矿物形成对纳希切万地区土壤结构恢复的影响及其地理分布合法性

Rae. Z. H. Aliyev
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引用次数: 0

摘要

粉土组分对土壤结构的形成有很大的影响。如果成土岩不受扰动、挤压和风化作用,其上的成土过程发生微弱,有机质形成的壤土层不完全翻转。这主要影响初始成土层。这些土壤中的再生矿物主要以弱发生的方式形成初始矿物。如果这些过程发生得很快,那么它们会导致再生矿物的逐渐增加和初始矿物的减少。这种地层在地理上分布的区域的高度取决于水平面。
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Impact of mineralformation on restoration of the soil structure in nakhchivan AR and geographical spreading legitimacy
The silt fractions have a great impact in soil structural formation. If the soil forming rocks don't disturb, crush and weather, the soil forming processes on them occur weakly, the organic substances cause formation of the loamy stratums without completely turning. This mostly influences the initial soil forming layers. The reproduction minerals in these soils cause initial minerals majority by occurring weakly. If these processes occur quickly then they cause a gradual increase of the reproduction minerals and reduction of the initial minerals. The heights of the zones where the geographical spreading of such stratums is situated depend on levels.
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