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Eco-geomorphology of banded vegetation patterns in arid and semi-arid regions

机译:干旱和半干旱地区带状植被格局的生态地貌

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摘要

The interaction between vegetation and hydrologic processes is particularlytight in water-limited environments where a positive-feedback links soilmoisture and vegetation. The vegetation of these systems is commonlypatterned, that is, arranged in a two phase mosaic composed of patches withhigh biomass cover interspersed within a low-cover or bare soil component.These patterns are strongly linked to the redistribution of runoff andresources from source areas (bare patches) to sink areas (vegetationpatches) and play an important role in controlling erosion.In this paper, the dynamics of these systems is investigated using a newmodeling framework that couples landform and vegetation evolution,explicitly accounting for the dynamics of runon-runoff areas. The objectiveof this study is to analyze water-limited systems on hillslopes with mildslopes, in which overland flow occurs predominantly in only one directionand vegetation displays a banded pattern. Our simulations reproduce bandsthat can be either stationary or upstream migrating depending on themagnitude of the runoff-induced seed dispersal. We also found thatstationary banded systems redistribute sediment so that a steppedmicrotopography is developed. The modelling results are the first toincorporate the effects of runoff redistribution and variable infiltrationrates on the development of both the vegetation patterns andmicrotopography. The microtopography for stationary bands is characterizedby bare soil on the lower gradient areas and vegetation on steeper gradientsareas. For the case of migrating vegetation bands the model generateshillslope profiles with planar topography. The success at generating notonly the observed patterns of vegetation, but also patterns of runoff andsediment redistribution suggests that the hydrologic and erosion mechanismsrepresented in the model are correctly capturing some of the key processesdriving these ecosystems.
机译:在水分有限的环境中,植被与水文过程之间的相互作用尤其紧密,在这种环境中,正反馈关系到土壤水分与植被之间的联系。这些系统的植被通常是有格局的,即由高生物量覆盖的斑块散布在低覆盖或裸露的土壤成分中组成的两阶段镶嵌,这些格局与源区的径流和资源的重新分配密切相关(裸露)。斑块)到下沉区域(植被斑块)并在控制侵蚀中起重要作用。 本文使用耦合地形和植被演化的新模型框架研究了这些系统的动力学,明确说明了动力学径流径流区域。这项研究的目的是分析具有缓坡的山坡上的水限制系统,在这些系统中,陆上流主要发生在一个方向上,而植被显示出带状格局。我们的模拟再现了根据径流诱导的种子扩散幅度而可以平稳或上游迁移的条带。我们还发现平稳的带状系统重新分布了沉积物,因此逐步形成了微形貌。模拟结果是第一个结合径流重新分配和变量入渗率对植被格局和微形貌发展的影响的模型。静止带的微形貌特征是较低坡度区的裸土和较陡坡度区的植被。对于迁移植被带的情况,模型会生成具有平面地形的坡度剖面。不仅成功地产生了观测到的植被格局,而且还成功地产生了径流和沉积物再分配的格局,这表明该模型所代表的水文和侵蚀机制正正确地捕捉了驱动这些生态系统的一些关键过程。

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