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CHEMICAL AND MINERALOGICAL CHARACTERISTICS OF SOLONCHAKOUS SOLONETZ AND MEADOW-CHESTNUT SOIL

机译:茄科SOLONETZ和草甸-栗子土壤的化学和矿物学特征

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The soil and plant covers of the vast areas of the clayey semideseit in the Northern Caspian Lowland are distinctly differentiated by meso- and microrelief determining the distribution of moisture with dissolved chemical elements. The largest low-lying landforms termed 'liman' reach dozens and even hundreds of hectares in area, and are occupied by 'liman solods'; smaller mesodepressions stretching over several hectares, and known as 'large padinas', have cheinozem-like soils as typical for their soilcover. The remainder of the area has a patterned, or complex, soil cover corresponding to well-pronounced microrelief Soils of the microhillocks are presented by solonchakous (semihydromorphic) solonetzes under Festuca sulcata--black wormwood communities, soils of the shallow mrcrodepressions are identified as meadow-chestnut soils under forb-grass communities, Light chestnut soils under dry-steppe vegetation occur on microslopes. The difference in height between the microhillocks and microdepressionsis about several dozens of centimeters, whereas the diameters of both are as great as several meters or dozens of meters.
机译:里海北部低地粘土质半宽阔地带的土壤和植物覆盖层通过中,微浮雕来确定,这些浮雕通过溶质化学元素确定了水分的分布。被称为“ liman”的最大的低洼地貌面积达数十甚至数百公顷,被“ liman solods”占据。较小的中压区覆盖数公顷,被称为“大型稻田”,其土壤覆盖层具有典型的千石斑状土壤。该区域的其余部分具有图案丰富或复杂的土壤覆盖物,对应于发音明确的微浮雕。小丘的土壤是由Festuca sulcata的solonchakous(半水形)solonetzes呈现的-黑色艾草群落,浅微凹陷的土壤被确定为草地牧草群落下的栗栗土壤,干草原植被下的栗栗土壤出现在微斜坡上。微丘群和微凹陷之间的高度差约为几十厘米,而两者的直径都高达几米或几十米。

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