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Pinhole test for identifying susceptibility of different horizons in less - derived soils to piping erosion

Treść / Zawartość
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The pinhole test is an empirical test based on the qualitative evaluation of the dispersivity (colloidal erodibility) of compacted fined-grained soils. This study evaluates the pinhole test device for the quantitative assessment of the susceptibility of soil horizons to piping. The experiments performed on different loess-derived soil horizons, with different hydraulic head and using distilled water show that the clay-enriched horizon (Bt horizon) is less susceptible to piping than the decalcified (C1) and the calcareous horizon (C2). This study demonstrates that the pinhole test is suitable for assessing the susceptibility of soil horizons to piping in a quantitative way.
Czasopismo
Rocznik
Tom
Strony
131--134
Opis fizyczny
Bibliogr. 13 poz., rys.
Twórcy
autor
  • Department of Earth and Environmental Sciences, Physical and Regional Geography Research Group, K.U. Leuven, Belgium, estelanr@unizar.es
Bibliografia
  • Barahona E., Quirantes J., Guardiola J.L. & Iriarte A., 1990. Factors affecting the susceptibility of soils to interrill erosion in South-eastern Spain. In: Rubio, J.L, & Rickson, R.J. (eds.) Strategies to combat desertification in Mediterranean Europe. Commission of the European Communities, EUR 11175: 216–227.
  • Bocco G., 1991. Gully erosion, processes and models. Progress in Physical Geography 15: 392–406.
  • Boucher S.C., 1990. Field tunnel erosion – its characteristics and amelioration. Department of Geography and Environmental Science, Monash University, Victoria: 64 pp.
  • Faulkner H., 2006. Piping Hazard on Collapsible and Dispersive Soils in Europe. In: Boardman, J. & Poesen, J. (eds.),Soil Erosion in Europe. Wiley (J.), Chichester: 537–562.
  • Higgins C.G., 1990. Gully development. In: Higgins, C.G. & Coates, D.R. (eds.),Groundwater Geomorphology, the Role of Subsurface Water in Earth-Surface Processes and Land-forms. Geol. Soc. Am. Spec. Pap. 252: 139–156.
  • Jones A., 1971: Soil piping and stream channel initiation. Water Resources Research 7: 602–610.
  • Nachtergaele J. & Poesen J., 2002. Spatial and temporal variations in resistance of loess-derived soils to ephemeral gully erosion. European Journal of Soil Science 53: 449–463.
  • Nadal-Romero E., Verachtert E., Maes R. & Poesen J., 2011. Quantitative assessment of the piping erosion susceptibility of loess-derived soil horizons using the pinhole test. Geomorphology 35: 66–79.
  • Peele T.C., Beale O.W. & Latham E.E., 1938. The effect of lime and organic matter on the erodibility of Cecil clay. Soil Science Society of America Proceedings 3: 289–295.
  • Poesen J., 1989. Conditions for gully formation in the Belgian loam belt and some ways to control them. Soil Technology Series 1: 39–52.
  • Poesen J., Vandaele K. & van Wesemael B., 1996. Contribution of gully erosion to sediment production in cultivated lands and rangelands. International Association of Hydrological Sciences Publication 236: 251–266.
  • Poesen J., Nachtergaele J., Verstraeten G. & Valentin C., 2003. Gully erosion and environmental change: importance and research needs.Catena 50: 91–133.
  • Sherard J., Dunningan L., Decker R. & Steele E., 1976. Pinhole test for identifying dispersive soils. Journal of the Geotechnical Engineering Division 11846: 69–85.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUJ5-0052-0001
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