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当前位置: 首页 > 文章 > 土壤初始含盐量对水分入渗特性的影响 干旱区研究 2014,31 (2) 222-225
Position: Home > Articles > Effect of Initial Soil Salt Content on Infiltration of Soil Water Arid Zone Research 2014,31 (2) 222-225

土壤初始含盐量对水分入渗特性的影响

作  者：
任长江;白丹;周文;田济扬;程鹏;梁伟
单  位：
西安理工大学水利水电学院
关键词：
土壤含盐量;入渗量;多元回归分析;盐碱地治理
摘  要：
研究土壤初始含盐量对入渗特性的影响,对盐碱地治理具有重要意义。在室内分别进行初始氯化钠含量为3.6、4.5、5.3、5.7 g·kg-1和9.0 g·kg-1的一维垂直土柱淋洗试验。根据试验数据,采用多元回归法,建立了湿润锋、累积入渗量与时间和土壤含盐量之间的量化关系,回归相关系数分别为0.992、0.922,回归模型拟合程度较好;根据累积入渗量得到了入渗率与时间和土壤含盐量之间的量化关系。实验和分析计算表明:土壤初始含盐量对入渗特性的影响大于时间对入渗特性的影响,相同时间土壤初始含盐量越高,入渗湿润锋、累积入渗量和入渗率值越小。
译  名：
Effect of Initial Soil Salt Content on Infiltration of Soil Water
作  者：
REN Chang-jiang;BAI Dan;ZHOU Wen;TIAN Ji-yang;CHENG Peng;LIANG Wei;Institute of Water Resources and Hydroelectric Engineering,Xi'an University of Technology;North China University of Water Resources and Hydropower;Shaanxi Normal University;
关键词：
soil salinity;;infiltration;;multiple regression analysis;;improvement of saline-alkaline soil
摘  要：
It has a great significance to study the effect of initial soil salt content on the infiltration of soil water for improving saline-alkaline soil. A one-dimensional vertical leaching experiment was carried out under different initial soil sodium chloride contents( 3. 6,4. 5,5. 3,5. 7 g·kg- 1and 9. 0 g·kg- 1) in laboratory. According the experiment data,the quantitative relationships between the wetting front,cumulative infiltration and time and the soil salt content were developed using the multiple regression analysis. The regression correlation coefficients were 0. 992 and 0. 922,and the fitting results of the regression model were good. According to the cumulative infiltration,the quantitative relationships between the infiltration rate and time and soil salt content were obtained. The analyzed result showed that the effect of initial soil salt content on the infiltration of soil water was higher than that of time. The higher the initial soil salt content was,the lower the values of wetting front,cumulative infiltration and infiltration rate would be.

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