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室内试验方法确定非饱和土壤水分运动参数
引用本文:赵晶晶,唐亚莉,虎胆·吐马尔白.室内试验方法确定非饱和土壤水分运动参数[J].新疆农业科学,2007,44(4):490-493.
作者姓名:赵晶晶  唐亚莉  虎胆·吐马尔白
作者单位:新疆农业大学水利与土木工程学院,乌鲁木齐,830052
基金项目:国家自然科学基金;新疆维吾尔自治区高校科研计划创新群体基金
摘    要:以土壤水动力学为理论基础,以原状砂壤土为例,进行了室内非饱和土壤水分运动参数的测定.通过实测数据与经验模型Van Genuchten的拟和,对试验结果和拟和结果进行了对比分析,发现计算值与实测数据吻合较好.结果表明选用的经验模型是可靠的,确定的非饱和土壤水分运动参数是合理的.

关 键 词:砂壤土  土壤水分特征曲线  土壤水分传导度  土壤扩散度
文章编号:1001-4330(2007)04-0490-04
收稿时间:2006-12-11
修稿时间:2006年12月11

Determination of Parameters for Unsaturated Soil Water Movement by Experimental Method in Laboratory
ZHAO Jing-jing,TANG Ya-li,Hudan·Tumaerbai.Determination of Parameters for Unsaturated Soil Water Movement by Experimental Method in Laboratory[J].Xinjiang Agricultural Sciences,2007,44(4):490-493.
Authors:ZHAO Jing-jing  TANG Ya-li  Hudan·Tumaerbai
Abstract:In this paper the experiment of the parameters for unsaturated soil water movement by experimental method in laboratory was carried out based on the theory of soil water dynamics and a case study of sandy clay loam.By observing the field data and fit values of Van Genuchten empirical model,it is found that the values of computation agree with the experimental data fairly well and also the result of selective empirical model is feasible,the determination of soil water movement by experimental method in laboratory is reasonable.
Keywords:sandy clay loam  parameters of soil water movement  hydraulic conductivity of soil  diffusion of soil
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