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Effects of rainfall intensity on splash erosion and its spatial distribution under maize canopy

机译:降雨强度对玉米冠层飞溅侵蚀及其空间分布的影响

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摘要

Splash erosion of soil particles by raindrops impacting a soil surface is the initiating mechanism of water erosion. To evaluate the effects of splash erosion on maize, spatial distribution of rainfall intensity and splash erosion rate were measured under maize cover in different growth stages. The relation between splash erosion rate under the maize canopy and rainfall intensity was analyzed. The results indicated that, the average rainfall intensity under the maize canopy gradually increased with the increase in rainfall intensity during the whole growth stage, and splash erosion rate under the maize canopy showed the same change. The average rainfall intensity and splash erosion rate under rainfall of 2.0 mm min(-1) were significantly higher than those of the rainfall of 1.0 mm min(-1). Under the same rainfall intensity, the minimum of splash erosion rate appeared in the jointing stage, while the maximum appeared in the tasseling stage. Compared with the seedling stage, the average splash erosion rates of the jointing stage showed the reduction of 23.9, 24.2, and 41.1 % the corresponding rainfall of 1.0, 1.5 and 2.0 mm min(-1), respectively, under the maize canopy. Under rainfall of 1.0 and 1.5 mm min(-1), there was a significant negative correlation between rainfall intensity under the canopy and splash erosion rate of every spot at the maize tasseling stage. Under rainfall of 2.0 mm min(-1), there was also a significant negative correlation between rainfall intensity and splash erosion rate under the canopy of every spot at maize seedling stage and mature stage. The distribution of splash erosion rate was concentrated at maize seedling stage and mature stage. However, the dispersion degree of splash erosion rate was obvious at jointing stage and tasseling stage of maize. Splash erosion rates showed great difference under the canopy at every period of maize growth. Under rainfall of 1.0 mm min(-1), the high splash erosion rate appeared at two spots, while under rainfall of 1.5 and 2.0 mm min(-1), splash erosion rate was only concentrated in a spot. This study would provide theoretical guidance for soil erosion control based on crop growth and coverage.
机译:雨滴撞击土壤表面对土壤颗粒的飞溅侵蚀是水蚀的起始机制。为了评价水土流失对玉米的影响,在不同生育期的玉米覆盖下测量了降雨强度和水土流失速率的空间分布。分析了玉米冠层下飞溅侵蚀速率与降雨强度之间的关系。结果表明,在整个生育期内,玉米冠层下的平均降雨强度随降雨强度的增加而逐渐增加,玉米冠层下的飞溅侵蚀率也发生了相同的变化。 2.0 mm min(-1)下的平均降雨强度和飞溅侵蚀速率显着高于1.0 mm min(-1)下的降雨。在相同降雨强度下,飞溅侵蚀率的最小值出现在拔节阶段,最大值出现在抽穗阶段。与苗期相比,拔节期的平均喷溅侵蚀率分别比玉米冠层下的1.0、1.5和2.0mm min(-1)减少了23.9%,24.2%和41.1%。在1.0和1.5 mm min(-1)的降雨下,玉米抽穗期冠层下的降雨强度与每个斑点的飞溅侵蚀率之间存在显着的负相关。在2.0 mm min(-1)的降雨条件下,玉米苗期和成熟期各点冠层下的降雨强度与飞溅侵蚀率之间也存在显着的负相关。飞溅侵蚀速率的分布主要集中在玉米苗期和成熟期。然而,在玉米拔节期和抽穗期,喷溅侵蚀速率的分散程度明显。在玉米生长的每个时期,冠层下的飞溅侵蚀速率显示出很大的差异。在1.0 mm min(-1)的降雨下,两个地方出现了较高的飞溅侵蚀率,而在1.5和2.0 mm min(-1)的降雨下,飞溅侵蚀率仅集中在一个斑点上。该研究将为基于作物生长和覆盖的土壤侵蚀控制提供理论指导。

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