饱和与非饱和带土壤水动力耦合模拟及入渗试验  

Dynamic coupled modeling and infiltration experiment on soil water in saturated and unsaturated zones

作　　者：程勤波[1] 陈喜[1] 赵玲玲[1] 凌敏华[1] 

机构地区：[1]河海大学水文水资源与水利工程科学国家重点实验室,江苏南京210098

出　　处：《河海大学学报（自然科学版）》2009年第3期284-289,共6页Journal of Hohai University(Natural Sciences)

基　　金：国家自然科学基金(50679025);国家"十一五"科技支撑计划重点项目(2006BAB14B00);教育部科学技术研究重大项目(308012)

摘　　要：利用可变坡土槽人工降水入渗试验,观测土壤水势及地下水出流量变化,建立了饱和与非饱和带土壤水数值计算模型MODFLOW-UZF1的参数率定及模型验证方法.结果表明:MODFLOW-UZF1能较为准确地模拟降水入渗补给过程,但忽略了非饱和带土壤水分运移中基质势的影响,在毛细管作用带土壤含水量模拟效果较差.Through artificial precipitation infiltration experiments in a soil trough with variable slopes, the variation of soil water potential and groundwater discharge was observed. A method of parametric calibration and model validation for the widely used nmnerical model of soil water in saturated and unsaturated zones, that is, MODFLOW-UZF1, was established. The numerical results show that the MODFLOW-UZF1 can correctly simulate the precipitation infiltration process. However, it ignores the effect of the matric potential in transport of soil water in the unsaturated zone, and it results in a larger error between the simulated and observed soil moisture contents in the capillary zone.

关 键 词：MODFLOW 饱和与非饱和带土壤水 耦合模拟 降水入渗试验 

分 类 号：TV139.16[水利工程—水力学及河流动力学]