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Titlebook: Soil Formation; Nico Breemen,Peter Buurman Book 1998 Springer Science+Business Media Dordrecht 1998 environment.soil.transport

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發(fā)表于 2025-3-21 19:09:43 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱Soil Formation
編輯Nico Breemen,Peter Buurman
視頻videohttp://file.papertrans.cn/872/871240/871240.mp4
圖書封面Titlebook: Soil Formation;  Nico Breemen,Peter Buurman Book 1998 Springer Science+Business Media Dordrecht 1998 environment.soil.transport
描述Soils form a unique and irreplaceable essential resource for all terrestrial organisms, including man. Soils form not only the very thin outer skin of the earth‘s crust that is exploited by plant roots for anchorage and supply of water and nutrients. Soils are complex natural bodies formed under the influence of plants, microorganisms and soil animals, water and air from their parent material, i.e. solid rock or unconsolidated sediments. Physically, chemically and mineralogically they usually differ strongly from the parent material, and normally are far more suitable as a rooting medium for plants. In addition to serving as a substrate for plant growth, including crops and pasture, soils play a dominant role in the biogeochemical cycling of water, carbon, nitrogen and other elements, influencing the chemical composition and turnover rates of substances in the atmosphere and the hydrosphere. Soils take decades to millennia to form. We tread on them and do not usually see their interior, so we tend to take them for granted. But improper and abusive agricultural management, careless land- clearing and reclamation, man-induced erosion, salinisation and acidification, desertification,
出版日期Book 1998
關鍵詞environment; soil; transport
版次1
doihttps://doi.org/10.1007/978-0-585-31788-5
isbn_softcover978-94-017-4140-8
isbn_ebook978-0-585-31788-5
copyrightSpringer Science+Business Media Dordrecht 1998
The information of publication is updating

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沙發(fā)
發(fā)表于 2025-3-21 21:15:02 | 只看該作者
Book 1998 the earth‘s crust that is exploited by plant roots for anchorage and supply of water and nutrients. Soils are complex natural bodies formed under the influence of plants, microorganisms and soil animals, water and air from their parent material, i.e. solid rock or unconsolidated sediments. Physical
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Why Soil Genesis?orizon decreases or increases, sedimentary layering disappears, etc. Mostly, such changes are slow, and can be seen only after decades to millenia. So most soil properties that change during soil formation are relatively stable. Sometimes, however, effects of soil formation can be seen within weeks
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Soil Physical Processesture gradients and fluctuations, and shrinkage and swelling. Here a short outline of such processes will be given. For more details on the principles involved in the movement of water through soils, reference is made to introductory tests as such in 2.7.
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Soil Chemical Processesal aspects of weathering of primary minerals, the nature of important crystalline and amorphous weathering products, cation exchange processes in relation to colloidal properties of clay, complexation of metals by organic ligands, and redox processes in soils.
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Studying Soil Profilessystems (FAO-Unesco and Soil Taxonomy). You will be able to describe the formation of these diagnostic horizons, and thereby, of the different genetic soil types, in terms of the physical, chemical and biological processes you studied in Part B.
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