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首页> 外文期刊>Moscow University Soil Science Bulletin >Physical, chemical, and mineralogical characteristics of steppe paleosols of the ural region.
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Physical, chemical, and mineralogical characteristics of steppe paleosols of the ural region.

机译:乌拉尔地区草原古土壤的物理,化学和矿物学特征。

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摘要

Investigation of paleosols with different ages of burial mounds and the unique fortified city of Arkhaim in the steppe zone of the Southern Trans-Urals (Chelyabinsk region) is carried out. They are located on the remnants of the Big Karaganka River valley. The time of construction of archaeological monuments dates back to the Early Iron Age (Sarmatian Culture, 2300-2200 years ago) and Middle Bronze Age (Sintashta culture, 3800-4100 years ago). The soils are of medium and light loamy granulometric composition. Morphological, chemical, and mineralogical investigations of paleosols and background soils indicate that, in the Sarmatian time, the climatic conditions in the region were drier than currently, while during the Sintashta cultural development, the climate of the region was similar to the present one.Notes Translated from Vestnik Moskovskogo Universiteta. Pochvovedenie (2013) (1), 13-22 (Ru).
机译:在南部Trans-Urals(车里雅宾斯克州)草原地区,调查了不同年龄的古坟和独特的设防城市Arkhaim的古土壤。它们位于大卡拉甘卡河谷的残余地区。考古纪念碑的建造时间可以追溯到早期铁器时代(2300-2200年前的萨尔玛文化)和中古铜器时代(3800-4100年前的新达斯塔文化)。土壤具有中等和轻质的壤质组成。对古土壤和本底土壤的形态,化学和矿物学研究表明,在萨尔马提时期,该地区的气候条件比目前更干燥,而在Sintashta文化发展期间,该地区的气候与现在的相似。注释摘自Vestnik Moskovskogo Universiteta。 Pochvovedenie(2013)(1),13-22(Ru)。

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