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Abstract

This study tests relationships between, on the one hand, field-saturated infiltration rate into the uppermost sloping soil layer (K-fsi) and field-saturated hydraulic conductivity in soil horizons (K-fsh) and, on the other hand, in situ determined macropore sizes in soil profile descriptions. It was carried out at six locations along a transect on a slope with loamy soils. The macropores were classified into representative size indices based on pore diameters (P-td) and pore areas (P-ta). A strong relationship was found between K-fsi and P-ta, and between K-fsh and P-td. The approach is promising and the methodology could be further developed with the aim of generalizing the functional relationships, so that K-fs can be estimated in areas where soil survey databases contain information on pore size abundance but lack K-fs values

Published in

Soil Use and Management
2005, volume: 21, number: 3, pages: 276-277
Publisher: CABI PUBLISHING

SLU Authors

  • Messing, Ingmar

    • Department of Soil Sciences, Swedish University of Agricultural Sciences

UKÄ Subject classification

Agricultural Science

Publication identifier

  • DOI: https://doi.org/10.1079/SUM2005333

Permanent link to this page (URI)

https://res.slu.se/id/publ/6350