Soil Resources of Southern Siberia

IF 0.3 Q4 GEOGRAPHY Geography and Natural Resources Pub Date : 2024-03-22 DOI:10.1134/s1875372823040030
O. I. Bazhenova, E. M. Tyumentseva, A. A. Cherkashina, V. A. Golubtsov, S. A. Tukhta
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Abstract

The article considers the issues of soil degradation and the possibility of conserving and restoring soil fertility in southern regions of Siberia. Long-term stationary research data is synthesized in order to determine the mechanism of erosion processes and obtain quantitative data on soil losses depending on key factors of water and wind erosion. Particular attention is given to the periodically extreme nature of processes that cause catastrophic soil degradation. Patterns of changes in the structure of processes that require agricultural soil conservation measures are revealed. The mechanism of soil erosion and soil degradation rate changes in the west to east direction along the belt of steppes and forest–steppes of southern Siberia. In the south of Western Siberia, the pressing issue is protecting soils from thawing erosion, in Khakassia the particular hazard is soil deflation, and in Cis-Baikal and Transbaikal region soil degradation is exacerbated by the combined effect of rainfall erosion and deflation. The results of a quantitative cartographic assessment of erosion hazard levels based on empirical models of potential soil loss and deflation are presented for the major agricultural regions with a case study of the Irkutsk–Cheremkhovo plain and the Nazarovskaya and Yuzhno-Minusinskaya depressions. A decrease in erosion soil losses as a result of socioeconomic agriculture reforms and a significant reduction in the area of agricultural land in the early 1990s and in the post-reform period (2010–2017) are noted. It is emphasized that the re-expansion of agricultural land observed in recent years creates the necessity of large-scale inventory mapping of erosion processes in southern Siberia. That data can be used to select an optimal nature management policy that promotes conservation of soil resources.

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南西伯利亚的土壤资源
摘要 本文探讨了西伯利亚南部地区的土壤退化问题以及保护和恢复土壤肥力的可能性。文章综合了长期固定研究数据,以确定侵蚀过程的机理,并根据水蚀和风蚀的关键因素获得土壤流失的定量数据。特别关注造成灾难性土壤退化的周期性极端过程。揭示了需要采取农业水土保持措施的过程结构的变化规律。沿着西伯利亚南部的草原和森林草原带,土壤侵蚀机制和土壤退化速度自西向东发生变化。在西西伯利亚南部,亟待解决的问题是保护土壤免受解冻侵蚀;在哈卡西亚,特别的危害是土壤塌陷;在西斯-贝加尔和外贝加尔地区,降雨侵蚀和塌陷的共同作用加剧了土壤退化。以伊尔库茨克-切列姆霍沃平原、纳扎罗夫斯卡娅洼地和尤日诺-米尼辛斯卡娅洼地为例,介绍了根据潜在土壤流失和塌陷的经验模型对主要农业区水土流失危害程度进行定量制图评估的结果。报告指出,由于社会经济农业改革,土壤侵蚀损失减少,20 世纪 90 年代初和改革后时期(2010-2017 年)的农业用地面积大幅减少。需要强调的是,近年来农业用地的重新扩大使得有必要对西伯利亚南部的水土流失过程进行大规模的清查测绘。这些数据可用于选择促进土壤资源保护的最佳自然管理政策。
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来源期刊
CiteScore
0.50
自引率
0.00%
发文量
24
期刊介绍: Geography and Natural Resources  publishes information on research results in the field of geographical studies of nature, the economy, and the population. It provides ample coverage of the geographical aspects related to solving major economic problems, with special emphasis on regional nature management and environmental protection, geographical forecasting, integral regional research developments, modelling of natural processes, and on the advancement of mapping techniques. The journal publishes contributions on monitoring studies, geographical research abroad, as well as discussions on the theory of science.
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