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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Combined hillslope diffusion and sediment transport simulation applied to landscape dynamics modelling
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Combined hillslope diffusion and sediment transport simulation applied to landscape dynamics modelling

机译:结合坡面扩散与泥沙运移模拟在景观动力学建模中的应用

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We present a new numerical approach for simulating geomorphic and stratigraphic processes that combines open-channel flow with non-uniform sediment transport law and semi-empirical diffusive mass wasting. It is designed to facilitate modelling of surface processes across multiple space- and time-scales, and under a variety of environmental and tectonic conditions. The physics of open-channel flow is primarily based on an adapted Lagrangian formulation of shallow-water equations. The interaction between flow and surface geology is performed by a non-uniform total-load sediment transport law. Additional hillslope processes are simulated using a semi-empirical method based on a diffusion approach. In the implementation, the resolution of flow dynamics is made on a triangulated grid automatically mapped and adaptively remeshed over a regular orthogonal stratigraphic mesh. These new methods reduce computational time while preserving stability and accuracy of the physical solutions. In order to illustrate the potential of this method for landscape and sedimentary system modelling, we present a set of three generic experiments focusing on assessing the influence of contrasting erodibilities on the evolution of an active bedrock landscape. The modelled ridges morphometrics satisfy established relationships for drainage network geometry and slope distribution, and provide quantitative information on the relative impact of hillslope and channel processes, sediment discharge and alluviation. Our results suggest that contrasting erodibility can stimulate autogenic changes in erosion rate and influence the landscape morphology and preservation. This approach offers new opportunities to investigate joint landscape and sedimentary systems response to external perturbations. The possibility to define and track a large number of materials makes the implementation highly suited to model source-to-sink problems where material dispersion is the key question that needs to be addressed, such as natural resources exploration and basin analysis. Copyright (c) 2014 John Wiley & Sons, Ltd.
机译:我们提出了一种模拟地貌和地层过程的新数值方法,该方法将明渠水流与不均匀的泥沙运移规律和半经验扩散质量浪费结合起来。它旨在促进在多种环境和构造条件下跨多个时空尺度对地表过程进行建模。明渠水流的物理学主要基于浅水方程的拉格朗日公式。流量和地表地质之间的相互作用是通过不均匀的总负荷沉积物输送定律进行的。使用基于扩散方法的半经验方法来模拟其他坡度过程。在实施中,在自动映射并在常规正交地层网格上进行自适应修正的三角网格上,对流动动力学进行了解析。这些新方法减少了计算时间,同时保留了物理解决方案的稳定性和准确性。为了说明此方法在景观和沉积系统建模中的潜力,我们提出了一组三个通用实验,重点是评估对比可蚀性对活动基岩景观演变的影响。建模的山脊形态学满足排水网络几何形状和坡度分布的既定关系,并提供有关坡度和河道过程,沉积物排放和冲积作用的相对影响的定量信息。我们的研究结果表明,可蚀性的对比可刺激侵蚀速率的自发变化并影响景观形态和保存。这种方法为调查联合景观和沉积系统对外部扰动的响应提供了新的机会。定义和跟踪大量材料的可能性使该实现方式非常适合于建模从源到汇的问题,在这些问题中,材料分散是需要解决的关键问题,例如自然资源勘探和盆地分析。版权所有(c)2014 John Wiley&Sons,Ltd.

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