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Timing and Causes of the Origin of the Solonetz Process in the Desert-Steppe Soils of the Southeastern Russian Plain

机译:Solonetz过程中俄罗斯平原沙漠草原土壤起源的时序及原因

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The article discusses the time frame and the role of the anthropogenic factor in the solonetz process in soils of the desert-steppe zone of the southeastern Russian Plain. Based on the study of soils of different ages buried under the mounds of the Bronze and Middle Ages (6200-700 years ago) within the Salsko-Manych ridge, it was established that the soils of the region did not bear signs of the solonetz process at the macro level before the beginning of the 3rd millennium BC. The first solonetzes in the region began to form 4800-4700 years ago. Their appearance chronologically coincided with the beginning of increased climate aridization. During this period, desert steppes began to be actively inhabited by ancient cattle breeders specializing in breeding small cattle, which resulted in a sharp increase in the load on the soils and ecosystems of the steppe. The article considers the possible cause-effect relationships in the system "climate-economic model-solonetz process."
机译:本文讨论了人为因子在俄罗斯平原沙漠草原区土壤中索妥茨工艺中的人为框架和作用。 根据萨尔斯科 - 多年(6200-700年前)在萨尔斯科 - 多年山脉下埋藏的不同年龄的土壤的研究,建立了该地区的土壤不承担Solonetz过程的迹象 在BC第三千年开始前的宏观水平。 该地区的第一个Solonetzes开始形成4800-4700年前。 他们的外表时间按时间顺序地恰逢加剧的增加的开始。 在此期间,沙漠草原开始被专门从事育种小牛的古代牛育种者积极居住,这导致草原土壤和生态系统的负荷急剧增加。 本文认为系统中可能的致命关系“气候 - 经济模型 - Solonetz过程”。

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