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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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The interaction between vegetation and hydrologic processes is particularly tight in water-limited environments where a positive-feedback links soil moisture and vegetation. The vegetation of these systems is commonly patterned, that is, arranged in a two phase mosaic composed of patches with high biomass cover interspersed within a low-cover or bare soil component. These patterns are strongly linked to the redistribution of runoff and resources from source areas (bare patches) to sink areas (vegetation patches) and play an important role in controlling erosion. In this paper, the dynamics of these systems is investigated using a new modeling framework that couples landform and vegetation evolution, explicitly accounting for the dynamics of runon-runoff areas. The objective of this study is to analyze water-limited systems on hillslopes with mild slopes, in which overland flow occurs predominantly in only one direction and vegetation displays a banded pattern. Our simulations reproduce bands that can be either stationary or upstream migrating depending on the magnitude of the runoff-induced seed dispersal. We also found that stationary banded systems redistribute sediment so that a stepped microtopography is developed. The modelling results are the first to incorporate the effects of runoff redistribution and variable infiltration rates on the development of both the vegetation patterns and microtopography. The microtopography for stationary bands is characterized by bare soil on the lower gradient areas and vegetation on steeper gradients areas. For the case of migrating vegetation bands the model generates hillslope profiles with planar topography. The success at generating not only the observed patterns of vegetation, but also patterns of runoff and sediment redistribution suggests that the hydrologic and erosion mechanisms represented in the model are correctly capturing some of the key processes driving 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为紧密,因为正向反馈将土壤水分与植被联系在一起。这些系统的植被通常是有图案的,即以两相镶嵌的形式排列,该镶嵌由散布在低覆盖或裸露土壤成分中的具有高生物量覆盖的斑块组成。这些模式与径流和资源从源区(裸露斑块)到汇聚区(植被斑块)的重新分配密切相关,并且在控制侵蚀方面起着重要作用。在本文中,使用新的建模框架对这些系统的动力学进行了研究,该模型将地形和植被演化耦合在一起,明确考虑了径流径流区域的动力学。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,而植被显示出带状分布。我们的模拟重现了条带,这些条带可以是固定的,也可以是上游迁移的,具体取决于径流引起的种子扩散的程度。我们还发现固定的带状系统会重新分配沉积物,因此逐步形成了微形貌。建模结果是第一个结合径流重新分配和可变渗透率对植被格局和微形貌发展的影响的模型。固定带的微观形貌的特征是较低坡度区的裸露土壤和较陡坡度的植被。对于迁移植被带的情况,模型会生成具有平面地形的山坡轮廓。成功地产生了不仅观察到的植被格局,而且还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在正确地捕捉驱动这些生态系统的一些关键过程。

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