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Lake-islands: A distinct morphology of river systems

机译:湖岛:河流系统的明显形态

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Islands are important morphologies in multichannel fluvial systems for maintaining secondary channels, increasing flow efficiency in the widest stretches, and hosting important ecological environments. This study presents a hitherto unclassified, distinct type of fluvial island that occurs in large rivers: the lake-island. We analyzed islands from large rivers, particularly from South American rivers, the Negro (Amazon Basin) and Paran ' a (La Plata Basin) Rivers. Satellite images were used for identification and morphometric analysis, while morphometric indices were used to compare island morphologies. Sedimentary facies analysis and dating were also conducted to characterize the island deposits. Lake-islands are differentiated from typical fluvial islands by their lenticular morphology, and frontal and lateral levees that protect and isolate the lake or allow it to be partially connected to the channel. Lake-island morphology can be elongated or circular, based on their morphometric indices and their relationship with channel width. Lake-island lengths varied from hundreds of meters to tens of kilometers. They are formed by in-channel deposition on preexisting sand bars or fluvial islands. Their sedimentary characteristics are relatively simple and comprise basal sandy facies capped by finer-grained deposits. The permanence of lake-islands depends on the flow regime and sedimentary load of the fluvial system. The lake-island's age ranges from 101 to 103 years. A comprehensive understanding of the formation processes and dynamics of lake-islands is of fundamental importance in the management of large fluvial systems, and studies of fluvial ecology.
机译:群岛是多通道河流系统中的重要形态,用于维持二次通道,增加最宽伸展的流量效率,以及托管重要的生态环境。本研究提出了一个迄今为止未分类的,不同类型的河岛,在大河里出现:湖岛。我们分析了大型河流的岛屿,特别是南美洲河流,黑人(亚马逊盆地)和Paran'A(La Plata Basin)河流。卫星图像用于鉴定和形态学分析,而形态学指数用于比较岛状形态。还进行了沉积相分析和约会,以表征岛沉积物。 Lake-Islands通过它们的透镜形态与典型的萤石群岛区分开来,以及保护和隔离湖泊的前部和侧向纹理,或者使其部分连接到通道。湖岛形态学可以基于它们的形态学指数及其与频道宽度的关系来伸长或圆形。湖岛长度从数百米到几十公里不同。它们是通过在预先存在的砂杆或氟岛上的通道沉积形成。它们的沉积特性相对简单,包括由细粒沉积物覆盖的基底砂白相。湖岛的持久性取决于河流系统的流动制度和沉积载荷。湖岛的年龄从101到103年。全面了解湖岛的形成过程和动态在大型河流系统管理方面具有根本重要性,以及河流生态学的研究。

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