Soil Micromorphology |
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2. Micromorphography Soil description under the microscope |
3. Micromorphology Soil interpretation under the microscope |
Clay eluviation/illuviation processes in soils
E. Fernández*, C. Dorronsoro-Fdez*, J. Aguilar*, B. Dorronsoro**, G. Stoops***, C. Dorronsoro Díaz****
* Dpto. Edafologia y Química Agricola, Facultad de Ciencias,
Universidad de Granada, 18002 Granada, Spain.
** Dpto. Lenguas y Ciencias de la Computacion, E.T.S.I. Informatica,
Universidad de Malaga, 29071 Malaga, Spain.
*** International Training Centre for Post-Graduate Soil Scientists, University
of Gent, Krijgslaan 281, B-9000 Gent, Belgium.
**** Instituto de Optica "Daza Valdes", Consejo Superior de Investigaciones
Cientificas, 28006 Madrid, Spain.
This program illustrates the features resulting from clay eluviation/illuviation processes, which consist of the mobilization, transportation and accumulation of clay in the B horizon, proceed of upper horizons.
As a result of this process, clay accumulations occur and we shall go on to consider the following aspects of these.
Formation: genesis, stages, factors
Properties of the acumulations of illuvial clay
Micromorphological classification
Recognition: techniques, confusions
Micromorphology of argillic horizons