用于地下地层学的三维体素地质建模:图卷积网络方法

Lai Wang, Qiujing Pan, Shan Huang, Dong Su
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引用次数: 0

摘要

三维(3D)地质建模增强了对复杂地下地层的理解和可视化,是岩土工程数字孪生和弹性设计的基础。现有的三维地质建模方法在进行具有复杂地下地层的大尺度区域建模时,要么计算量大,要么建模精度低。本文提出了一种新颖的深度学习方法,将图卷积网络(GCN)应用于使用有限钻孔的三维体素地质建模。首先构建拓扑图,将空间点编码为图节点。地层类型和空间坐标被纳入每个节点的特征向量。通过连接立方体相邻系统内的节点对,以加权边量化空间相关性。此外,地层在所有钻孔中的出现概率也被嵌入到每个图节点的特征向量中,以进一步提高模型的鲁棒性。一系列比较表明,所提出的方法在建模精度方面优于传统的 TPS 和 MPS 方法。最后,将所提出的方法应用于长沙市的实际隧道工程中,证明了所提出的方法在复杂三维地质环境中的有效性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Three-dimensional voxel geological modelling for subsurface stratigraphy: A graph convolutional network approach
Three-dimensional (3D) geological modelling enhances the understanding and visualisation of complex subsurface stratigraphy, which underpins geotechnical digital twin and resilience design. Existing methods for 3D geological modelling suffer from either high computational burden or low modelling accuracy in large-scale region modelling with complex subsurface stratigraphy. This paper presents a novel deep learning method that applies the graph convolutional network (GCN) to 3D voxel geological modelling using limited boreholes. A topological graph is firstly constructed, with spatial points encoded as graph nodes. The strata types and spatial coordinates are incorporated into the feature vector of each node. Spatial correlations are quantified through weighted edges by connecting pairs of nodes within a cuboid neighbouring system. Besides, the occurrence probability of strata in all boreholes is embedded into the feature vector of each graph node to further improve the model robustness. A series of comparisons shows that the proposed method outperforms traditional TPS and MPS methods in terms of modelling accuracy. The proposed method is finally applied to a real tunnel engineering in Changsha City, which demonstrates the effectiveness of the proposed method in complex 3D geological settings.
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