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首页> 外文期刊>Soil & Tillage Research >Fly-ash distribution to assess erosion and deposition in an Illinois landscape.
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Fly-ash distribution to assess erosion and deposition in an Illinois landscape.

机译:粉煤灰分布,以评估伊利诺伊州景观中的侵蚀和沉积。

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摘要

Fly ash, the particulate matter resulting from high temperature combustion of coal, was historically dispersed into the atmosphere and settled as fly-ash spheres on the surface soil from a variety of boilers, including those of steam locomotives and steam-powered farm machinery. In Central Illinois, fly ash provides a time marker extending back to 1850s, coinciding with the development of railroads and cultivation. Two railroads, the primary sources of fly ash, were constructed just south of the Cahokia study site in 1852 and 1854. The objectives of this study were to determine: (1) the distribution, depth of occurrence and the total amount of fly ash present in soil profiles on stable, cultivated and uncultivated summit sites with little or no soil erosion; (2) the effects of elevation, aspect, slope gradient, landscape position, distance from source, past vegetation and time on the amount and depth of fly ash; (3) the effects of erosion on sloping sideslopes; and (4) the amount of deposition of fly-ash rich sediment on footslopes and toeslopes. Total fly-ash content of soil was similar for stable, cultivated and uncultivated summits. Two mound sideslopes maintained a high amount of fly ash because of a lack of cultivation and erosion for the past 80 or more years. Erosion reduced the depth of occurrence and the amount of fly ash present on cultivated sideslopes. It appeared that fly-ash content was initially deposited uniformly within the local landscape even though there were slight variations in the aspect, elevation, slope gradient, and distance from the source. The erosion phases of the soils on all landscape positions were determined based on the amount of fly ash remaining in soil surface layers. Accelerated erosion of cultivated sideslopes resulted in the deposition of fly-ash rich sediment on the adjacent footslopes or toeslopes. The proposed fly-ash method provides a tool to assess the extent of soil translocation from a cultivated landscape and subsequent deposition..
机译:粉煤灰是由煤的高温燃烧产生的颗粒物,历来被散布到大气中,并以粉煤灰球的形式从各种锅炉(包括蒸汽机车和以蒸汽为动力的农用机械的锅炉)中沉淀出来。在伊利诺伊州中部,粉煤灰提供了一个可以追溯到1850年代的时标,与铁路和耕种的发展相吻合。两条铁路是粉煤灰的主要来源,分别于1852年和1854年在卡奥基亚研究基地的南部建造。该研究的目的是确定:(1)粉煤灰的分布,发生深度和总量在稳定的,耕种的和未耕种的山顶地点的土壤剖面中,土壤侵蚀很少或没有; (2)海拔,纵横比,坡度,景观位置,距源的距离,既往植被和时间对粉煤灰数量和深度的影响; (3)侵蚀对倾斜的边坡的影响; (4)在山坡和脚趾坡上沉积有飞灰的沉积物的量。稳定,耕种和未耕种的山顶土壤总飞灰含量相似。由于过去80或80多年的耕种和侵蚀缺乏,两个土墩的边坡保持了大量的粉煤灰。侵蚀减少了耕作边坡的发生深度和粉煤灰的数量。看起来飞灰含量最初是均匀地沉积在局部景观中的,即使在外观,高程,坡度梯度和距源的距离上有微小变化。根据土壤表层中残留的飞灰量,确定所有景观位置的土壤侵蚀阶段。耕地边坡的加速侵蚀导致富含粉煤灰的沉积物沉积在相邻的山坡或脚趾坡上。提出的粉煤灰方法提供了一种工具,可以评估耕地景观中土壤移位的程度以及随后的沉积情况。

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