初始含水量、降雨量和降雨强度是影响地被物层水分传输的主导因子。

Initial water content, precipitation quantity and precipitation intensity are the major factors influencing water transport in litters and moss layer.

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入渗深度与降雨量和降雨强度之间存在线性关系，土壤渗透能力随土壤剖面初始含水量的增加而减小，土壤稳定入渗速率的时间趋于缩短。

The infiltration rate is intensively affected by rainfall intensity, and there exists a linear relation between the depth of infiltration and precipitation and rainfall intensity.

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