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Soil compaction influences soil physical quality and soybean yield under long-term no-tillage

机译:长期免耕下土壤板结影响土壤物质和大豆产量

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摘要

Soil compaction under no-tillage (NT) exerts a negative impact on the soil physical quality. The objective of this study was to quantify the influence of compaction on soil's physical quality and soybean crop yield in a Rhodic Ferralsol under NT in southern Brazil. Soil compaction was established through an increasing number of passes (0, 3, 6, and 9 passes) by a 4510 kg tractor, which promoted a degree of compactness of 84, 89, 94, and 99, respectively. Undisturbed soil samples were taken from depths of 0.0-0.1 and 0.1-0.2 m from row (R) and interrow (IR) after soybean harvests in 2014 and 2015 seasons. Soil bulk density (Bd) and least limiting water range (LLWR) were then determined. Also, soybean yields were evaluated. The contrast in Bd and LLWR observed between R and IR positions was restricted to the 0.0-0.1 m soil depth layer. The assessment of LLWR under NT must consider the sampling positions. The increase in the degree of compactness promoted soil physical quality degradation and decreasing soybean yield (up to 12 and 19 for 2013 and 2014 seasons, respectively). The LLWR has been correlated to soybean yield and could be a useful tool for soil management practices.
机译:免耕(NT)下的土壤板结对土壤物理质量产生负面影响。本研究旨在量化压实对巴西南部北领地红鳍鲷土壤物理品质和大豆作物产量的影响。4510 kg 拖拉机通过增加通过(0、3、6 和 9 次)的通过建立土壤压实度,这促进了 84%、89%、94% 和 99% 的密实度。在2014年和2015年大豆收获后,从行(R)和行间(IR)的0.0-0.1和0.1-0.2 m深度采集未受干扰的土壤样品。然后测定土壤容重(Bd)和最小极限水位(LLWR)。此外,还评估了大豆产量。R和IR位置之间观察到的Bd和LLWR的对比度仅限于0.0-0.1 m土壤深度层。NT下LLWR的评估必须考虑抽样位置。紧结度的增加促进了土壤物理质量的退化和大豆产量的下降(2013年和2014年分别高达12%和19%)。LLWR与大豆产量相关,可以成为土壤管理实践的有用工具。

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