流域内自然地理要素的空间差异导致了流域水文过程的时空变化。
Spatial heterogeneity of physiogeographical components leads to spatial and chronological changes of hydrological process in watershed.
降水入渗规律的研究可为流域水文过程的预测和评价提供重要的科学依据。
Study of water through soil infiltration may offer a scientific support for prediction and evaluation of watershed hydrological processes.
因此，对流域水文过程研究的最终目的，就是建立基于“流域二元水循环模式”的流域水文模型。
The essence of So-called Dual Water Evolvement Mode is to study the impact of nature processes and man's activities respectively.
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