简易降雨模拟器在未铺路面土壤可蚀性研究中的校准

Esdras Ngezahayo, M. Burrow, G. Ghataora
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引用次数: 4

摘要

降雨模拟器用于侵蚀研究已有50多年的历史。这些被广泛应用于农业土壤,以评估土壤的渗透能力和孔隙度,从而了解植物根系渗透这些土壤的潜力。近年来,降雨模拟器已成为研究雨滴动能和随后的流动剪切应力对土壤分离的重要工具。这导致对基础设施故障的理解取得了显着进展,例如由于表面土壤流失和侵蚀特征的形成而未铺设的道路,由于填充物的移除而埋下的管道和设施,以及桥梁冲刷和堤防故障等等。为了进行彻底而严谨的研究,降雨模拟器必须产生与自然降雨相同大小的雨滴。校准降雨模拟器以满足雨滴大小在1毫米至6毫米范围内的这一关键需求,这是多年来的挑战,因此导致不同研究结果不一致。本文研制了一种经济型降雨模拟器,可用于评价非铺装道路土壤的可蚀性。用面粉法测定了雨滴的大小。在30 mm/hr、51 mm/hr和68 mm/hr降雨强度为2.0 m时,平均雨滴大小分别为3.0 mm、3.2 mm和3.5 mm。在相同的降雨强度顺序下,雨滴撞击被测表面的动能分别为193.5µJ、244µJ和301µJ,这足以在d50约0.4 ~ 1.5 mm压实至最大干密度的土壤中引发分离。
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Calibration of the Simple Rainfall Simulator for Investigating Soil Erodibility in Unpaved Roads
- Rainfall simulators have been used for erosion research for more than 50 years now. These are widely used in agricultural soils to assess the infiltration capacity and porosity of soils, and hence learn lessons on the potential of plant roots to penetrate those soils. Recently, rainfall simulators have been very useful to investigate soils detachment by both the raindrops kinetic energy and the subsequent flow shear stress. This has led to notable advances in the understanding of the failure of infrastructures such as unpaved roads due to surface soil loss and formation of erosion features, buried pipes and facilities due to removal of fill materials, as well as bridge scour and embankments failures to mention a few. To help conduct a thorough and rigorous research, rainfall simulators must produce raindrops of the same size as those produced by the natural rainfall. Calibrating rainfall simulators satisfying this key demand of raindrops sizes in the range of 1 mm to 6 mm posed challenges for years, and therefore led to inconsistencies in results from different studies. In this paper, an economical rainfall simulator which can be used for assessing erodibility of soils in unpaved roads was developed. The flour method technique was used to determine the sizes of the raindrops. The mean raindrops sizes were found to be 3.0 mm, 3.2 mm, and 3.5 mm, respectively for the rainfall intensities of 30 mm/hr, 51 mm/hr and 68 mm/hr falling through 2.0 m. In the same order of rainfall intensities, raindrops hit the surface of the tested surfaces by 193.5 µJ, 244 µJ and 301 µJ kinetic energies, which were sufficient to initiate detachment in soils of D 50 ranging from about 0.4 mm to 1.5 mm compacted to maximum dry density.
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