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Laboratory investigation of rill erosion on compost blankets under concentrated flow conditions.

机译:在集中流动条件下堆肥毯子上的小溪侵蚀的实验室研究。

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摘要

A flume study was conducted using a soil, yard waste compost, and an erosion control compost to investigate the response to concentrated flow and determine if the shear stress model could be used to describe the response. Yard waste compost (YWC) and the bare Cecil soil (CS) control responded to concentrated laboratory runoff similarly in rill formation, and the shear stress model was useful in estimating sediment yields from both of these land covers. Results indicated that critical shear stress values for yard waste compost and Cecil soil were not significantly different. However, the erodibility of the soil was higher, resulting in increased solids loss, on the Cecil soil. Micro-dams, the main mechanism for limiting soil erosion for the compost, often occurred in the rills of the erosion control compost (ECC), causing the concentrated flow to infiltrate and fan out through the compost. Since flow could not be maintained in the rill, parameters for the stress model could not be determined for the erosion control compost.
机译:使用土壤,院子垃圾堆肥和侵蚀控制堆肥进行了水槽研究,以调查对集中流的响应并确定是否可以使用剪切应力模型来描述响应。堆场废料堆肥(YWC)和塞西尔裸露土壤(CS)的对照在小溪形成过程中对集中的实验室径流的响应相似,并且剪应力模型可用于估算这两个土地覆盖层的沉积物产量。结果表明,堆肥和塞西尔土壤的临界剪切应力值没有显着差异。但是,土壤的可蚀性较高,导致塞西尔土壤上的固体损失增加。微型水坝是限制堆肥土壤侵蚀的主要机制,通常发生在侵蚀控制堆肥(ECC)的小溪中,导致浓缩液渗透并通过堆肥散开。由于无法保持小溪中的流量,因此无法确定侵蚀控制堆肥的应力模型参数。

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