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首页> 外文期刊>Journal of Environmental Management >Impacts of grazing on ground cover, soil physical properties and soil loss via surface erosion: A novel geospatial modelling approach
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Impacts of grazing on ground cover, soil physical properties and soil loss via surface erosion: A novel geospatial modelling approach

机译:地表侵蚀地面覆盖,土壤物理性质和土壤损失的影响:一种新型地理空间建模方法

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Agricultural expansion and overgrazing are globally recognized as key contributors to accelerated soil degradation and surface erosion, with direct consequences for land productivity, and environmental health. Measured impacts of livestock grazing on soil physical properties and ground cover are absent in soil loss models (e.g., Revised Universal Soil Loss Equation, RUSLE) despite significant impacts to surface erosion. We developed a novel model that captures changes to ground cover and soil properties (permeability and structure) as a function of grazing intensity (density, duration, history, and stock type), as well as soil clay and water contents. The model outputs were integrated within RUSLE to calculate a treaded soil erodibility (K_(tr)) and grazed cover factors (C_(gr)) at seasonal timescales (3-month windows) to account for variability in soil moisture content, grazing practices, vegetation growth and senescence, and rainfall. Grazed pastures and winter-forage paddocks exhibit distinct changes in soil erodibility and soil losses, which are most pronounced for wet soils when plant cover is reduced/ minimal. On average, typical pasture grazing pressures increase soil erodibility by 6% (range = 1-90%), compared to 60% (18-310%) for intensive winter forage paddocks. Further, negligible ground cover following forage crop grazing increases surface erosion by a factor of 10 (±_1~3) relative to grazed pastures, which exhibit soil losses (μ = 83 t km~(-2) yr~(-1); range = 11.6 to 246) comparable to natural uncropped catchments (100-200 t km~(-2) yr~(-1)). Exacerbated soil losses from winter forage-crop paddocks (μ = 1,100 t km~(-2) yr~(-1)) arose from significant degradation of soil physical properties and exposing soils directly to rainfall and runoff. We conclude that proactive decisions to reduce treading damage and avoid high-density grazing will far exceed reactive practices seeking to trap sediments lost from grazed lands.
机译:农业扩张和过度普查全球被认为是加速土壤退化和表面侵蚀的关键贡献者,具有直接影响土地生产力和环境健康。在土壤损失模型中没有测量牲畜放牧在土壤物理性质和地面覆盖的影响,尽管对表面侵蚀有重大影响,但在土壤损失模型中不存在于土壤物理性质和地面覆盖物中的影响。我们开发了一种新颖的模型,捕获地面覆盖和土壤性质(渗透率和结构)的变化,作为放牧强度(密度,持续时间,历史和股票类型)以及土壤粘土和水含量的函数。模型输出集成在风格内,以计算季节性时间尺度(3个月窗口)的踩踏土壤蚀(K_(TR))和放牧覆盖因子(C_(GR)),以考虑土壤水分含量的可变性,放牧实践,植被生长和衰老,降雨量。放牧的牧场和冬季饲养围场在植物覆盖减少/最小时,对土壤蚀和土壤损失的不同变化具有最明显的湿土壤。平均而言,典型的牧场放牧压力将土壤易用程度提高6%(范围= 1-90%),而密集的冬季饲料围场的60%(18-310%)。此外,在饲料作物放牧后可忽略不计的地面覆盖,相对于放牧牧场,将表面侵蚀增加了10(±1〜3),其表现出土壤损失(μ= 83 k〜(-2)Yr〜(-1);范围= 11.6至246)与天然未折叠的集水区相当(100-200 k〜(-2)Yr〜(-1))。从冬季牧草围草(μ= 1,100 k〜(-2)Yr〜(-1))中加剧了土壤损失从土壤物理性质的显着降解,直接降雨和径流暴露。我们得出结论,积极决定减少踩踏损坏,避免高密度放牧将远远超过寻求从放牧地丢失的沉积物陷入沉积物的反应实践。

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