Micromorphological features of clay translocations in Mediterranean red soils (Rhodoxeralfs-Haploxeralfs)
1986
Baños Moreno, Clemente | Ayerbe Sales, María
1 página, 5 referencias.-- Aparece en la serie Mineralogica et Petrographica Acta volume XXIX-A.-- Congreso celebrado del 24-28 de septiembre 1984, en Seiano di Vico Equense y Amalfi, Italia.-- En el IRNAS se encuentran originales para su consulta.
显示更多 [+] 显示较少 [-]In Soil Micromorphology, a thin-section is representative of a horizon. The basic descriptive unit is the s-matrix; it consists of the plasma, skeletcm grains and voids (porosity) ... (Kubiena, 1938; Brewer, 1964). The arrangement of these basic components and the proportions of plasma, silt and sand lead to formation of distinct «related distribution patterns». The plasma - colloidal fraction of the soil- is the most active component of the soil material and is capable of reorganization, translocation and neoformation.
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