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基于遗传算法的土壤水分运动参数识别
引用本文:杨 坤,白 丹,郝祥琪,陈 博.基于遗传算法的土壤水分运动参数识别[J].农业工程学报,2009,25(9):32-35.
作者姓名:杨 坤  白 丹  郝祥琪  陈 博
作者单位:1. 西安理工大学西北水资源与环境生态教育部重点实验室,西安,710048;哈尔滨工业大学市政环境工程学院,哈尔滨,150090
2. 西安理工大学西北水资源与环境生态教育部重点实验室,西安,710048
3. 哈尔滨工业大学市政环境工程学院,哈尔滨,150090;山西省水利厅,太原,030000
基金项目:国家自然科学基金资助项目(50549018, 50979089)
摘    要:土壤水分运动参数的识别是研究土壤水分运动的基础。该文以反映土壤含水率实测值和计算值吻合程度的均方差最小为优化目标,以土壤导水率和扩散率经验参数上下限为约束条件,建立了土壤水分运动参数识别的优化计算模型。采用遗传算法和田间均质土壤一维非饱和运动数值计算相结合的方法,获得土壤导水率和扩散率经验参数最优值。经验证计算,土壤含水率实测值和计算值吻合程度较高,表明这一方法是可行的。

关 键 词:遗传算法,土壤含水率,水力,非饱和土壤水,土壤水分运动参数
收稿时间:2007/11/27 0:00:00
修稿时间:2009/9/11 0:00:00

Identification of soil hydraulic properties based on genetic algorithm
Yang Kun,Bai Dan,Hao Xiangqi and Chen Bo.Identification of soil hydraulic properties based on genetic algorithm[J].Transactions of the Chinese Society of Agricultural Engineering,2009,25(9):32-35.
Authors:Yang Kun  Bai Dan  Hao Xiangqi and Chen Bo
Institution:1. Key Laboratory of Northwest Water Resources and Environment Ecology of Ministry of Education, Xi'an University of Technology, Xi'an 710048, China; 2. School of Municipal and Environmental Engineering, Harbin Institute of Technology, Harbin 150090, China,1. Key Laboratory of Northwest Water Resources and Environment Ecology of Ministry of Education, Xi'an University of Technology, Xi'an 710048, China,1. Key Laboratory of Northwest Water Resources and Environment Ecology of Ministry of Education, Xi'an University of Technology, Xi'an 710048, China and 2. School of Municipal and Environmental Engineering, Harbin Institute of Technology, Harbin 150090, China; 3. Department of Water Resources of Shanxi Province, Taiyuan 030000, China
Abstract:The identification of the soil hydraulic properties is the basis of studying soil water movement. An optimization model was established for identifying the soil hydraulic properties. The optimization objective was the minimum mean square deviation of simulation between measured and observed values of soil water content, and the constraint conditions were the upper and lower limit values of empirical soil hydraulic conductivity and water diffusion coefficients. The optimal values of the soil hydraulic conductivity and water diffusion coefficients could be obtained through applying genetic algorithm and numerical simulation method of one-dimensional flow movement in unsaturated homogeneous soil. The test showed that the numerical simulation results of soil water content were well coincided with the observed values. Therefore, the method is feasible.
Keywords:genetic algorithm  soil moisture  hydraulics  unsaturated soil water  soil hydraulic properties
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