Abstract

The southern part of European Russia includes regions between two mainland-forming seas: the Black Sea from the northwest and the Caspian Sea from the southeast. The Caucasus Mountains characterized by variegated topography stretch between these seas in the submeridional direction for the total distance of more than 1500 km. The temperate and subtropical belts of steppes, semi-deserts, deserts, forests, and shrub vegetation are located to the north of the mountains within 42°–48° N and 38°–49° E (Dokuchaev, 1951). Ideas about generally the accepted parallels and meridians along which systems with increased geodynamic activity stretch are formulated within the framework of the zonal concept of nature. Latitudinal mountain belts clearly belong to the 36°–60° parallels on some continents and include a wide range of landscapes and conditions of soil cover formation. It is well known that within 30°–40° N, the atmospheric pressure is at its maximum, and these latitudes are called roaring latitudes, because winds that blow from them are transformed into catastrophic storms that affect the development of aridization and desertification.

中文翻译：

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俄罗斯欧洲南部的土壤地理现象

摘要

欧洲俄罗斯的南部包括两个大陆形成海之间的区域：西北部的黑海和东南部的里海。高加索山脉以多样化的地形为特征，在这些海域之间沿海底方向延伸，总距离超过 1500 公里。草原、半沙漠、沙漠、森林和灌木植被的温带和亚热带带位于北纬 42° 至 48° 和东经 38° 至 49° 的山脉以北（Dokuchaev，1951）。关于普遍接受的平行线和子午线的想法，地球动力学活动增加的系统沿着这些平行线和子午线延伸，是在自然的带状概念框架内制定的。纬度山带明显属于某些大陆的 36°–60° 纬线，包括范围广泛的地貌和土壤覆盖形成条件。众所周知，在北纬30°～40°范围内，大气压力最大，这些纬度被称为咆哮纬度，因为从那里吹来的风会转化为灾难性的风暴，影响干旱化和荒漠化的发展。