑塘）周边渗透补给量、河道及渠系渗透补给量和田间灌溉入渗补给量组成。对无资料地区通常采用临近站地形、地貌等相似的地区借用其现有的水文资料来计算地下水资源量。文章对此进行探讨研究。
지하수시지저존재지면이하포화암토공극、렬극급용동적수。지하수자원량시지모시단내지하함수층접수강수、지표수체、측향경류급인공회관등항삼투보급량적총화。기중，지표수체삼투보급량유호박（수고、갱당）주변삼투보급량、하도급거계삼투보급량화전간관개입삼보급량조성。대무자료지구통상채용림근참지형、지모등상사적지구차용기현유적수문자료래계산지하수자원량。문장대차진행탐토연구。
Groundwater is stored below ground pore,fissure and cave in rock and soil saturated water.Groundwater resources amount refers to total amount of water for aquifers receiving precipitation, surface water,lateral runoff and artificial recharge,infiltration recharge in a period.Among them,the surface water is consisted of infiltration recharge by the lake (reservoir,pool)surrounding infiltration recharge,river and canal seepage recharge and irrigation infiltration recharge.But for the area without data,the data near the area,the similar terrain landform,nearby stations are borrowed to calculate the groundwater resources amount.