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Effectiveness of straw mulch on infiltration, splash erosion, runoff and sediment in laboratory conditions

机译:秸秆覆盖在实验室条件下对入渗,飞溅侵蚀,径流和沉积物的有效性

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摘要

Mulches have extraordinary potential in reducing surface runoff, increasing infiltration of water into the soil and decreasing soil erosion. The straw mulches as a biological material, has the ability to be a significant physical barrier against the impact of raindrops and reduce the detachment of soil aggregates. The present study is an attempt to determine the efficiency of straw mulch as conservation treatment in changes in the splash erosion, time-to-runoff, runoff coefficient, infiltration coefficient, time-to-drainage, drainage coefficient, sediment concentration and soil loss. The laboratory experiments have been conducted for sandy-loam soil taken from deforested area, about 15 km of Warsaw west, Poland under lab conditions with simulated rainfall intensities of 60 and 120 mm·h~(-1), in 4 soil moistures of 12, 25, 33 and 40% and the slope of 9%. Compared with bare treatments, results of straw mulch application showed the significant conservation effects on splash erosion, runoff coefficient, sediment concentration and soil loss and significant enhancement effects on infiltration and drainage. The results of Spearman-Rho correlation showed the significant (p=<0.05) correlation with r= -0.873, 0.873, 0.878 and 0.764 between rainfall intensity and drainage coefficient, downstream splash, sediment concentration and soil loss and with r=-0.976, 0.927 and -0.927 between initial soil moisture content and time-to-runoff, runoff coefficient and infiltration coefficient, respectively.
机译:覆盖物在减少地表径流,增加水向土壤的渗透和减少土壤侵蚀方面具有非凡的潜力。秸秆覆盖物是一种生物材料,具有成为抵抗雨滴影响并减少土壤团聚体分离的重要物理屏障的能力。本研究试图确定秸秆覆盖物作为养护处理的效率,以改变飞溅侵蚀,径流时间,径流系数,入渗系数,排水时间,排水系数,沉积物浓度和土壤流失。在实验室条件下对波兰华沙以西约15 km的森林砍伐地区的沙壤土进行了实验室实验,模拟降雨强度为60和120 mm·h〜(-1),在4种土壤湿度为12的条件下,25%,33%和40%,以及9%的斜率。与裸露处理相比,秸秆覆盖施用的结果显示出对飞溅侵蚀,径流系数,沉积物浓度和土壤流失具有显着的保护作用,并且对入渗和排水具有显着的增强作用。 Spearman-Rho相关性结果显示降雨强度与排水系数,下游飞溅,沉积物浓度和土壤流失之间的r = -0.873、0.873、0.878和0.764的显着(p = <0.05)相关,r = -0.976,土壤初始含水量与径流时间,径流系数和入渗系数之间分别为0.927和-0.927。

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