Soil & Water Res., 2013, 8(1):34-41 | DOI: 10.17221/58/2012-SWR

HYPRESCZ - database of soil hydrophysical properties in the Czech RepublicOriginal Paper

Markéta MIHÁLIKOVÁ, Svatopluk MATULA, František DOLEŽAL
Department of Water Resources, Faculty of Agrobiology, Food and Natural Resources, Czech University of Life Sciences in Prague, Prague, Czech Republic

The database of soil hydrophysical properties in the Czech Republic called HYPRESCZ was created. It is based on the European database HYPRES, HYdraulic PRoperties of European Soils, and follows its structure with few modifications. It collects the available data from the Czech Republic from which pedotransfer functions (PTFs) for the estimation of soil hydrophysical properties from easily available soil properties can be derived and 2101 database entries were collected. The entries have different quality of data, out of the total number of entries 707 entries were applicable to PTFs derivation for the estimation of soil water retention curves (SWRCs). After elimination of replicates, finally 159 unique soil horizons (arable land only) were used for PTFs derivation. The parametric continuous pedotransfer functions for estimation of SWRCs in the Czech Republic were derived within this study and are based on Wösten's model. The retention curves were estimated using both these newly derived PTFs and Wösten's original model, which was derived for European soils in general. The uncertainty of estimation was evaluated, employing the root mean squared error (RMSE) and the coefficient of determination (R2) comparing the PTF-estimated and the directly fitted retention curves. The reliability of the newly derived PTFs for Czech soils was higher (RMSE = 0.059 cm3/cm3 and R2 = 71%) compared to Wösten's general PTFs (RMSE = 0.11 cm3/cm3 and R2 = 36%).

Keywords: HYPRES; pedotransfer functions; soil water retention curve

Published: March 31, 2013  Show citation

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MIHÁLIKOVÁ M, MATULA S, DOLEŽAL F. HYPRESCZ - database of soil hydrophysical properties in the Czech Republic. Soil & Water Res.. 2013;8(1):34-41. doi: 10.17221/58/2012-SWR.
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References

  1. Anderson C.E., Stormont J.C. (2003): Laboratory Measurement of Soil Moisture at Capillary Potential Greater than 1500kPa. TRB Annual Meeting, Washington, D.C.
  2. Bakker G., van der Ploeg M.J., de Rooij G.H., Hoogendam C.W., Gooren H.P.A., Huiskes C., Koopal L.K., Kruidhof H. (2007): New polymer tensiometers: measuring matric pressures down to the wilting point. Vadose Zone Journal, 6: 196-202. Go to original source...
  3. Bouma J. (1989): Using soil survey data for quantitative land evaluation. Advanced Soil Science, 9: 177-213. Go to original source...
  4. Cancela J.J., Dafonte J., Martínez E.M., Cuesta T.S., Neira X.X. (2006): Assessment of a water activity meter for rapid measurements of soil water potential. Biosystems Engineering, 94: 285-295. Go to original source...
  5. Campbell G.S., Shiozawa S. (1992): Prediction of hydraulic properties of soils using particle-size distribution and bulk density data. In: van Genuchten M.T., Leij R.J., Lund L.J. (eds): Int. Workshop on Indirect Methods of Estimating the Hydraulic Properties of Unsaturated Soils. University of California, Riverside, 317-328.
  6. Doležal F., Vlčková. M., Dušek J., Vogel T. (2008): Mathematical modelling of wilting point measurement of Váša's technical method aimed to finding out a correlation between wilting point and retention curves parameters. In: Zborník príspevkov VII. vedecké konferencie s medzinárodnou účasťou.Vplyv antropogénnej činnosti na vodný režim nížinného územia a 17. slovensko-českopoĺský seminár Fyzika vody v pôde. Michalovce, Ústav hydrológie SAV/IH SAS. (in Czech)
  7. Fayer M.J., Simmons C.S. (1995): Modified soil water retention functions for all matric suctions. Water Resources Research, 31: 1233-1238. Go to original source...
  8. Helsel D.R., Hirsch R.M. (2002): Statistical Methods in Water Resources Techniques of Water Resources Investigations. Book 4, Chapter A3. U.S. Geological Survey. Available at http://pubs.usgs.gov/twri/twri4a3/index.html
  9. Kosugi K., Hopmans J.W., Dane J.H. (2002): Parametric models. In: Dane J.H., Topp G.C. (eds): Methods of Soil Analysis - Part 4, Physical Methods. Soil Science Society of America, Inc., Madison, 739-757. Go to original source...
  10. McBratney A.B., Minasny B., Tranter G. (2011): Necessary meta-data for pedotransfer functions. Geoderma, 160: 627-629. Go to original source...
  11. Minasny B., McBratney A., Bristow K.L. (1999): Comparison of different approaches to the development of pedotransfer functions for water retention curves. Geoderma, 93: 225-253. Go to original source...
  12. Minasny B., Hopmans J.W., Harter T., Eching S.O., Tuli A., Denton M. (2004): Neural networks prediction of soil hydraulic functions from multi-step outflow data. Soil Science Society of America Journal, 68: 417-429. Go to original source...
  13. Mualem Y. (1976): A new model for predicting the hydraulic conductivity of unsaturated porous media. Water Resources Research, 12: 513-522. Go to original source...
  14. Němeček J., Mühlhanselová M., Macků J., Vokoun J., Vavříček D., Novák P. (2011): Taxonomic Classification System of Soils of the Czech Republic. 2nd revised Ed. CULS, Prague. (in Czech)
  15. Nemes A. (2002): Unsaturated soil hydraulic database of Hungary: HUNSODA. Agrokémia és Talajtan, 51: 17-26. Go to original source...
  16. Nemes A., Schaap M.G., Leij F.J., Wösten J.H.M. (2001): Description of the unsaturated soil hydraulic database UNSODA version 2.0. Journal of Hydrology, 251: 151-162. Go to original source...
  17. Nemes A., Schaap M.G., Wösten J.H.M. (2003): Functional evaluation of pedotransfer functions derived from different scales of data collection. Soil Science Society of America Journal, 67: 1093-1102. Go to original source...
  18. Nemes A., Wösten J.H.M., Bouma J., Várallyay G. (2006): Soil water balance scenario studies using predicted soil hydraulic parameters. Hydrological Processes, 20: 1075-1094. Go to original source...
  19. Scanlon B.R., Andrski B.J., Bilskie J. (2002): Miscellaneous methods for measuring matric or water potential. In: Dane J.H., Topp G.C. (eds): Methods of Soil Analysis - Part 4, Physical Methods. Soil Science Society of America, Inc., Madison, 643-670. Go to original source...
  20. Schindler U., Müller L. (2006): Simplifying the evaporation method for quantifying soil hydraulic properties. Journal of Plant Nutrition and Soil Science, 169: 623-629. Go to original source...
  21. Schindler U., Müller L. (2010): Data of hydraulic properties of North East and North Central German soils. Earth System Science Data, 2: 189-194. Go to original source...
  22. Štekauerová V., Skalová J., Šútor J. (2002): Using of pedotransfer functions for assessment of hydrolimits. Rostlinná výroba, 48: 407-412. Go to original source...
  23. van Genuchten M.T. (1980): A closed-form equation for predicting the hydraulic conductivity of unsaturated soils. Soil Science Society of America Journal, 44: 892-898. Go to original source...
  24. van Genuchten M.T., Leij F.J., Yates S.R. (1991): The RETC Code for Quantifying the Hydraulic Functions of Unsaturated Soils, Version 1.0. [EPA Report 600/291/065.] U.S. Salinity Laboratory, USDA, ARS, Riverside.
  25. Vereecken H., Herbst M. (2004): Statistical regression. In: Pachepsky Y., Rawls W.J. (eds): Development of Pedotransfer Functions in Soil Hydrology, Developments in Soil Science. Vol. 30, Elsevier, Town, 3-19. Go to original source...
  26. Wösten J.H.M., Lilly A., Nemes A., Le Bas C. (1999): Development and use of a database of hydraulic properties of European soils. Geoderma, 90: 169-185. Go to original source...
  27. Wösten J.H.M., Pachepsky Y.A., Rawls W.J. (2001): Pedotransfer functions: bridging the gap between available basic soil data and missing soil hydraulic characteristics. Journal of Hydrology, 251: 123-150. Go to original source...

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