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首页> 外文期刊>The Science of the Total Environment >Humans reshape wetlands: Unveiling the last 100 years of morphological changes of the Mara Wetland, Tanzania
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Humans reshape wetlands: Unveiling the last 100 years of morphological changes of the Mara Wetland, Tanzania

机译:人类重塑湿地:揭开坦桑尼亚马拉湿地近100年的形态变化

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The Lower Mara River and Wetland. Tanzania, is an impoitant ecosystem and unique water resource for a vast semi-arid area The river, an affluent of Lake Victoria, and the wetland are experiencing morphological and vegetation changes resulting in channel avulsions and wetland expansion. This study analyses the changes over the last 100 years and investigates natural and anthropogenic behaviors to explain the increase of the Mara Wetland area. We collated historical topographic maps and satellite images. We conducted two field surveys in low and high flow condition with an unmanned aerial vehicle, a sonar and an ADCP. We mapped selected areas as well as the bed topography in some stretches of the river, measured discharges, and collected river bed and suspended sediment samples. The analysis of the sediments shows that the wetland system, dominated by papyrus sp. is very efficient in trapping sediment, releasing clear water to the Lake Victoria. The historical reconstruction using topographic maps, satellite images and a multivariable analysis including hydrology and land cover, shows that 4 major avulsions occurred in the last 70 years due to a combination of natural behaviors, hydrological fluctuations and anthropogenic factors such as basin deforestation, farming and grazing along the river banks and in the wetland. Each avulsion led to substantial expansion of the wetland. Combined, they increased the wetland area by a factor of 3.6. Describing the Lower Mara River dynamic behavior, this work provides relevant information for sustainable future water and sediment management in order to preserve wetland habitats and natural resources. (C) 2019 Elsevier B.V. All rights reserved.
机译:下马拉河和湿地。坦桑尼亚是广阔的半干旱地区的无力生态系统和独特的水资源河流,维多利亚湖的丰富地带和湿地正在经历形态和植被变化,导致河道撕裂和湿地扩展。这项研究分析了过去100年的变化,并调查了自然和人为行为来解释Mara湿地面积的增加。我们整理了历史地形图和卫星图像。我们使用无人飞行器,声纳和ADCP在低流量和高流量条件下进行了两次现场调查。我们绘制了部分区域以及河段的河床地形图,测量了流量,并收集了河床和悬浮沉积物样本。对沉积物的分析表明,以纸莎草为主的湿地系统。在捕集沉积物方面非常有效,可以向维多利亚湖释放清澈的水。使用地形图,卫星图像以及包括水文和土地覆盖在内的多变量分析进行的历史重建表明,由于自然行为,水文波动和人为因素(如流域森林砍伐,耕作和耕作)的综合作用,在过去70年中发生了4次重大崩塌。沿着河岸和湿地放牧。每次撕裂都导致湿地的大量扩张。结合起来,他们将湿地面积增加了3.6倍。描述了下马拉河的动态行为,这项工作为未来可持续的水和泥沙管理提供了相关信息,以保护湿地的栖息地和自然资源。 (C)2019 Elsevier B.V.保留所有权利。

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