青铜器时代人为影响下草原地区小型考古聚落的土壤

L. Plekhanova
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摘要

“自然成土/土壤科学的当代方向是古代的人为影响和气候波动变化。河谷中的大量聚落是独特的对象,具有悠久的发展历史和现代土壤覆盖的形成。我们研究了青铜器时代的一个小定居点扎里亚的住所之间的土壤。该定居点是青铜时代早期大型设防城市Sarym-Sakla的养牛(马、牛和羊)经济区的一部分,Sarym-Sakla是该国跨乌拉尔高原的原始伊朗城市之一。古代社会活动在宏观和微观尺度上改变了陆地生态系统的功能。微地形形态异质性的增加导致了土壤覆盖的多样性。在微高程和微洼地发现了不同寻常的土壤类型。揭示了文化层中磷化合物的富集,并证实了该地区低漫滩阶地土壤覆盖层中黑钙土-茄钙土“反向”比例的形成是由于古代人类压力和气候干旱化的几个阶段的结果。我们着重于测定有机碳含量、磁化率、盐组成、阳离子交换容量以及沿土壤剖面的流动磷酸盐分布,作为古代人为影响的可能指标。在人为影响过程中土壤性质的变化程度与其在几个世纪甚至几千年的自然演变过程中的变化程度是相称的。过去的人为变化在土壤覆盖发展的历史上留下了印记,预先决定了退化现象的现代危险。此外,我们在生态系统形成的历史中得出了相似之处,并概述了进一步研究的任务。”
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SOILS OF SMALL ARCHAEOLOGICAL SETTLEMENTS IN THE STEPPE ZONE AS A RESULT OF BRONZE AGE ANTHROPOGENIC IMPACT
"The contemporary direction of natural pedogenesis/soil science is ancient anthropogenic impact and climate fluctuations changes. A large number of settlements in the river valleys are unique objects with a long history of development and modern soil cover formation. We studied the soil between the dwellings for a small settlement Zarya of the Bronze Age. The settlement was part of the economic zone of cattle breeding (horses and cows and sheep) of the large early Bronze Age fortified city Sarym-Sakla, one of the country's Proto-Iranian Cities of the Trans-Ural Plateau. The activity of ancient societies changed the terrestrial ecosystem functioning at macro and microscales. Increased heterogeneity of microrelief forms led to the diversity of soil cover. We found the unusual soil types on microelevations and microdepressions. The enrichment of the cultural layer with phosphorus compounds was revealed, and the hypothesis of the formation of a ""reverse"" ratio of chernozems-solonetzes of the soil cover of the low above-floodplain terrace as a consequence of several stages of ancient anthropogenic pressure and climatic aridization was confirmed in this area. We focused on the determination of organic carbon content, magnetic susceptibility, salt composition, cation exchange capacity, and the distribution of mobile phosphates along the soil profile as possible indicators of ancient anthropogenic influence. The degree of soil properties changes during the anthropogenic impact is commensurate with their transformation in the natural evolution of centuries and even several millennia. Past anthropogenic changes leave a mark in the history of the development of the soil cover predetermining the modern danger of the degradation phenomena. Moreover, we draw parallels in the history of ecosystems formation and outlined tasks for further research."
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