Influence of organic matter on aggregation in Oxisols rich in gibbsite or in goethite. II. Clay dispersion, aggregate strength and water-stability-Reference-Cited by-同舟云学术

Influence of organic matter on aggregation in Oxisols rich in gibbsite or in goethite. II. Clay dispersion, aggregate strength and water-stability

Published:1992-09 Issue:1-4 Volume:54 Page:259-274
ISSN:0016-7061
Container-title:Geoderma
language:en
Short-container-title:Geoderma

Author:

Bartoli F.,Burtin G.,Guerif J.

Publisher

Elsevier BV

Subject

Soil Science

Reference30 articles.

1. Disaggregation and clay dispersion of Oxisols: Na resin, a recommended methodology;Bartoli;Geoderma,1991

2. Structure and self-similarity in silty and sandy soils: the fractal approach;Bartoli;J. Soil Sci.,1991

3. Influence of organic matter on aggregation in Oxisols rich in gibbsite or in goethite. I. Structures: the fractal approach;Bartoli;Geoderma,1992

4. Poorly-ordered hydrous Fe oxides, colloidal dispersion and soil aggregation. II. Modification of silty soil aggregation by addition of Fe (III) polycations associated or not with humic macromolecule models;Bartoli;J. Soil Sci.,1992

5. Studies on a Nigerian forest soil. I. The distribution of organic matter in the profile and in various soil fractions;Bates;J. Soil Sci.,1960

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