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区域地下水溶质运移随机理论的研究与进展

杨金忠 蔡树英 叶自桐

杨金忠, 蔡树英, 叶自桐. 区域地下水溶质运移随机理论的研究与进展[J]. 水科学进展, 1998, 9(1): 84-98.
引用本文: 杨金忠, 蔡树英, 叶自桐. 区域地下水溶质运移随机理论的研究与进展[J]. 水科学进展, 1998, 9(1): 84-98.
Yang Jinzhong, Cai Shuying, Ye Zitong. A Review of Stochastic Analysis for Solute Transport at Regional Scale[J]. Advances in Water Science, 1998, 9(1): 84-98.
Citation: Yang Jinzhong, Cai Shuying, Ye Zitong. A Review of Stochastic Analysis for Solute Transport at Regional Scale[J]. Advances in Water Science, 1998, 9(1): 84-98.

区域地下水溶质运移随机理论的研究与进展

基金项目: 自然科学基金,霍英东教育基金(No.59379404)
详细信息
  • 中图分类号: P641.2

A Review of Stochastic Analysis for Solute Transport at Regional Scale

  • 摘要: 在总结近年来国内外区域地下水溶质运动研究的基本理论、方法和部分成果的基础上,论述了溶质在大区域运动的主要影响因素为区域介质的空间变异性。首先总结了野外条件下饱和介质和非饱和介质土壤渗透性能的空间变异性结果,由于野外渗透介质严重的空间变异性,研究溶质在野外条件下的运动采用了随机理论方法。基于Lagrange方法和Euler方法,研究结果表明,在渗透系数为对数正态二阶平稳及一阶扰动近似条件下,平均浓度满足对流-弥散方程,方程中宏观弥散度决定于介质渗透性能的统计特征,总结了一系列宏观弥散系数的表达形式,在此基础上,指出了需要进一步研究的问题。
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出版历程
  • 收稿日期:  1996-06-16
  • 修回日期:  1996-10-15
  • 刊出日期:  1998-01-25

区域地下水溶质运移随机理论的研究与进展

    基金项目:  自然科学基金,霍英东教育基金(No.59379404)
  • 中图分类号: P641.2

摘要: 在总结近年来国内外区域地下水溶质运动研究的基本理论、方法和部分成果的基础上,论述了溶质在大区域运动的主要影响因素为区域介质的空间变异性。首先总结了野外条件下饱和介质和非饱和介质土壤渗透性能的空间变异性结果,由于野外渗透介质严重的空间变异性,研究溶质在野外条件下的运动采用了随机理论方法。基于Lagrange方法和Euler方法,研究结果表明,在渗透系数为对数正态二阶平稳及一阶扰动近似条件下,平均浓度满足对流-弥散方程,方程中宏观弥散度决定于介质渗透性能的统计特征,总结了一系列宏观弥散系数的表达形式,在此基础上,指出了需要进一步研究的问题。

English Abstract

杨金忠, 蔡树英, 叶自桐. 区域地下水溶质运移随机理论的研究与进展[J]. 水科学进展, 1998, 9(1): 84-98.
引用本文: 杨金忠, 蔡树英, 叶自桐. 区域地下水溶质运移随机理论的研究与进展[J]. 水科学进展, 1998, 9(1): 84-98.
Yang Jinzhong, Cai Shuying, Ye Zitong. A Review of Stochastic Analysis for Solute Transport at Regional Scale[J]. Advances in Water Science, 1998, 9(1): 84-98.
Citation: Yang Jinzhong, Cai Shuying, Ye Zitong. A Review of Stochastic Analysis for Solute Transport at Regional Scale[J]. Advances in Water Science, 1998, 9(1): 84-98.
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