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- W2564367009 abstract "Abstract Hydraulic conductivity of saturated soil, K s , controls many hydrological processes. Parameterization of basin hydrological models in terms of K s is complicated and uncertain owing to the very high spatial variability of this soil property. A small Sicilian basin was intensively sampled by the simplified falling head technique to obtain spatially distributed K s data, and an attempt to explain their spatial variability on the basis of soil physical characteristics, digital elevation model‐derived topographic attributes and land cover was carried out. High K s values were obtained when clay content was low and both elevation and mean slope were high. Moreover, differences in K s among land cover classes were detected. However, soil texture was found to have a main role on K s variability. This finding was supported by a subsequent intensive sampling of two areas differing by elevation and land cover. The conclusion was that, for the sampled basin, a good knowledge of the spatial distribution of the soil textural fractions is necessary to develop an appropriate sampling plan for K s , regardless of both the position within the basin and land use. Copyright © 2016 John Wiley & Sons, Ltd." @default.
- W2564367009 created "2017-01-06" @default.
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- W2564367009 date "2017-03-09" @default.
- W2564367009 modified "2023-09-30" @default.
- W2564367009 title "Factors Influencing Point Measurement of Near‐surface Saturated Soil Hydraulic Conductivity in a Small Sicilian Basin" @default.
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- W2564367009 doi "https://doi.org/10.1002/ldr.2674" @default.
- W2564367009 hasPublicationYear "2017" @default.
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