Topography-based and vectorized algorithm for extracting physical quantities in 3D-SPH form and its application in debris-flow entrainment modeling

IF 6.9 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Engineering Geology Pub Date : 2024-08-22 DOI:10.1016/j.enggeo.2024.107693
Bin Su , Yange Li , Zheng Han , Yangfan Ma , Weidong Wang , Bo Ruan , Wei Guo , Wendu Xie , Shaofeng Tan
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Abstract

Extraction of physical quantities such as flow depth and velocities, is one of the major purposes of geophysical flow numerical modeling and critical for estimating consequent impact forces and sediment entrainment. It is simple in nature for mesh-based models but presenting challenges in three-dimensional smoothed particle hydrodynamics (SPH) schemes. The difficulties lie in the substantial number of particles and their uneven spatial-temporal distribution, particularly over complex topography. Inspired by our previous surface cell (SC) -based approach, we propose a novel topography-based and vectorized algorithm that significantly enhances the ability to extract physical quantities over complex topography. In the proposed algorithm, geomorphologic characteristics are mathematically represented by topographical normal vectors. The correlations of physical quantities with distinct coordinate descriptions are established through the vectorization concept, ultimately leading to effective extraction of physical quantities in SPH form over complex topography. This algorithm provides an important tool to incorporate topography-linked physical models within discretized frameworks. To validate its effectiveness, we employed the algorithm to integrate the debris-flow entrainment law with our previous HBP-SPH model, utilizing the 2010 Yohutagawa debris-flow event in Japan as a case study. The results demonstrate a good agreement between the numerical simulation and on-site observation. Discussion regarding the applicability and limitation of the algorithm concludes the paper.

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基于地形和矢量的 3D-SPH 物理量提取算法及其在泥石流夹带模型中的应用
提取水流深度和流速等物理量是地球物理水流数值模拟的主要目的之一,也是估算冲击力和沉积物夹带的关键。对于基于网格的模型来说,这种方法非常简单,但对于三维平滑粒子流体力学(SPH)方案来说,则是一种挑战。困难在于大量颗粒及其不均匀的时空分布,尤其是在复杂地形上。受之前基于表面单元(SC)方法的启发,我们提出了一种新颖的基于地形的矢量化算法,大大提高了在复杂地形上提取物理量的能力。在所提出的算法中,地貌特征用地形法向量进行数学表示。通过矢量化概念建立物理量与不同坐标描述之间的相关性,最终在复杂地形上以 SPH 形式有效提取物理量。该算法为将与地形相关的物理模型纳入离散化框架提供了重要工具。为了验证该算法的有效性,我们以 2010 年日本 Yohutagawa 泥石流事件为例,使用该算法将泥石流夹带规律与我们之前的 HBP-SPH 模型进行了整合。结果表明,数值模拟与现场观测结果非常吻合。本文最后讨论了该算法的适用性和局限性。
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来源期刊
Engineering Geology
Engineering Geology 地学-地球科学综合
CiteScore
13.70
自引率
12.20%
发文量
327
审稿时长
5.6 months
期刊介绍: Engineering Geology, an international interdisciplinary journal, serves as a bridge between earth sciences and engineering, focusing on geological and geotechnical engineering. It welcomes studies with relevance to engineering, environmental concerns, and safety, catering to engineering geologists with backgrounds in geology or civil/mining engineering. Topics include applied geomorphology, structural geology, geophysics, geochemistry, environmental geology, hydrogeology, land use planning, natural hazards, remote sensing, soil and rock mechanics, and applied geotechnical engineering. The journal provides a platform for research at the intersection of geology and engineering disciplines.
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