EXPERIMENTAL-STUDY OF FRAGIPANS FORMATION IN SOILS - ROLE OF BOTH CLAY DISPERSION AND WETTING-DRYING CYCLES

Authors
Citation
F. Attou et A. Bruand, EXPERIMENTAL-STUDY OF FRAGIPANS FORMATION IN SOILS - ROLE OF BOTH CLAY DISPERSION AND WETTING-DRYING CYCLES, Comptes rendus de l'Academie des sciences. Serie II. Sciences de la terre et des planetes, 326(8), 1998, pp. 545-552
Citations number
32
Categorie Soggetti
Geosciences, Interdisciplinary
ISSN journal
12518050
Volume
326
Issue
8
Year of publication
1998
Pages
545 - 552
Database
ISI
SICI code
1251-8050(1998)326:8<545:EOFFIS>2.0.ZU;2-Q
Abstract
There is considerable literature about fragipans but their origin is s till under discussion. In the laboratory, we investigated silt-clay fa brics which were obtained by mixing a sill fraction with either air-dr ied clay forming clayey aggregates or wet clay as a paste. The results from scanning electron microscopy and porosity analysis were used to study the formation of fragipans. Our results suggest that fragipans o riginate from successive wetting and drying cycles. Each wetting perio d would favour the dispersion of clay particles within the soil matrix and each drying period would favour its reorganization into coatings over the skeleton grains and wall-shaped bridges between these grains. The prevalence of these processes makes possible the formation of fra gipans under varied climatic conditions. (C) Acadimie des sciences/Els evier, Paris.