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Using fluid dynamic concepts to estimate species movement rates in terrestrial landscapes

机译:使用流体动力学概念估算陆地景观中物种的移动速度

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摘要

Habitat loss and fragmentation threatens biodiversity and ecosystem function. ‘Permeability’ and ‘connectivity’ indices are used to estimate how individuals, populations or genes move spatially through a landscape. Yet, despite the analogies between landscape permeability and the physical definition of permeability (the ability for a porous media to transport a fluid), there have been few attempts to apply the physical concepts of permeability and fluid flow to problems in landscape movement ecology beyond some simple examples in the early literature. Here, we present a conceptual model linking physical principles to ecological terms and illustrate how concepts from Darcy’s Law of fluid flow through porous media could be used to quantify species movement rates through a heterogeneous terrestrial landscape. Although further refinement is needed to take this concept to two dimensions and into a full predictive model, the approach presented shows promise for quantifying the relative impacts of landscape change (e.g. habitat fragmentation or creation) on species movement rates.
机译:生境的丧失和破碎化威胁着生物多样性和生态系统的功能。 “通透性”和“连通性”指数用于估算个人,种群或基因在景观中的空间移动方式。然而,尽管在景观渗透率和渗透率的物理定义(多孔介质输送流体的能力)之间进行了类比,但很少有人尝试将渗透率和流体流动的物理概念应用于景观运动生态学中的问题。早期文献中的简单例子。在这里,我们介绍了一个将物理原理与生态学术语联系起来的概念模型,并说明了达西定律中通过多孔介质的流体流动的概念如何用于量化物种在异质陆地景观中的运动速率。尽管需要进一步完善以将这一概念扩展到两个维度并成为一个完整的预测模型,但本文提出的方法显示出量化景观变化(例如生境破碎或创造)对物种移动速率的相对影响的希望。

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