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Field investigation of compost blankets for erosion control under concentrated flow conditions.

机译:堆肥毯的现场调查,用于在集中流动条件下控制侵蚀。

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Compost blankets are recognized as an effective erosion control practice that has been utilized widely. While previous studies have proven that compost blankets can control erosion as well or better than traditional methods under normal rainfall and sheet flow conditions, little attention has been paid to how compost will respond to concentrated flow conditions. The objective of this research was to investigate erosion processes on compost blankets under concentrated flow conditions. Erosion control compost (ECC), yard waste compost (YWC), and a bare soil (BS, loam) were studied using four concentrated flow rates on 12.5% slope plots. Time to initiate discharge, flow velocity, solids concentration, and total loss of solids were measured. The erosion process and rill evolution under these conditions were observed and recorded. Results indicated that the time elapsed to commence discharge from compost plots was significantly longer than that from soil plots. Large amounts of inflow were able to infiltrate into the compost matrix and flow through it, leaving a smaller portion of surface flow on compost plots than on soil plots. Under high inflow rates (2.7x10-4 and 3.3x10-4 m3/s), solids loss from compost plots was significantly less than those from soil plots. Under a same inflow conditions, average solids concentrations were significantly lower on compost plots than on soil plots, as deposition occurred in compost rills. Deposited solids often formed micro-dams in the compost rills, which further promoted flow through the compost matrix and deposition of suspended particles. The formation of micro-dams in compost plots was an important mechanism in preventing soil erosion under concentrated flow conditions. Results of this study indicated that the erosion process on compost blankets may differ from classical shear-induced rill erosion on soil surfaces. Future work will investigate models that may be used to better understand and predict erosion of compost material under concentrated flow conditions.
机译:堆肥毯被认为是一种有效的侵蚀控制方法,已被广泛使用。尽管先前的研究已经证明堆肥毯在正常的降雨和表层流条件下可以比传统方法更好地控制侵蚀,但很少有人关注堆肥如何应对浓缩流条件。这项研究的目的是研究堆肥毯在集中流动条件下的侵蚀过程。在12.5%的坡度上使用四个浓缩流量研究了侵蚀控制堆肥(ECC),院子废物堆肥(YWC)和裸土(BS,壤土)。测量开始排放的时间,流速,固体浓度和固体总损失。在这些条件下,观察并记录了侵蚀过程和小溪的演化。结果表明,从堆肥区开始排放的时间比从土壤区开始排放的时间明显更长。大量流入物能够渗入堆肥基质并流过堆肥基质,与堆肥地块相比,堆肥地块上的地表流所占比例较小。在高流量下(2.7x10 -4 和3.3x10 -4 m 3 / s),堆肥区的固体损失显着小于那些来自土壤地块。在相同的流入条件下,堆肥区的平均固体浓度显着低于土壤区,这是因为堆肥小溪中发生了沉积。沉积的固体经常在堆肥小钻中形成微坝,这进一步促进了通过堆肥基质的流动和悬浮颗粒的沉积。堆肥区微水坝的形成是在集中流动条件下防止水土流失的重要机制。这项研究的结果表明,堆肥毯子上的侵蚀过程可能不同于经典的剪切诱导的小孔对土壤表面的侵蚀。未来的工作将研究可用于更好地理解和预测在集中流动条件下堆肥材料腐蚀的模型。

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