Características mineralógicas de la fracción inferior A 2$ en vitrandepts (IV)
The mineralogical composition of the clay fraction ($2u) of four soil profiles from Zahagu, Tajanara, Chio. Chinyero, have been studied by X-ray diffraction and I. R. absorption techniques. This clay fraction contains a great amount of amorphous gels and some kaolin-type minerals (hallosyte and disordered kaolinite, probably in a transformation stage), they also contain allophane and illite. Primary minerals present in the clay fraction of the four profiles are felspars and piroxenes. Quartz and a-crystohallite are also founds in the clay fraction in some soil horizons.
Main Authors: | , , , |
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Format: | artículo biblioteca |
Language: | Spanish / Castilian |
Published: |
CSIC - Instituto Nacional de Edafología y Agrobiología José María Albareda
1977
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Online Access: | http://hdl.handle.net/10261/20676 |
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Summary: | The mineralogical composition of the clay fraction ($2u) of four soil profiles from Zahagu, Tajanara, Chio. Chinyero, have been studied by X-ray diffraction and I. R. absorption techniques. This clay fraction contains a great amount of amorphous gels and some kaolin-type minerals (hallosyte and disordered kaolinite, probably in a transformation stage), they also contain allophane and illite.
Primary minerals present in the clay fraction of the four profiles are felspars and piroxenes.
Quartz and a-crystohallite are also founds in the clay fraction in some soil horizons. |
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