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首页> 外文期刊>Soil & Tillage Research >Significance of soil erosion on soil surface roughness decay after tillage operations.
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Significance of soil erosion on soil surface roughness decay after tillage operations.

机译:耕作后土壤侵蚀对土壤表面粗糙度衰减的意义。

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Soil surface roughness (SSR) indicates a soil's susceptibility to wind and water erosion and it is strongly related to field management practices. Several methods have been developed to capture and evaluate SSR under specific field and climate conditions. Based on previously developed techniques, the shadow analysis method has been shown to be a suitable technique for characterising SSR in the field when used in arid and semi-arid regions of Spain. This is because of the climate and soil conditions that prevail during the spring and summer in the semiarid regions of Spain. However, the method has not yet been used in whole climate and edaphic conditions and still needs further development. Therefore, the goal of this study was to assess the SSR decay of a sandy clay loam soil after fall tillage operations using the shadow analysis method. The experiment was performed in the field in eight controlled 1 m2 plots of a Technosol (FAO, 2006). The project was designed to evaluate the validity of the method for further measuring SSR decay and to overcome potential problems associated with the method. The data were collected from the beginning of the fall of 2009, after tillage operations, through the spring of 2010, when the fields were tilled again. Half of the experimental plots were covered and used as controls. The remainder of the plots was uncovered to evaluate SSR decay mainly associated with water erosion. The average SSR was similar for the two subsets at the beginning of the experiment with 68% and 70%, respectively. The SSR after the experimental trial showed marked differences between the covered (45%) and uncovered plots (20%) after 53.2 mm of rainfall. The parameters demonstrated that the method can be used to study the influence of wind and water erosion on SSR decay at field conditions throughout the year. The shadow analysis technique has the advantages of being non-disturbing, easy to handle and less time consuming than other classical techniques. However, the method presents some limitations and further research must be conducted to adjust for utilisation in the field.Digital Object Identifier http://dx.doi.org/10.1016/j.still.2011.08.006
机译:土壤表面粗糙度(SSR)表明土壤易受风蚀和水蚀的影响,并且与田间管理实践密切相关。已经开发出几种方法来捕获和评估在特定田间和气候条件下的SSR。基于以前开发的技术,阴影分析方法已证明是在西班牙的干旱和半干旱地区使用时表征现场SSR的合适技术。这是由于春季和夏季在西班牙半干旱地区普遍存在的气候和土壤条件。但是,该方法尚未在整个气候和深海条件下使用,仍需要进一步开发。因此,本研究的目的是使用阴影分析方法评估秋季耕作后沙质壤土的SSR衰减。该实验是在野外以8个Technosol受控1 m 2 样地进行的(粮农组织,2006年)。该项目旨在评估进一步测量SSR衰减的方法的有效性,并克服与该方法相关的潜在问题。数据是从2009年秋季开始的,直到耕作结束,直到2010年春季,直到田间再次耕种为止。覆盖了一半的实验地块并用作对照。其余的图未发现以评估主要与水蚀有关的SSR衰减。在实验开始时,两个子集的平均SSR相似,分别为68%和70%。实验试验后的SSR显示,在53.2 mm的降雨后,覆盖地(45%)和未覆盖地(20%)之间存在显着差异。这些参数表明,该方法可用于研究风蚀和水蚀对全年田间条件下SSR衰减的影响。与其他经典技术相比,阴影分析技术具有无干扰,易于处理且耗时少的优点。然而,该方法存在一些局限性,必须进行进一步的研究以适应该领域的应用。数字对象标识符http://dx.doi.org/10.1016/j.still.2011.08.006

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