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初始含水率及容重影响下红壤水分入渗规律

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运用室内模拟土柱试验,研究了初始含水率为7%,11%和15%这3个梯度及容重为1.2,1.3,1.4,1.5 g/cm3这4个梯度对均质红壤水分入渗规律的影响;根据Kostiakov模型和Philip模型对入渗过程进行拟合分析,得出入渗模型参数.试验结果表明:均质红壤水分入渗,入渗率、湿润锋运移速率与时间呈幂函数递减关系,Philip入渗模型较适用;随着时间的推进,土壤逐渐达到饱和,入渗率、湿润锋运移速率的变化也越来越小;入渗率与初始含水率成反比关系,初始含水率越高,入渗率越低;湿润锋运移速率随初始含水率增加而增大;土壤容重越大,入渗率越低,湿润锋运移越慢.
Impacts of Soil Initial Water Content and Bulk Density on Infiltration Law of Red Soil
Effects of different soil initial water contents(7%,11% and 15%) and bulk densities(1.2,1.3,1.4,1.5 g/cm3) on the laws of infiltration in red soil were explored through indoor soil column simulation experiments.Base on Kostiakov model and Philip model,the fitting analysis of infiltration process was conducted and infiltration model parameters were obtained.The results showed that:in the homogeneous red soil,the water infiltration,infiltration rate,and wetting front movement rate were of exponential decrease with time,and Philip infiltration model was more suitable.In the progress of time,the soil water content gradually reached saturation point,and the changes of soil infiltration rate and wetting front movement rate become smaller and smaller.The infiltration rate and initial water content were inversely correlated.The initial water content increased with the decrease of infiltration rate.The wetting front movement rate increased with the increase of initial moisture content.The infiltration rate and wetting front movement rate decreased with the increase of the soil bulk density.

red soilwater infiltrationinitial water contentsoil bulk density

康金林、杨洁、刘窑军、涂安国

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江西农业大学园林与艺术学院,江西南昌330045

江西省水土保持科学研究院,江西南昌330029

江西省土壤侵蚀与防治重点实验室,江西南昌330029

红壤 水分入渗 初始含水率 容重

国家自然科学基金国家自然科学基金水利部公益性项目水利部鄱阳湖水资源水生态环境研究中心开放基金

4136106041501287201301050KFJJ201409

2016

水土保持学报
中国土壤学会 中国科学院水利部水土保持研究所

水土保持学报

CSTPCDCSCD北大核心
影响因子:1.226
ISSN:1009-2242
年,卷(期):2016.30(1)
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