在自然环境下,对土壤中温度和湿分分布以及水分蒸发的动态特性进行了实验研究,分析了干饱和层对土壤热湿迁移及水分蒸发的影响.结果表明:(1)在周期性变化的大气环境条件下,土壤温度、湿分含量和水分蒸发强度在一天内变化;随着土壤温度的降低,土壤水分含量在晚上会出现略有增加的情况.(2)形成干饱和层后,水分蒸发锋面由土壤表面下移至非饱和层与干饱和层界面处,水分蒸发强度明显减弱,干饱和层的厚度增长缓慢.(3)随着干饱和层不断向深处发展,土壤温度的日变化幅度增大,且随着土壤深度的增加,土壤温度变化呈现出明显的滞后性.
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