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Livestock redistribute runoff and sediments in semi-arid rangeland areas

机译:牲畜重新分配半干旱牧场地区的径流和沉积物

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Semi-arid areas where grazing is the main land use exhibit a"three-phase-mosaic" pattern of dominant surface patches: shrubs, tramplingroutes, and intershrub areas. This pattern differs from the "two-phasemosaic" seen in grazing-free semi-arid areas. The patches might create apositive feedback process in which enhanced infiltration beneath shrubsminimizes overland flow from under their canopies, thereby strengthening thesink–source mechanism by which overland flow generated between shrubsrapidly infiltrates into the soil beneath them, where it deposits soilparticles, litter, nutrients and organic matter, thereby enhancinginfiltration by changing the local microtopography, and improving soilproperties. To analyze sink–source relationships among the patches in grazedareas in rangelands of the semi-arid northern Negev region of Israel, weconstructed small runoff plots, 0.25–1.0 m2 in area, of five types:shrub (Sarcopoterium spinosum), intershrub, route, route–shrub combination, andintershrub–shrub combination. The shrubs always occupied the downslope partof the plot. Overland flow and sediment deposits were measured in all plotsduring 2007/8 and 2008/9. The combined plots yielded much less overland flowand sediments than intershrub, routes and shrub ones, indicating that theshrubs absorbed almost all the yields of the upper part of their plots. Theshrubs generated less runoff and sediments than routes and intershrubs;runoff flows from the routes and intershrubs were similar; sediment yieldwas highest in the intershrubs. Thus, runoff yield exhibited a two-phasemosaic pattern, and sediment yield, i.e., soil erosion, a three-phase mosaicpattern.
机译:以干旱为主要土地利用方式的半干旱地区表现出主要的表面斑块的“三相马赛克”模式:灌木丛,践踏路线和灌木丛间地区。这种模式不同于在无草场的半干旱地区看到的“两相马赛克”。这些斑块可能会产生积极的反馈过程,在这种过程中,灌木下面的渗透作用增强,从而最小化了其冠层下的陆上水流,从而加强了水源机制,从而使灌木丛之间产生的陆上水流迅速渗入其下方的土壤中,并在其中沉积土壤颗粒,凋落物,养分和有机质。物质,从而通过改变局部微观形貌增强了入渗,并改善了土壤特性。为了分析以色列半干旱北部内盖夫地区牧场的放牧区斑块之间的汇源关系,我们构建了面积为0.25–1.0 m 2 的五种小径流图:灌木( Sarcopoterium spinosum ),灌木间,路线,路线-灌木组合和灌木间-灌木组合。灌木丛总是占据地块的下坡部分。在2007年8月和2008年9月的所有土地上测量了陆上流量和沉积物沉积物。组合地块产生的陆上径流和沉积物比灌木间,道路和灌木地少,这表明灌木几乎吸收了其地上部的全部产量。灌木丛产生的径流和沉积物少于路线和灌木丛;径流和灌木丛的径流相似;灌丛间的泥沙产量最高。因此,径流产量表现为两相马赛克图案,而沉积物产量即为水土流失,表现为三相马赛克图案。

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