地下水
地下水
지하수
GROUNDWATER
2014年
4期
153-153,162
,共2页
地表水资源量%计算方法%水资源管理%依据
地錶水資源量%計算方法%水資源管理%依據
지표수자원량%계산방법%수자원관리%의거
surface water resources%calculation method%water resources management%basis
地表水资源量是指河流、湖泊、冰川等地表水体中由当地降水形成的、可以逐年更新的动态水量,用河川天然径流量表示,阐述区域地表水资源量的计算方法,分析了地表水资源量及其分布规律,为加强水资源管理,掌握水资源动态,为决策部门对水资源调度、利用提供依据。
地錶水資源量是指河流、湖泊、冰川等地錶水體中由噹地降水形成的、可以逐年更新的動態水量,用河川天然徑流量錶示,闡述區域地錶水資源量的計算方法,分析瞭地錶水資源量及其分佈規律,為加彊水資源管理,掌握水資源動態,為決策部門對水資源調度、利用提供依據。
지표수자원량시지하류、호박、빙천등지표수체중유당지강수형성적、가이축년경신적동태수량,용하천천연경류량표시,천술구역지표수자원량적계산방법,분석료지표수자원량급기분포규률,위가강수자원관리,장악수자원동태,위결책부문대수자원조도、이용제공의거。
As surface water resources refer to precipitation stored in rivers, lakes and glaciers, it varies year from year and is always be expressed by river runoff. In this paper, surface water resources calculation method is explained and the total a-mount and distribution of surface water resources are analyzed to provide supporting data for decision-making department to strengthen water resources management, master water resources situation and optimize water resources scheduling.