首页> 外文期刊>Polish Journal of Soil Science >STABILITY AND SORPTIVITY OF SOIL AGGREGATES IN GRASSED AND CULTIVATED SLOPING VINEYARDS
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STABILITY AND SORPTIVITY OF SOIL AGGREGATES IN GRASSED AND CULTIVATED SLOPING VINEYARDS

机译:牧草和耕作坡地土壤团聚体的稳定性和可比性

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摘要

The physical characteristics of soil aggregates influence soil tilth, surface sealing, water infiltration and root growth. Soil management and compaction significantly affect these characteristics. The aim of this work was to determine the effects oftractor traffic across the slope on bulk density, water stability, tensile strength and sorptivity of aggregates from grass covered and cultivated sloping (18%) vineyard soils. The grass covered (G) treatment included periodical mowing and cutting back of herbage and cultivation (C) treatment consisting of autumn ploughing (18 cm) and spring and summer rotary hoeing in the vineyard inter-row zones (2.7 m). A crawler tractor (2.82 Mg) was used in the inter-row zones, moving across the slope for all tillage and chemical operations. Soil aggregates were taken from the inter-rut and the upper and lower rut areas (0-10 and 20-30 cm) in the inter-row zones and then air-dried. Bulk density and tensile strength were lowest in the inter-rut areas and highest inthe lower crawler rut. Aggregate water stability was greater under the lower rut and sorptivity in the inter-rut area in comparison to the remaining inter-row areas. In comparable inter-row areas, water stability and sorptivity of soil aggregates were greater and lower under G than C, respectively. The differences in bulk density and tensile strength between G and C were not consistent and varied depending on the inter-row zone and depth.
机译:土壤团聚体的物理特性会影响土壤的倾斜度,表面密封性,水分渗透和根系生长。土壤管理和压实作用显着影响这些特性。这项工作的目的是确定横跨山坡的牵引车流量对草覆盖和耕种的倾斜(18%)葡萄园土壤聚集体的堆积密度,水稳定性,抗张强度和吸水性的影响。草覆盖(G)处理包括定期割草和剪草,耕种(C)处理包括在葡萄园行间区域(2.7 m)进行秋季耕作(18 cm)和春季和夏季旋转。行间区域使用了履带式拖拉机(2.82 Mg),在所有耕作和化学操作中都横过斜坡移动。从行间区域的车辙间和上,下车辙区域(0-10和20-30 cm)中采集土壤团聚体,然后风干。在车辙间区域的堆积密度和抗拉强度最低,而在较低的履带车辙中最高。与其余的行间区域相比,在车辙间区域较低的车辙和吸水性下,总水稳定性更高。在可比较的行间区域,G下土壤团聚体的水稳定性和吸附性分别高于C和C。 G和C之间的堆积密度和拉伸强度的差异不一致,并且取决于行间区域和深度而变化。

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