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Long-term wheat-soybean successions affecting the cover and soil management factor in USLE, under subtropical climate

机译:在亚热带气候下,影响封面和土壤管理因子的长期小麦大豆演替

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Vegetation cover and soil management influence the magnitude of soil losses. In the Universal Soil Loss Equation (USLE), cover and management are represented by the C factor, as it is the easiest factor to manage to reduce loss of soil and water in agricultural areas. This study aimed to determine the C factor of a succession of wheat (Triticum aestivum L.) followed by soybean (Glycine max) under conventional tillage, reduced tillage, and no-tillage. For this, data of soil losses obtained in the field, under natural rainfall conditions, in a long-term experiment that lasted for 13 years were used. The cycle of both crops was divided into five stages with different time intervals between winter and summer, which resulted in ten periods per year constituting the succession. The C factor values varied widely among the treatments and the stages during the crop cycle, and they were influenced mainly by the rainfall distribution of the region, growth of the vegetation and soil disturbance level. By the end of the 13 years of experimentation, the C factor of the wheat-soybean succession under conventional tillage was 0.1576, 0.0407 under reduced tillage, and 0.0368 under no-tillage.
机译:植被覆盖,土壤管理,将影响土壤损失的规模。在通用土壤流失方程(USLE),盖和管理由C因子为代表,因为它是管理,以减少农业区的土壤和水的损失的最简单的因素。本研究旨在确定小麦一连串的C-因子(普通小麦),随后通过常规的耕作下大豆(Glycine max),减少耕作和免耕。为此,在该领域获得的土壤流失数据,自然降水条件下,在持续使用13年的长期试验。两种作物的周期分为冬季和夏季之间的不同的时间间隔,这导致构成连续每年10个期间五个阶段。的C因子值作物周期期间的治疗和各个阶段之间相差很大,他们被该地区的雨量分布主要影响,植被和土壤扰动水平的增长。通过13年的实验结束时,传统耕作小麦大豆演替的C-因子为0.1576,0.0407下减少耕作,和0.0368免耕。

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