An Introduction to UNSODA Soil Bank and Its Application in Soil and Water Research

Document Type : review paper

Authors

Ferdowsi University of Mashhad

Abstract

There are numerous mathematical models that predict and analyze the movement of water and pollutants in saturated and unsaturated zones beneath the soil. The usefulness and accuracy of these models severely depend on the reliable characterization of the soil hydraulic properties, i.e. water retention and hydraulic conductivity of the unsaturated zone. The accurate measurements of these properties are highly cumbersome and are not feasible for many applications including issues concerning soil contamination. UNSODA is a soil database containing unsaturated soil hydraulic properties (water retention, hydraulic conductivity, and soil water diffusivity), basic soil properties (particle-size distribution, bulk density, organic matter content, etc.), which are used for indirect prediction of the unsaturated soil hydraulic functions. This paper introduces this database, explains its applications, and shows how it can be used in soil and water research.

Keywords


امیدی، س.، قهرمان، ب. 1388. استفاده از سطح ویژه بخار- مایع در برآورد تابع هدایت هیدرولیکی غیراشباع. پژوهش‏های حفاظت آب و خاک، 16(3): 83-104.
مهدیان، م.، قهرمان، ب. 1392. رابطه تجربی بین شاخه خشک و تر منحنی رطوبتی خاک با استفاده از مدل ون‏گنوختن. پژوهش‏های خاک (علوم خاک و آب)، 27(4): 521-529.
Arya L.M. and Paris J.F. 1981. A physicoempirical model to predict the soil moisture characteristic from particle size distribution and bulk density data. Soil Sci Soc Am J, 45:1023-1030.
Carsel R. F. and R. S. Parrish. 1988. Developing joint probability distributions of soil water retention characteristics. Water Resour. Res., 24: 755-769.
Ghahraman B., Omidi S. and Khoshnood Yazdi A. 2012. Scaling and Fractal Concepts in Saturated Hydraulic Conductivity: Comparison of Some Models. Iran agricultural research, 31.
Ghanbarian b., Taslimitehrani V. and Pachepsky Y.A. 2017. Accuracy of sample dimension-dependent pedotransfer functions in estimation of soil saturated hydraulic conductivity. CATENA, 149 (1):374-380.
Leij F. J., Alves W. J. and Van Genuchten M. Th. 1996. The UNSODA Unsaturated Soil Hydraulic Database User’s Manual Version 1.0. U.S. Salinity Laboratory. EPA/600/R-96/095.
Nemes A., Schaap M. and Leij F. J. 1999. The UNSODA Unsaturated Soil Hydraulic Database Version 2.0. U.S. Salinity Laboratory Riverside CA 92507. USA.
Van Genuchten M.Th., Leij F.J. and Yates S.R. 1991. The RETC code for quantifying the hydraulic functions of unsaturated soils. (Available at www.ussl.ars.usda.gov/models/retc.htm; verified 11 Jan. 2005). Report No. EPA/600/2–91/065. R.S. Kerr Environ. Res. Lab., USEPA, Ada, OK.
Van Genuchten M. Th., Leij F. J. and Lund L. J. 1992. Proceedings International Workshop Indirect methods for estimating the hydraulic properties of unsaturated soils. Univ. California, Riverside.
Wösten J. H. M. and Bouma J. 1992. Applicability of soil survey data to estimate hydraulic properties of unsaturated soils, 463-472. In M. Th. van Genuchten, F. J. Leij, and L. J. Lund (ed.) Proc. Int. Workshop on Indirect Methods for Estimating the Hydraulic Properties of Unsaturated Soils. Univ. California, Riverside, CA.
Zhuang J., Nakayama K., Yu G. R. and Miyazaki T. 2000a. Scaling of saturated hydraulic conductivity: A comparison of models. Soil Sci, 165(9):718-727.
CAPTCHA Image