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Reconstructing lateral migration rates in meandering systems – a novel Bayesian approach combining optically stimulated luminescence (OSL) dating and historical maps

机译:重建曲折系统中的横向迁移速率–一种新颖的贝叶斯方法,结合了光激发发光(OSL)测年和历史地图

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Identifying lateral migration rates of meandering rivers is relevant both for fluvial geomorphology and to support river management. Lateral migration rates for contemporary meandering systems are often reconstructed based on sequential remote-sensing images or historical maps; however, the time frame for which these sources are available is limited and hence likely to represent fluvial systems subjected to human influence. Here, we propose to use scroll bar sequences as an archive to look further back in time using optically stimulated luminescence (OSL) dating of sand-sized quartz grains. We develop a modelling procedure for the joint Bayesian analysis of (OSL) dating results and historical map data. The procedure is applied to two meanders from the Overijsselse Vecht, a medium-sized sand-bed river in the Netherlands. We obtained nine?samples for OSL dating from scroll bars and combined OSL dating results with historical map data for the period 1720–1901?CE (Common Era). The procedure we propose here incorporates the strengths of both data types for reconstructing fluvial morphodynamics over longer time frames. Using an iterative modelling approach, we translate spatial uncertainty of historical maps into temporal uncertainty of channel position required for Bayesian deposition modelling. Our results indicate that meander formation in the Overijsselse Vecht system started around 1400 CE, and lateral migration rates were on average 2.6 and 0.9?m?yr sup?1/sup for the two investigated bends, until river channelization around 1900?CE.
机译:确定蜿蜒河流的横向迁移率与河流地貌和支持河流管理都息息相关。通常基于连续的遥感图像或历史地图来重建当代蜿蜒系统的横向迁移率;但是,这些来源可用的时间范围有限,因此很可能代表受人类影响的河流系统。在这里,我们建议使用滚动条序列作为存档,以使用沙粒大小石英颗粒的光学激发发光(OSL)年代来回顾过去。我们为(OSL)约会结果和历史地图数据的联合贝叶斯分析开发了一种建模程序。该程序适用于来自荷兰中型沙床河流Overijsselse Vecht的两条河曲。我们从滚动条中获得了9个OSL约会样本,并将OSL约会结果与1720–1901?CE(共同时期)的历史地图数据相结合。我们在此提出的程序结合了两种数据类型的优势,可以在更长的时间范围内重构河流形态动力学。使用迭代建模方法,我们将历史地图的空间不确定性转换为贝叶斯沉积建模所需的通道位置的时间不确定性。我们的研究结果表明,Overijsselse Vecht系统中的曲折形成始于1400 CE左右,两个被测弯头的横向迁移率平均分别为2.6和0.9?m?yr ?1 ,直到1900年左右的河道渠化为止CE。

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