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Geochemical and Pedochemical Weathering,e second stage the effects of vegetation, both living and dead, together with the effects of metabolism of microorganisms living in the geochemically altered rock material, are added to the continued inorganic processes, and this combination produces a soil which is the culmination of weathering at that particular locality.Basal-Ganglia 发表于 2025-3-22 03:22:01
,The Earth’s Crust,d the core of the earth. The crust is the exposed surface of the lithosphere that has been modified in various ways by climate and by the vegetation that forms a cover where the climate is favorable to the growth of plants. According to the climate we find regions of tundra, prairies, semitropical afrivolous 发表于 2025-3-22 05:28:49
The Weathering Environment,usceptibility to alteration by weathering processes. Furthermore, the chemical environment in which rocks are altered varies with position on the earth’s surface and also with local conditions. The environments under which most atmospheric weathering takes place are oxidizing with an oxidation poten注入 发表于 2025-3-22 09:30:09
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Physical Weathering,ing occurs in very cold, dry or very hot, dry climates, and splitting is largely due to insolation. A chemical analysis of the fragmented rock would be similar to that of the solid rock. Disintegration of rocks in moist climates accompanies chemical weathering.angina-pectoris 发表于 2025-3-23 03:34:30
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Biological Activity in Weathering,tion of the microflora and chemical processes, produces the soil humus. The effect of the flora and its products reacting with the mineral particles of weathered rocks changes geochemical weathering into pedochemical weathering and affects the consequent development of soils.