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INFLUENCE OF COVER CROPS AND GRAZING ON SOIL PHYSICAL PROPERTIES IN SAVANNA SOIL

机译:覆草和放牧对草地沙地土壤理化性质的影响。

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Production systems based on single crops and grazing of crop leftovers have produced grave soil degradation problems in soils of Venezuelan savannas. As alternatives to prevent degradation and improve the quality of these soils, some conservation management systems have been proposed. With the objective of evaluating changes in physical properties of a typical soil of a natural savanna, from use of cover crops (Brachiaria dictyoneura and Centrosema macrocarpum) as residues for direct corn (Zea mays L.) sowing and later grazing with cattle, a trial was set up in a soil classified as Typic Plinthustults, located in the savannas of Guárico (Venezuela). The initial physical characteristics of natural savanna soils were characterized, before establishing the trial (2002) and the following were evaluated in samples collected in each plot (in two seasons of the 2006-2007 cycle; before and after grazing): bulk density, saturated hydraulic conductivity, porosity and its distribution, resistance to mechanical penetration, and humidity volume content, in samples taken at 0 to 5 and 5 to 15 cm of depth, in each parcel. Analysis of the results indicates that there were statistical differences in the physical properties evaluated, which could be due to the cover crop and the season; especially bulk density, saturated hydraulic conductivity, total porosity and mechanical resistance. The best physical conditions were present in the superficial layer of the soil (0 to 5 cm) and in the B. dictyoneura cover.
机译:以单一农作物为基础的生产系统和农作物剩余的放牧方式在委内瑞拉大草原的土壤中产生了严重的土壤退化问题。作为防止退化和改善这些土壤质量的替代方法,已经提出了一些保护管理系统。为了评估天然稀树草原典型土壤的物理性质的变化,将覆盖农作物(Brachiaria dictyoneura和Centrosema macrocarpum)用作直接播种玉米(Zea mays L.)的残留物,然后再与牛放牧,进行了一项试验是在瓜里科(委内瑞拉)的稀树草原上被分类为典型的典型土壤的土壤中建立的。在建立试验之前,先对天然稀树草原土壤的初始物理特性进行了表征(2002年),然后在每个样地(2006-2007年周期的两个季节;放牧前后)中对每个样品收集的样品进行了以下评估:堆积密度,饱和在每个包裹中以0至5和5至15厘米深度采集的样品中的水导率,孔隙率及其分布,抗机械渗透性和湿度体积含量。对结果的分析表明,所评估的物理特性存在统计差异,这可能是由于覆盖作物和季节造成的;特别是堆积密度,饱和导水率,总孔隙率和机械阻力。最佳物理条件出现在土壤表层(0至5厘米)和双歧杆菌中。

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