A field method for determining the soil hydraulic properties using a parameter estimation technique is presented. Input data for the inverse problem are soil-water potentials and soil-water contents measured at different soil depths and different times during a field transient drainage experiment.
Use of an inverse method and geostatistics to estimate soil hydraulic conductivity for spatial variability analysis / Romano, Nunzio. - In: GEODERMA. - ISSN 0016-7061. - 60:1-4(1993), pp. 169-186. [10.1016/0016-7061(93)90025-G]
Use of an inverse method and geostatistics to estimate soil hydraulic conductivity for spatial variability analysis.
ROMANO, NUNZIO
1993
Abstract
A field method for determining the soil hydraulic properties using a parameter estimation technique is presented. Input data for the inverse problem are soil-water potentials and soil-water contents measured at different soil depths and different times during a field transient drainage experiment.File in questo prodotto:
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