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Soil physical parameters of a recently established agricultural recultivation site after brown coal mining in Eastern Germany

机译:德国东部褐煤开采后最近建立的农业复垦点的土壤物理参数

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Our study deals with agricultural recultivation of open cast brown coal mining areas in Lusatia, Eastern Germany. In this region the largest brown coal (lignite) mining area of Germany is located. Lignite mining activities lead to major disturbances of the landscape. Recultivation efforts attempt to regenerate mining areas for agricultural land use options. The geological "parent" material is of saaleian origin, has a sandy texture and was excavated from several meters depths before mining and is now used for recultivating the excavated area. Consequently, it is free of recent soil organic carbon. The substrate itself is unstructured. The partly wet or dry substrate is subjected to strong mechanical stresses during the excavation, deposition, refilling and levelling processes throughout the year. This practice leads to more or less compacted soils/substrates which may result in small yields of agricultural crops. In this context we investigate the effect of different organic soil additives in combination with different recultivation crop rotations on the development of soil structure for improved agricultural land use. Our experimental site has been heaped up and levelled off in 2006 and 2007. On each of the 24 experimental sub areas undisturbed soil samples have been taken to characterise the substrates according to their mechanical and hydraulic parameters and to determine the scattering of these parameters on a site that is assumed to be recultivated as homogenously as possible. First results of our ongoing experimental study indicate that the soil physical properties such as texture, bulk density, precompression stress, air permeability and saturated hydraulic conductivity are not identical on each of the 24 subplots. The soil physical properties behave differently in relation to each other. E.g. we found a negative correlation between bulk density (similar to 1.35-similar to 1.90 g/cm(3)) and precompression stress (similar to 30-70 kPa) and no decisive interrelation between bulk density and air permeability or saturated hydraulic conductivity. 2010 Elsevier B.V. All rights reserved.
机译:我们的研究涉及德国东部卢萨蒂亚(Lusatia)露天褐煤开采区的农业复垦。该地区是德国最大的褐煤(褐煤)开采区。褐煤开采活动导致景观的重大扰动。耕种工作试图使采矿区再生为农业用地选择。地质上的“母体”材料是萨利族起源的,具有沙质质地,在开采前从几米深处开挖,现在用于开挖区域的重新耕作。因此,它不含近期的土壤有机碳。基材本身是非结构化的。一年中,部分潮湿或干燥的基材在开挖,沉积,重新填充和找平过程中会承受强烈的机械应力。这种做法导致或多或少的土壤/基质被压实,这可能导致农作物的单产降低。在这种情况下,我们调查了不同有机土壤添加剂与不同耕作作物轮作组合对土壤结构发展的影响,以改善农业用地。我们的实验场地已于2006年和2007年堆积并夷为平地。在24个实验子区域的每一个上,均采集了未扰动的土壤样品,以根据其机械和水力参数表征基质,并确定这些参数在地面上的散射。假定尽可能均匀地重新培养的位点。我们正在进行的实验研究的初步结果表明,在24个子图上,每个土壤的物理特性(例如质地,堆积密度,预压缩应力,透气性和饱和导水率)都不相同。土壤物理性质彼此之间表现不同。例如。我们发现堆积密度(类似于1.35类似于1.90 g / cm(3))与预压缩应力(类似于30-70 kPa)之间呈负相关,并且堆积密度与透气性或饱和水力传导率之间没有决定性的相互关系。 2010 Elsevier B.V.保留所有权利。

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