Description of the unsaturated soil hydraulic database UNSODA version 2.0

被引:297
作者
Nemes, A
Schaap, MG
Leij, FJ
Wösten, JHM
机构
[1] Alterra Res Inst Green World Res, NL-6700 AA Wageningen, Netherlands
[2] Hungarian Acad Sci, Res Inst Soil Sci & Agr Chem, H-1022 Budapest, Hungary
[3] USDA ARS, George E Brown Jr Salin Lab, Riverside, CA 92507 USA
基金
美国国家科学基金会; 美国国家航空航天局;
关键词
soil hydraulic database; unsaturated soils; water retention; hydraulic conductivity; soil water diffusivity; particle-size distribution;
D O I
10.1016/S0022-1694(01)00465-6
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Quantifying water flow and chemical transport in the vadose zone typically requires knowledge of the unsaturated soil hydraulic properties. The UNsaturated Soil hydraulic DAtabase (UNSODA) was developed to provide a source of unsaturated hydraulic data and some other soil properties for practitioners and researchers. The current database contains measured soil water retention, hydraulic conductivity and water diffusivity data as well as pedological information of some 790-soil samples from around the world. A first MS-DOS version of the database was released in 1996. It has been applied in numerous studies. In this paper, we describe the second version (UNSODA V2.0) for use with Microsoft Access-97((R)1). The format and structure of the new database have been modified to provide additional and more convenient options for data searches, to provide compatibility with other programs for easy loading and downloading of data. and to allow users to customise the contents and look of graphical output. This paper reviews the structure and contents of the database as well as the operations that can be performed on the different data types in UNSODA V2.0, The use and application of the new database are illustrated with two examples. The retrieval of data is briefly illustrated, followed by a more detailed example regarding the interpolation of soil particle-size distribution data obtained according to different national definitions of particle-size classes, The interpolation procedure, which is based on finding similar particle-size distribution curves from a large European data set, also performed well for soils that originate from other geographical areas. (C) 2001 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:151 / 162
页数:12
相关论文
共 21 条
  • [1] Relationship between the hydraulic conductivity function and the particle-size distribution
    Arya, LM
    Leij, FJ
    Shouse, PJ
    van Genuchten, MT
    [J]. SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1999, 63 (05) : 1063 - 1070
  • [2] Scaling parameter to predict the soil water characteristic from particle-size distribution data
    Arya, LM
    Leij, FJ
    van Genuchten, MT
    Shouse, PJ
    [J]. SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1999, 63 (03) : 510 - 519
  • [3] FAO, 1993, GLOB NAT SOILS TERR
  • [4] FAO, 1995, DIG SOIL MAP WORLD D
  • [5] FINKE PA, 1995, BODEMKAART TOT INFOR, P111
  • [6] Gee GW, 1999, P INT WORKSH CHAR ME, P241
  • [7] Hoffmann-Riem H., 1999, Proceedings of the International Workshop, Characterization and Measurements of the Hydraulic Properties of Unsaturated Porous Media, P31
  • [8] General model for unsaturated hydraulic conductivity for soils with lognormal pore-size distribution
    Kosugi, K
    [J]. SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1999, 63 (02) : 270 - 277
  • [9] Estimating the soil water retention from particle-size distributions: A fractal approach
    Kravchenko, A
    Zhang, RD
    [J]. SOIL SCIENCE, 1998, 163 (03) : 171 - 179
  • [10] Closed-form expressions for water retention and conductivity data
    Leij, FJ
    Russell, WB
    Lesch, SM
    [J]. GROUND WATER, 1997, 35 (05) : 848 - 858