不连续性分类
岩土工程
地质学
地质力学
磁导率
孔隙水压力
复理石
刚度
山崩
地下水
岩土工程
工程类
沉积岩
数学
结构工程
生物
遗传学
数学分析
古生物学
膜
作者
Luciano Picarelli,Caterina Di Maio,Paolo Tommasi,Gianfranco Urciuoli,Luca Comegna
标识
DOI:10.1016/j.enggeo.2021.106442
摘要
A set of materials covering a wide class comprised between soils and fractured rocks displays a variable and complex hydraulic/mechanical response to external inputs that make both the measurement of properties and the modeling of material behaviour quite complicated. In fact, weak interparticle bonding and a network of irregular and often interconnected discontinuities can strongly and unevenly affect permeability, stiffness and shear strength, making difficult the interpretation of natural events, such as landslides, and uncertain the analysis and design of engineered slopes and man-made works. This paper reports some examples taken from the Authors' experience and from the literature, which illustrate the difficulty to correctly understand or analyze the behaviour of such complex materials through the classical approaches of Soil or of Rock Mechanics, highlighting at the same time the complex role that discontinuities play in groundwater flow and pore water pressure regime.
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