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Assessment of the relationships between the distribution of soil horizons and the climatic parameters

机译:评估土壤层位分布与气候参数之间的关系

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The influence of 15 parameters of atmospheric and soil climates on the distribution of 12 genetic soil horizons (humus, eluvial, illuvial, and metamorphic) in the soils of Russian plains was studied. Quantitative characteristics of the relationships between these climatic parameters and the distribution of soil horizons were estimated by the rank correlation method. The initial dataset was prepared with the use of digitized maps in the MapInfo program. The results of our study made it possible to estimate the climatic parameters with respect to their impact on the formation of soil horizons. The difference between precipitation and potential evaporation, evaporation, and bulk atmospheric moistening of the soils proved to be the most significant climatic parameters affecting the distribution of soil horizons. These characteristics reflect the redistribution of moisture under the influence of temperature factors. The weakest correlation with the distribution of soil horizons was found for the index characterizing the depth of penetration of temperatures > 10A degrees C into the soils.
机译:研究了大气和土壤气候的15个参数对俄罗斯平原土壤中12种遗传土壤层(腐殖质,冲积层,冲积层和变质层)分布的影响。利用秩相关法估算了这些气候参数与土壤层位分布之间关系的定量特征。初始数据集是使用MapInfo程序中的数字化地图准备的。我们的研究结果使估算气候参数对土壤层形成的影响成为可能。降水量与潜在蒸发量,蒸发量以及土壤的整体大气增湿之间的差异被证明是影响土壤层位分布的最重要的气候参数。这些特性反映了在温度因素的影响下水分的重新分布。发现与温度分布最弱的关联关系的是表征温度> 10A摄氏度的土壤渗透深度的指数。

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