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Systematization of the topsoil fabrics in soils of the arid lands in northwest of central Asia

机译:中亚西北地区干旱地区土壤中的表土织物的系统化

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The micromorphological data concerning aridic soils are far from being numerous; therefore, the information presented contributes to the development of pedogenetic ideas and characterization of diagnostic horizons and genetic properties in the substantive-genetic classification systems. The diversity, functioning and resilience of aridic soils are basically determined by the properties of their topsoils, which are regarded as recent dynamic formations opposite to the subsoils mostly formed under different paleoclimatic environment; top-soil properties are more important for soil classification. Each of two upper horizons in the new Russian system of soil classification (the light-humus and xero-humus) has the same micromorphological features in different soils; however, in a sequence of soils, some individual micromorphological properties were revealed that indicate the increasing aridity. The micromorphological properties of the topsoils make it possible to identify the mechanisms of some phenomen
机译:有关干旱土壤的微晶数据远远无数;因此,提出的信息有助于在实质性遗传分类系统中产生基础思想和诊断视野和遗传性质的表征。发生的变化土壤的多样性,功能和韧性基本上由其表土的性质决定,其被认为是与大多在不同古叶环境下形成的底层相对的动态结构;土壤分类更为重要。新的俄罗斯土壤分类(轻腐殖质和Xero-Humus)中的两个上视部中的每一个都具有不同土壤中的微晶特征;然而,在一系列土壤中,揭示了一些单独的微晶性质,其表示含量增加。表土的微观性质使得可以识别一些诸如诸如诸如令人挥之不志的机制

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