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土壤水热耦合模型的研究
引用本文:刘振华,赵英时. 土壤水热耦合模型的研究[J]. 水土保持通报, 2007, 27(5): 83-88
作者姓名:刘振华  赵英时
作者单位:1. 华南农业大学,信息学院,广东,广州,510642
2. 中国科学院,研究生院,北京,100039
基金项目:国家重点基础研究发展计划(973计划);广东省自然科学基金;广东省环境科学与技术公共实验室开放基金
摘    要:将二维有限元方法和遗传算法结合起来,求解土壤水热耦合方程,获取土壤含水量数据。通过遗传算法来反演水热耦合边界条件,再应用二维有限元方法来正演土壤水热耦合方程,并以遥感数据作为方程的初始条件,实现对土壤水分的时空监测。通过使用内蒙西部研究区的土壤温度和土壤水分数据对此模型进行模拟和检验,结果表明此方法是合理的,应用效果令人满意。

关 键 词:土壤水热耦合  有限元  遗传算法  土壤温度  土壤含水量
文章编号:1000-288X(2007)05-0083-06
收稿时间:2006-12-20
修稿时间:2006-12-20

Study of Coupled Soil Moisture and Heat Flow Equation
LIU Zhen-hua and ZHAO Ying-shi. Study of Coupled Soil Moisture and Heat Flow Equation[J]. Bulletin of Soil and Water Conservation, 2007, 27(5): 83-88
Authors:LIU Zhen-hua and ZHAO Ying-shi
Affiliation:1. College of Informatics , South China Agricultural University, Guangzhou, Guangdong 510642, China; 2. Graduate School of the Chinese Academy of Sciences, Beijing 100039, China
Abstract:In order to improve inversion accuracy for soil moisture and enhance the research on quantitative soil moisture, a method combining finite element with Genetic Algorithms is proposed. Affected by precipitation, irrigation, wind speed, and so on, there exist complex material and energy exchanges on the interface of atmosphere and soil, which lead to very complex boundary conditions of coupled moisture and heat flow equation. Then, Genetic Algorithms are applied to calculating the boundary conditions of the equation. Surface initial condition of the equation is obtained by remote sensing technique. Finally, the finite element method is applied to solving the equation. Thus, monitoring of soil moisture is fulfilled. The tested results show that the method is feasible and satisfactory by comparing with observed data of soil temperature and soil moisture.
Keywords:coupled moisture and heat flow equation   finite element   Genetic Algorithms   soil temperature   soil moisture
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