跨过渡带土壤性质的空间变化:简要综述

Pub Date : 2018-05-30 DOI:10.2478/bgeo-2018-0006
Theodore Danso Marfo, Klement Resjek, V. Vranová
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引用次数: 4

摘要

交错带被认为是一种独特的环境。边缘效应和过渡带物种(动植物)的概念被广泛使用。考虑到在过渡带中发现的大多数物种通常处于生理决定的分布极限,它们对全球气候变化的反应就变得至关重要。交错带被认为比其附近的地区具有更多的生物多样性,因此具有很高的保护价值,但对不同交错带土壤性质的变化知之甚少。在本文中,我们首先强调了过渡带在评估全球气候变化影响中的作用,以及它们在物质(水和养分)进出区域运动中的中介作用。其次,我们回顾了土壤性质在不同过渡带之间的变化,值得注意的是,土壤性质在不同的过渡带之间趋于不同(例如,森林-林地过渡带的pH值增加,P和N减少,古今森林过渡带的pH值减少),这种方式定义了现有过渡带的特征。
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Spatial variations in soil properties across ecotones: a short review
Abstract Ecotones are considered as unique environments. The concepts of edge effect and ecotone species (flora and fauna) are widely used. Considering the fact that the majority of the species found in ecotones are usually at their physiologically determined limits of distribution, how they react to global climate changes becomes crucial. Ecotones are reputed to be more biologically diverse than areas close to them, and therefore possesses a high conservation value, yet little is known on how soil properties vary across ecotones. In this paper, we firstly highlighted the roles ecotones play in assessing the effect on global climate change, the mediatory role they play in the movement of material (water and nutrients) into and out of the region. Secondly, we reviewed studies on how soil properties change across ecotones and it is worthwhile to note that soil properties tend to differ across various ecotones (e.g. increasing pH and decreasing P & N across forest–glade ecotones, decreasing pH across ancient–recent forest ecotones) in a manner that defines the character of the ecotones existing.
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