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Titlebook: Micromorphology of Soils; E. A. Fitzpatrick Book 1984 E.A. FitzPatrick 1984 Oxide.fabric.geomorphology.growth.microorganism.serpentine.soi

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書目名稱Micromorphology of Soils
編輯E. A. Fitzpatrick
視頻videohttp://file.papertrans.cn/634/633345/633345.mp4
圖書封面Titlebook: Micromorphology of Soils;  E. A. Fitzpatrick Book 1984 E.A. FitzPatrick 1984 Oxide.fabric.geomorphology.growth.microorganism.serpentine.soi
描述One of the first major studies of weathering and soil formation was made by Harrison (1933) who used thin sections in association with other procedures to study the transformation of minerals in different kinds of rock under the tropical conditions of Guyana. However, Kubiena (1938) is regarded as pioneering thin section studies of soils and during the last two decades there has been a rapid increase in the number of publications devoted almost exclusively to the study of soils in thin sections. In addition to the rather straightforward examinations with the polarizing microscope, thin section techniques are being linked with X-ray diffraction, X-ray microprobe, transmission and scanning electron microscopy, microbiological and other procedures to obtain a fuller insight into the composition and genesis of soils. Thus the study of thin sections of soils is now a major pedological technique for investigating small details in the nature, type and degree of organization of the soil fabric and structure. Thin sections reveal that particles of various sizes and composition react differently to pedological processes and become weathered or organized to form many specific patterns. This b
出版日期Book 1984
關(guān)鍵詞Oxide; fabric; geomorphology; growth; microorganism; serpentine; soil; soil science
版次1
doihttps://doi.org/10.1007/978-94-009-5544-8
isbn_softcover978-94-010-8946-3
isbn_ebook978-94-009-5544-8
copyrightE.A. FitzPatrick 1984
The information of publication is updating

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Description of thin sections and polished blocks,nerals, weathered minerals and plant fragments. Although generally speaking this is the case, the wide range in the composition, frequency and arrangement of these components creates a number of problems that are unique to the description of thin sections of soils. These problems can be discussed under the following headings:
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Principles of thin section preparation,Thin sections of soils are prepared by a technique similar to that employed by geologists for making thin sections of rocks, but soils must normally be impregnated with a resin and hardened before they can be cut, lapped and polished. The resins currently employed are polyester, polystyrene or epoxy compounds.
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