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Reassessment of tillage erosion rates by manual tillage on steep slopes in northern Thailand
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机译:在泰国北部陡坡上通过人工耕作对耕作侵蚀率的重新评估
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摘要
Changing land-use practices in northern Thailand have increased tillage intensity. This study re-assesses the rate of tillage erosion by manual hoeing on steep slopes (17-82%) in northern Thailand. Previously collected soil translocation data during an on-farm tillage erosion experiment and additionally collected data during an on-farm tillage erosion survey have been analysed whereby a new calculation method (i.e. trapezoid tillage step) has been used. A comparison with previously collected data indicates that the trapezoid tillage step method and the tracer method are the most reliable methods to assess downslope translocation by manual tillage. Based on newly acquired understanding of the processes involved, soil fluxes by tillage erosion are quantified by linear functions for different slope gradient classes rather than one single diffusion-type equation for the whole slope range. For slope gradients smaller than 3%, soil fluxes are close to zero as farmers do not have a preferred tillage direction. For slope gradients between 3% and 70%, soil is tilled only in the downslope direction and soil fluxes range between 16 and 67 kg m(-1) tillage pass(-1). On slopes with gradients in excess of 70%, the angle of repose for soil clods is often exceeded resulting in a sliding down of the complete tilled top layer. These data are used to assess the soil flux for complete cropping cycles for the most dominant cropping systems in the highlands of northern Thailand: i.e. upland rice, maize, (soy) beans, cabbage and ginger. The on-site effects of tillage erosion will be, very pronounced if parcels are short with respect to their slope length, cultivated for upland rice or cabbage, or when weed pressure is high. Tillage erosion results in a tillage step with low soil fertility and low infiltration capacity. Solutions to reduce tillage erosion intensity depend on the degree that tillage intensity can be reduced. This might happen by an improved weed management or by changing landuse to perrenial cropping. Other strategies are concentrating nutrients on the truncated hillslope sections and retaining soil on the held by vegetative buffers. (C) 1999 Elsevier Science B.V. All rights reserved.
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机译:泰国北部不断变化的土地利用方式增加了耕作强度。这项研究通过在泰国北部的陡坡(17-82%)上进行人工耕来重新评估耕作侵蚀的速率。在农场耕作侵蚀实验期间先前收集的土壤移位数据以及在农场耕作侵蚀调查期间另外收集的数据已经过分析,从而使用了新的计算方法(梯形耕作步骤)。与以前收集的数据进行比较表明,梯形耕作分步法和示踪法是通过人工耕作评估下坡易位的最可靠方法。基于对所涉及过程的最新了解,耕作侵蚀造成的土壤通量通过线性函数对不同的坡度梯度类别进行量化,而不是对整个坡度范围采用单一的扩散类型方程式进行量化。对于坡度小于3%的坡度,由于农民没有偏爱的耕作方向,土壤通量接近于零。对于介于3%和70%之间的坡度,土壤仅在下坡方向耕作,土壤通量在16至67 kg m(-1)耕作通行证(-1)之间。在坡度超过70%的斜坡上,经常会超过土壤凝块的休止角,从而导致完整耕作的顶层滑落。这些数据用于评估泰国北部高地最主要的种植系统(即旱稻,玉米,(大豆)豆,白菜和姜)整个种植周期的土壤通量。如果包裹的坡度相对较短,耕种为旱稻或白菜或杂草压力高时,耕作侵蚀的现场影响将非常明显。耕作侵蚀导致耕作步骤,土壤肥力低,渗透力低。减少耕作侵蚀强度的解决方案取决于耕作强度可以降低的程度。这可能是由于改善了杂草管理或将土地利用改为了多年生作物而发生的。其他策略是将营养物集中在截断的山坡部分上,并将土壤保留在营养缓冲带上。 (C)1999 Elsevier Science B.V.保留所有权利。
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