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Ecological site-based assessments of wind and water erosion: informing accelerated soil erosion management in rangelands

机译:基于生态现场的风蚀和水蚀评估:为牧场加速土壤侵蚀管理提供信息

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Accelerated soil erosion occurs when anthropogenic processes modify soil, vegetation, or climatic conditions causing erosion rates at a location to exceed their natural variability. Identifying where and when accelerated erosion occurs is a critical first step toward its effective management. Here we explored how erosion assessments structured in the context of ecological sites (a land classification based on soils, landscape setting, and ecological potential) and their vegetation states (plant assemblages that may change due to management) can inform systems for reducing accelerated soil erosion in rangelands. We evaluated aeolian horizontal sediment flux and fluvial sediment erosion rates for five ecological sites in southern New Mexico, USA, using monitoring data and rangeland-specific wind and water erosion models. Across the ecological sites, plots in shrub-encroached and shrub-dominated vegetation states were consistently susceptible to aeolian sediment flux and fluvial sediment erosion. Both processes were found to be highly variable for grassland and grass-succulent states across the ecological sites at the plot scale (0.25 ha). We identified vegetation thresholds that define cover levels below which rapid (exponential) increases in aeolian sediment flux and fluvial sediment erosion occur across the ecological sites and vegetation states. Aeolian sediment flux and fluvial erosion in the study area could be effectively controlled when bare ground cover was <20% of a site or the cover of canopy interspaces >100 cm in length was less than similar to 35%. Land use and management activities that alter cover levels such that they cross thresholds, and/or drive vegetation state changes, may increase the susceptibility of areas to erosion. Land use impacts that are constrained within the range of natural variability should not result in accelerated soil erosion. Evaluating land condition against the erosion thresholds identified here will enable identification of areas susceptible to accelerated soil erosion and the development of practical management solutions.
机译:当人为过程改变土壤,植被或气候条件,导致某个地点的侵蚀率超过其自然变异性时,就会加速土壤侵蚀。确定加速侵蚀发生的时间和地点是实现有效管理的关键的第一步。在这里,我们探讨了在生态场所(基于土壤,景观环境和生态潜力的土地分类)及其植被状态(可能因管理而改变的植物组合)的背景下进行的侵蚀评估如何为减少加速土壤侵蚀的系统提供信息在牧场上。我们使用监测数据和牧场特定的风与水侵蚀模型,评估了美国新墨西哥州南部五个生态区的风沙水平泥沙通量和河流泥沙侵蚀速率。在整个生态区中,处于灌木丛生和灌木为主的植被状态的地块始终易受风沙沉积物通量和河流沉积物侵蚀的影响。研究发现,在样地范围(0.25公顷)上,整个生态区的草地和草质多肉状态这两个过程都高度可变。我们确定了定义覆盖水平的植被阈值,在该阈值以下,生态位点和植被状态之间的风沙沉积通量迅速(指数)增加,河流沉积物侵蚀发生。当裸露的地面覆盖率小于站点的20%或天棚间隙的长度大于100 cm时小于35%时,可以有效控制研究区域的风沙沉积物通量和河流侵蚀。土地使用和管理活动会改变覆盖水平,使其超过阈值和/或驱动植被状态变化,这可能会增加区域遭受侵蚀的敏感性。限制在自然变异范围内的土地利用影响不应导致加速的土壤侵蚀。根据此处确定的侵蚀阈值评估土地条件,将有助于确定容易遭受土壤侵蚀的地区,并制定切实可行的管理解决方案。

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