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Effects of a deep-rooted crop and soil amended with charcoal on spatial and temporal runoff patterns in a degrading tropical highland watershed

机译:根深蒂固的农作物和土壤用木炭改性对退化热带高地流域的时空径流格局的影响

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Placement and hence performance of many soil and water conservation structures in tropical highlands has proven to be challenging due to uncertainty of the actual location of runoff-generating areas in the landscape. This is the case especially in the (sub-) humid areas of the Ethiopian highlands, resulting in limited success of such conservation measures. To improve understanding of the effect of land use on spatial and temporal runoff patterns in the Ethiopian highlands, we monitored runoff volumes from 24 runoff plots constructed in the 113 ha Anjeni watershed, where historical data of rainfall and stream discharge were available. In addition, we assessed the effectiveness of charcoal amendment of the soil and crop rooting depth in reducing runoff, and we compared the effect of lupine (a deep-rooted crop) to that of barley. We also measured daily rainfall, surface runoff, and root zone moisture contents during the monsoon seasons of 2012 and 2013 (with all plots being tilled in 2012, but only barley plots tilled in 2013). In addition, we analyzed longterm surface runoff from four plots, and outlet discharge data from the research site (1989-1993) were analyzed and compared with our observations. Results showed that the degrees of soil degradation and soil disturbance (tillage) were significant factors affecting plot-scale runoff responses. As expected, runoff was greater from more degraded soils. Overall, under the commonly applied lupine cropping practice, runoff was higher than under the commonly applied barley cropping practice. In particular, considerable difference was observed during smaller rainfall events (approximately <20 mm) in 2013, when lupine plots (non-tilled) had greater runoff than barley plots (tilled). Charcoal tended to decrease runoff, but results were not significant.
机译:由于不确定地表径流产生区的实际位置,已证明热带高地上许多水土保持结构的位置及其性能具有挑战性。尤其是在埃塞俄比亚高地的(半)潮湿地区,情况就是如此,导致这种保护措施的成功有限。为了更好地了解埃塞俄比亚高地土地利用对空间和时间径流格局的影响,我们监测了113公顷安杰尼流域建造的24个径流小区的径流量,那里有降雨和溪流排放的历史数据。此外,我们评估了木炭改良土壤和作物生根深度对减少径流的有效性,并比较了羽扇豆(一种根深蒂固的作物)和大麦的效果。我们还测量了2012年和2013年的季风季节的每日降雨量,地表径流和根区水分含量(所有地块均在2012年耕种,但只有大麦地块在2013年耕种)。此外,我们分析了四个地块的长期地表径流,并分析了研究地点(1989-1993年)的出口流量数据,并将其与我们的观察结果进行了比较。结果表明,土壤退化程度和土壤扰动(耕作)是影响样地径流响应的重要因素。不出所料,退化程度更大的土壤径流更大。总体而言,在常用的羽扇豆种植实践下,径流高于常用的大麦种植实践。尤其是,2013年的降雨事件较小(大约<20 mm),而羽扇豆地(非平地)的径流比大麦地(平地)大,观测到的差异很大。木炭倾向于减少径流,但结果并不显着。

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