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首页> 外文期刊>The Science of the Total Environment >Biogeomorphological processes in an arid transgressive dunefield as indicators of human impact by urbanization
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Biogeomorphological processes in an arid transgressive dunefield as indicators of human impact by urbanization

机译:干旱海侵沙丘地带的生物地貌过程作为城市化对人类影响的指标

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Urban and tourist developments can have long-lasting impacts on coastal environments and fundamentally alter the evolution of coastal dune systems. This is the case of the Maspalomas dunefield (Gran Canaria, Canary Islands), hosting one of the largest tourist resorts in Spain. The resort was built on top of a sedimentary terrace at 25 m above sea level (El Ingles) in the 1960s, and has subsequently affected local winds and therefore aeolian sediment transport patterns. Buildings on the terrace deflect the winds to the south of the dunefield, where the rate of sediment transport accelerated. A shadow zone appeared to the lee side of the resort with a consequent decrease in wind speed and aeolian sediment transport and an increase in vegetation cover. In this paper, first we characterize the environmental changes around El Ingles terrace in recent decades, and describe the changes in the shadow zone through an analysis of the evolution of sedimentary volumes and vegetation characteristics (density, spatial patterns, and plants communities). A series of historical aerial photographs, recent orthophotos and digital elevation models obtained by digital photogrammetry and LiDAR, as well as fieldwork were used to characterize plant communities and spatial-temporal changes in erosive landforms. Results show changes in the pattern and migration rates of dunes located at the southern edge of the urbanization, as well as the formation of blowouts and large deflation areas, where the vegetation increases in density and number of plant communities. We discuss eco-anthropogenic factors that have produced these environmental changes. (C) 2018 Elsevier B.V. All rights reserved.
机译:城市和旅游业的发展会对沿海环境产生长期影响,并从根本上改变沿海沙丘系统的发展。 Maspalomas dunefield(加那利群岛大加那利岛)就是这种情况,这里是西班牙最大的旅游胜地之一。该度假村建于1960年代海拔25 m(El Ingles)的沉积阶地之上,随后影响了局部风,因此影响了风沙沉积物的运输方式。露台上的建筑物将风偏转到沙丘南部,在那里泥沙传输速度加快。度假村的背风侧出现了一个阴影区,其结果是风速和风沙输送减少,植被覆盖率增加。在本文中,首先,我们描述了近几十年来El Ingles阶地周围的环境变化,并通过分析沉积体积和植被特征(密度,空间格局和植物群落)的演变来描述阴影区的变化。通过数字摄影测量和LiDAR获得的一系列历史航拍照片,最近的正射照片和数字高程模型以及野外工作被用来刻画侵蚀性地貌中的植物群落和时空变化。结果表明,位于城市化南部边缘的沙丘的格局和迁移率发生了变化,并形成了井喷和大的放气区,植被在其中的密度和植物群落数量增加。我们讨论了导致这些环境变化的生态人为因素。 (C)2018 Elsevier B.V.保留所有权利。

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