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Response of a clay loam agricultural soil to mechanical stress from tractor traffic with and without slip

机译:粘土壤土农业土壤与拖拉机交通的机械压力的反应

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Agricultural wheeled tractors apply traction force by means of a stress-strain interaction between tyres and topsoil. The traction force and wheel slip of the tractor exert a noticeable effect on the soil stress state, and hence on soil deformation. In this study, changes to soil physical and hydraulic properties owing to deformation caused by the passage of a mechanical front wheel drive (MFWD) tractor (65 kW engine power), both when self-propelled without wheel slip and with high traction force and wheel slip, were compared in a clay loam (Albic luvisol) agricultural field. An analytical soil-tyre interaction model, adapted for a MFWD vehicle, was used to simulate the stress state at the soil-tyre contact surface. Effects of the different stress states on the soil were analysed in terms of changes in total porosity (TP), pore size distribution (PSD), and saturated water conductivity K_(sat). Results clearly showed that the stress state at the soil-tyre contact significantly rose when the tractor moved with slip than when it moved without slip, mostly in terms of shear stress (from 6.0 to 61.6 kPa at the soil-rear tyre contact surface). As a consequence, the severity of soil degradation owing to tractor traffic increased significantly. Changes in soil structure and soil hydraulic properties were more pronounced in the first 0.15 m, where TP decreased from 53.8% to 43% and macro-pores (Φ> 50μm) fell from 2% to 0% due to the effect of high wheel slip. The K_(sat) at soil surface (0-0.04 m depth) decreased from 10.0 mm/h in the trafficked site without slip, to 0.5 mm/h in the trafficked site with slip, with no significant reduction below this depth. Because macropores play a key role in controlling water movement in the soil and in reducing surface runoff, the change in structure and degradation of hydraulic properties exert a great impact on soil erosion and soil management. The considerable influence of the tractor working condition on soil deformation and degradation needs to gain more attention in the future in order to better develop a proper soil management and prevent soil erosion.
机译:农业轮式拖拉机通过轮胎和表土之间的应力 - 应变相互作用应用牵引力。拖拉机的牵引力和车轮滑动对土壤应力状态发出明显的影响,因此对土壤变形。在这项研究中,由于机械前轮驱动器(MFWD)拖拉机(65 kW发动机电源)的变形而改变了土壤物理和液压特性,这两者都是在没有车轮滑动和高牵引力和车轮滑动,在粘土壤土(alAlc洛维斯)农业领域进行比较。使用适用于MFWD载体的分析土壤轮胎相互作用模型,用于在土轮胎接触表面处模拟应力状态。在总孔隙率(TP),孔径分布(PSD)和饱和导电性K_(SAT)的变化方面分析了不同应激状态对土壤的影响。结果清楚地表明,当拖拉机用滑动机移动时,土轮胎接触处的应力状态显着上升,而不是在没有滑动的情况下移动时,主要是在剪切应力(在土壤后轮胎接触表面处的6.0至61.6kPa。因此,由于拖拉机交通的土壤退化严重程度显着增加。在前0.15米中,土壤结构和土壤液压性能的变化更加明显,其中TP从53.8%降至43%,宏观孔(φ>50μm)由于高轮滑的效果,从2%降至0%。 。土壤表面(0-0.04米深度)的K_(SAT)在随着贩运部位的10.0毫米/小时下降,无需滑动,在被贩运部位的速度下降至0.5毫米/小时,并且在该深度以下没有显着降低。因为大孔在控制土壤中的水运动和降低表面径流方面发挥着关键作用,因此液压性能的结构变化和液压性能的降解对土壤侵蚀和土壤管理产生了重大影响。拖拉机工作条件对土壤变形和降解的相当大的影响需要在未来获得更多关注,以便更好地发展适当的土壤管理,防止土壤侵蚀。

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