中伏尔加河地区米克拉舍夫斯基聚落中部埋藏土

I. Spiridonova, S. Lomov
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引用次数: 0

摘要

Maklasheevsky II定居点是一个复杂的考古遗址,其中包括铁器时代早期和中世纪早期的定居点,相隔六百多年的自然发展和人为结构的转变。马克拉舍夫斯基II古定居点是一个比水库高10米的梯田的遗迹,上面保存着铁器时代早期和中世纪早期的防御结构(3.0米高)。从起源上看,这个物体是一个自然和人为的地质系统。在Maklasheevsky II II聚落中部的自然发育时期,土壤形成以相对平坦的表面为主,并形成欠发达的土壤-碳酸盐岩,随后被洪积物掩埋。在埋藏的土壤中,与重叠的雨淋层相比,结构和抗水性的改善是明显的,可以很好地估计。此外,腐殖质的含碳量增加了近1.5倍,实际酸度降至中性,水解酸度增加。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Buried soils of the middle part Miklashevsky II settlement (Middle Volga region)
Maklasheevsky II settlement is a complex archaeological site, which includes settlements of the early Iron Age and the early Middle Ages, separated by more than six hundred years of natural development and transformation of anthropogenic structures. Maklasheevsky II ancient settlement is a remnant of a terrace 10 m high above the reservoir level and the defensive structures (3.0 m high) of the Early Iron Age and the early Middle Ages preserved on it. By origin, this object is a natural and anthropogenic geosystem. During the period of natural development of the middle part of the Maklasheevsky II settlement, soil formation prevailed on relatively flat surfaces and the formation of underdeveloped soils – sod-carbonate, subsequently buried by deluvium. In buried soils, an improvement in structure and water resistance is noticeable, up to a good estimate, in comparison with overlapping deluvium. In addition, there was an increase in the carbon content of humus by almost 1.5 times, the actual acidity decreased to neutral, the hydrolytic acidity increased, compared with overlapping deluvium.
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