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INVERSE METHOD TO DETERMINE SOIL HYDRAULIC PROPERTIES FROM TRANSIENT OUTFLOW EXPERIMENTS
作者姓名:ZHANGJun  XUShao-hui  LIUJian-li  ZHANGJia-bao
作者单位:InstituteofSoilScience,ChineseAcademyofSciences,Nanjing210008,China
基金项目:ProjectsupportedbytheNationalNaturalScienceFoundationofChina(GrantNos:49971041,40271059),andtheNationalKeyBasicResearchandDevelopmentProgramofChina(GrantNo:1999011803).
摘    要:Transient outflow experiments coupling with an inverse method are promising to derive soil hydraulic information. The water retention curves obtained from one-step and multi-step outflow experiments were compared with those from the pressure cell method. We found that in one-step experiments the increment of pressure would reduce the non-uniqueness of inverse technique and that in multi-step experiment the combination of cumulative outflow with pressure head in the objective function would improve the final estimation and also reduce the non-uniqueness of inverse problem.

关 键 词:逆推法  土壤水压性质  多步流出实验  操作流程

INVERSE METHOD TO DETERMINE SOIL HYDRAULIC PROPERTIES FROM TRANSIENT OUTFLOW EXPERIMENTS
ZHANGJun XUShao-hui LIUJian-li ZHANGJia-bao.INVERSE METHOD TO DETERMINE SOIL HYDRAULIC PROPERTIES FROM TRANSIENT OUTFLOW EXPERIMENTS[J].Journal of Hydrodynamics,2004,16(6):675-680.
Authors:ZHANG Jun  XU Shao-hui  LIU Jian-li  ZHANG Jia-bao Institute of Soil Science  Chinese Academy of Sciences  Nanjing  China
Affiliation:ZHANG Jun,XU Shao-hui,LIU Jian-li,ZHANG Jia-bao Institute of Soil Science,Chinese Academy of Sciences,Nanjing 210008,China
Abstract:Transient outflow experiments coupling with an inverse method are promising to derive soil hydraulic information. The water retention curves obtained from one-step and multi-step outflow experiments were compared with those from the pressure cell method. We found that in one-step experiments the increment of pressure would reduce the non-uniqueness of inverse technique and that in multi-step experiment the combination of cumulative outflow with pressure head in the objective function would improve the final estimation and also reduce the non-uniqueness of inverse problem.
Keywords:inverse method  hydraulic properties  one-step outflow experiment  multi-step outflow experiment
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