By means of GIS, land-use and hydrology were modeled and analyzed.
本研究应用GIS技术，模拟分析了汤旺河流域的土地利用类型与地表水文状况。
参考来源 - 汤旺河流域土地利用与地表水文模拟分析及评价·2,447,543篇论文数据，部分数据来源于NoteExpress
同一坡度和近地表水文条件下，平均侵蚀率是随雨强的增大而增加。
When slope gradient and soil surface hydrological condition had not change, runoff increased with increasing of rainfall intensity.
红层地下水水量受控于气候、地形地貌、地表水文网、岩性、构造运动等环境因素。
The groundwater allocation in red beds is controlled by environment factors such as climate, geomorphology, surface water system, lithology and tectonics.
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.
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