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Reduzierte Bodenbearbeitung reichert Humus und mikrobielleudBiomasse oberflächlich an

机译:减少耕作可丰富腐殖质和微生物表面生物量

摘要

When residues and organic fertilizers are not incorporated into the soil, they build a top soil layer that is enriched in soil organic matter. This is leading to a soil layer withudincreased biological activity, while the soil layers below, receive less inputs in form of residues or manures and show a reduction in soil organic matter and biological activity. Soils from a replicated field trial and two on-farm trials were analysed for biological soil quality 6 years after the implementation of reduced tillage (RT) as compared to plough. Whilst crop yields were slightly lower with RT, weed cover was increasing, but not to a level that would compromise yields. Soils under RT accumulated soil organic matter in the tilled top layer of 0-10 cm, while in the layer below either no change or a decrease as compared to the plough system was found. The same was true for microbial biomass, but the difference between RT and plough became more pronounced. Dehydrogenase activity was found to react most to the tillage induced changes. Accumulated soil organic matter, living and active organisms at the soil surface render soils more resistant to the weather impact.
机译:当残留物和有机肥料未掺入土壤时,它们会在土壤顶层形成一层富含​​土壤有机质的土壤。这将导致土壤层的生物活性降低,而下面的土壤层则以残留物或肥料的形式接受较少的投入,并降低了土壤有机质和生物活性。与耕作相比,实施减耕(RT)6年后,对重复田间试验和两次农场试验中的土壤的生物土壤质量进行了分析。尽管RT导致农作物单产略低,但杂草覆盖率却在增加,但不会降低到单产的水平。 RT下的土壤在耕作的顶层0-10 cm处积累了土壤有机质,而在下层则与耕作系统相比没有变化或减少。微生物生物量也是如此,但是RT和犁之间的差异变得更加明显。发现脱氢酶活性对耕作引起的变化反应最大。土壤表面累积的土壤有机质,生物和活性生物使土壤更能抵抗天气的影响。

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