A metamodel for estimating time-dependent groundwater-induced subsidence at large scales

IF 6.9 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Engineering Geology Pub Date : 2024-09-10 DOI:10.1016/j.enggeo.2024.107705
Ezra Haaf , Pierre Wikby , Ayman Abed , Jonas Sundell , Eric McGivney , Lars Rosén , Minna Karstunen
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Abstract

Construction of large underground infrastructure facilities routinely leads to leakage of groundwater and reduction of pore water pressures, causing time-dependent deformation of overburden soft soil. Coupled hydro-geomechanical numerical models can provide estimates of subsidence, caused by the complex time-dependent processes of creep and consolidation, thereby increasing our understanding of when and where deformations will arise and at what magnitude. However, such hydro-mechanical models are computationally expensive and generally not feasible at larger scales, where decisions are made on design and mitigation. Therefore, a computationally efficient Machine Learning-based metamodel is implemented, which emulates 2D finite element scenario-based simulations of ground deformations with the advanced Creep-SCLAY-1S-model. The metamodel employs decision tree-based ensemble learners random forest (RF) and extreme gradient boosting (XGB), with spatially explicit hydrostratigraphic data as features. In a case study in Central Gothenburg, Sweden, the metamodel shows high predictive skill (Pearson's r of 0.9–0.98) on 25 % of unseen data and good agreement with the numerical model on unseen cross-sections. Through interpretable Machine Learning, Shapley analysis provides insights into the workings of the metamodel, which alignes with process understanding. The approach provides a novel tool for efficient, scenario-based decision support on large scales based on an advanced soil model emulated by a physically plausible metamodel.

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估算随时间变化的大尺度地下水诱发沉降的元模型
大型地下基础设施的建设通常会导致地下水的渗漏和孔隙水压力的降低,从而引起覆盖层软土随时间变化的变形。水文地质力学耦合数值模型可以估算由随时间变化的复杂蠕变和固结过程引起的沉降,从而加深我们对何时何地会发生变形以及变形程度的理解。然而,这种水力机械模型的计算成本很高,在较大范围内通常不可行,因为在较大范围内需要对设计和缓解措施做出决策。因此,我们实施了一种基于机器学习的计算效率高的元模型,利用先进的 Creep-SCLAY-1S 模型模拟基于二维有限元场景的地面变形。该元模型采用了基于决策树的集合学习器随机森林(RF)和极梯度提升(XGB),并将空间明确的水文地层数据作为特征。在瑞典哥德堡中部的一项案例研究中,元模型在 25% 的未见数据上显示出较高的预测能力(皮尔逊 r 为 0.9-0.98),并在未见断面上与数值模型保持良好一致。通过可解释的机器学习,夏普利分析提供了对元模型工作原理的见解,这与对过程的理解是一致的。这种方法提供了一种新颖的工具,可根据物理上可信的元模型模拟的先进土壤模型,在大尺度上提供高效、基于情景的决策支持。
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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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