实质上，所有地表水和接近地表的水是作为一个单一的大水文体系的一部分而存在和运动的。
Virtually all surface and near-surface terrestrial water occurs and moves as part of a single vast hydrologic system.
地表水以及土壤水的侧向流动成为山区水文过程必须考虑的部分。
Lateral routing flow of surface water and subsurface soil water become necessary in land surface simulation in mountainous regions.
对地表水源包括无调蓄工程的峪（河）水、有水库控制的峪（河）水进行水文分析，确定地表水的可利用量；
This paper analyzed the river water without and with configuration engineering to sure the reliable quantity of surface water;
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