Instituto Geológico y Minero de España

LogoSistema de información documental - SID

 

 

 

Resultados de la consulta :
Instituto Geológico y Minero de España
 Registros del al 9 de 9 encontrados

1.-  A simplified parametric model to describe the magnitude and geometry of soil shrinkage
Blackwell Science and the British Society of Soil Science on behalf of National Societies of Soil Sc, 2006
Ver registro

2.-  Comparison of single- and double-ring infiltrometer methods on stony soils
Soil Science Society of America; Madison, WI; USA; United States, 2010
Ver registro

3.-  Estimating the spatial distribution of hillslope sediment delivery to river channels using information at three different spatial scales in the Cuyaguateje Basin, Cuba
Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Federal R, 2009
European Geosciences Union general assembly 2009
Ver registro

4.-  Estimating the water retention curve of stony soils from on-the-spot tension infiltrometry
Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Federal R, 2008
European Geosciences Union general assembly 2008
Ver registro

5.-  Hydraulic conductivity as influenced by stoniness in degraded drylands of Chile
Soil Science Society of America; Madison, WI; USA; United States, 2009
Ver registro

6.-  Measuring and modelling the soil shrinkage characteristic curve
Elsevier; Amsterdam; NLD; Netherlands, 2006
Ver registro

7.-  On the influence of coarse fragments on soil water retention
American Geophysical Union; Washington, DC; USA; United States, 2009
Ver registro

8.-  Parameterizing a coupled surface-subsurface three-dimensional soil hydrological model to evaluate the efficiency of a runoff water harvesting technique
Soil Science Society of America; Madison, WI; USA; United States, 2012
Model-data fusion in the vadose zone
Ver registro

9.-  Regional frequency analysis for mapping drought events in north-central Chile
Elsevier; Amsterdam; NLD; Netherlands, 2011
Ver registro


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