Deciphering near-surface architecture and landslide triggers in granitic environments: A regression-driven multiphysics modeling framework for geoengineering integrity

IF 4.1 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Adedibu Sunny Akingboye , Andy Anderson Bery , Hui Tang , Meng Heng Loke , Muslim Babatunde Aminu , Taiwo Adewumi , Muhammad Hasan
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引用次数: 0

Abstract

In crystalline basement terrains, understanding near-surface crustal architecture is vital for assessing geoengineering integrity and mitigating landslide risks. This study focuses on the granitic terrain of Penang Island, Malaysia, where rapid urbanization and landslides could threaten infrastructure stability. Integrating multiphysics with statistically optimized borehole-based rock quality designation (RQD) modeling provides the first geophysical–geotechnical–statistical framework to evaluate lithological conditions and landslide triggers in granitic terrains. The innovative methodology develops lithology-based geoengineering integrity models to assess soil–rock profiles at steep and low-lying sections across four sites: Sungai Ara (east; Site 1), Batu Maung (south; Site 2), Jelutong (north; Site 3), and Balik Pulau (west; Site 4). The findings identify varied subsurface characteristics using resistivity and seismic P-wave velocity tomographic models, correlated with borehole logs and RQD data. The subsurface is categorized into residual soils, highly to moderately weathered/fractured granite, and hard/fresh granitic bedrock. The study framework revealed contrasting lithologic differentiation between southern Penang Island and the northern section, including the western and eastern parts, likely due to differences in granitic feldspar magma mineralogy and susceptibility to weathering. Sites 1, 3, and 4 are dominated by lower resistivity and seismic velocity values—indicating weaker, looser, and deeper weathered materials—whereas Site 2 is characterized by more compact, sandy-rich residual soils and hard/fresh bedrock with deeper fractures. Weathered and fractured zones amplify water–rock interactions, increasing pore pressure and landslide susceptibility in the area. Contractive clay/silt (<200 Ωm) and water-escape structures within creeping residual soils are identified as primary landslide triggers, particularly in unstable, steep sections. For infrastructure design integrity, reinforced piling foundations reaching fresh granitic bedrock (RQD Units III and IV) are recommended. These measures are crucial in Penang's rapidly urbanizing terrain with numerous tall buildings. While site-specific, the study introduces a globally adaptable framework for cost-effective, large-scale geoengineering assessments in similar geological contexts, enhancing risk mitigation and infrastructure design strategies.
解读花岗岩环境中的近地表结构和滑坡触发因素:地球工程完整性的回归驱动多物理场建模框架
在结晶基底地形中,了解近地表地壳结构对于评估地球工程完整性和减轻滑坡风险至关重要。本研究的重点是马来西亚槟城岛的花岗岩地形,那里的快速城市化和山体滑坡可能威胁到基础设施的稳定性。将多物理场与统计优化的钻孔岩石质量指定(RQD)建模相结合,为评估花岗岩地形的岩性条件和滑坡触发因素提供了第一个地球物理-岩土工程-统计框架。该创新方法开发了基于岩性的地球工程完整性模型,用于评估四个站点的陡峭和低洼路段的土壤-岩石剖面:Sungai Ara(东部;峇都貌(南;场址2),路通(北;地盘3)及巴力克岛(西面;网站4)。研究结果利用电阻率和地震纵波速度层析模型,结合井眼测井和RQD数据,确定了不同的地下特征。地下分为残余土壤、高度至中度风化/断裂花岗岩和坚硬/新鲜花岗岩基岩。研究框架揭示了槟城岛南部与北部(包括西部和东部)的岩性差异,这可能是由于花岗岩长石岩浆矿物学和风化敏感性的差异。站点1、3和4以较低的电阻率和地震速度值为主,表明风化物质更弱、更疏松、风化程度更深,而站点2的特征是更致密、富含沙质的残余土壤和坚硬/新鲜基岩,裂缝更深。风化和破裂带放大了水岩相互作用,增加了该地区的孔隙压力和滑坡易感性。收缩粘土/淤泥(<200 Ωm)和蠕变残积土中的泄水结构被认为是主要的滑坡诱因,特别是在不稳定的陡峭地段。为了基础设施设计的完整性,建议采用加固桩基础,达到新鲜的花岗岩基岩(RQD单元III和IV)。这些措施对于槟城快速城市化的地形和众多高层建筑至关重要。虽然具体地点不同,但该研究提出了一个适用于全球的框架,用于在类似地质背景下进行具有成本效益的大规模地球工程评估,加强风险缓解和基础设施设计战略。
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来源期刊
Physics and Chemistry of the Earth
Physics and Chemistry of the Earth 地学-地球科学综合
CiteScore
5.40
自引率
2.70%
发文量
176
审稿时长
31.6 weeks
期刊介绍: Physics and Chemistry of the Earth is an international interdisciplinary journal for the rapid publication of collections of refereed communications in separate thematic issues, either stemming from scientific meetings, or, especially compiled for the occasion. There is no restriction on the length of articles published in the journal. Physics and Chemistry of the Earth incorporates the separate Parts A, B and C which existed until the end of 2001. Please note: the Editors are unable to consider submissions that are not invited or linked to a thematic issue. Please do not submit unsolicited papers. The journal covers the following subject areas: -Solid Earth and Geodesy: (geology, geochemistry, tectonophysics, seismology, volcanology, palaeomagnetism and rock magnetism, electromagnetism and potential fields, marine and environmental geosciences as well as geodesy). -Hydrology, Oceans and Atmosphere: (hydrology and water resources research, engineering and management, oceanography and oceanic chemistry, shelf, sea, lake and river sciences, meteorology and atmospheric sciences incl. chemistry as well as climatology and glaciology). -Solar-Terrestrial and Planetary Science: (solar, heliospheric and solar-planetary sciences, geology, geophysics and atmospheric sciences of planets, satellites and small bodies as well as cosmochemistry and exobiology).
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