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Daniel Locci-Lopez and Juan M. Lorenzo
Shear-wave seismic reflection velocity-versus-depth models can complement our understanding of seepage pore pressure variations beneath earthen levees at locations between geotechnical sites. The seasonal variations of water level in the Mississippi Rive...
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Nikita Dubinya, Irina Bayuk, Alexei Hortov, Konstantin Myatchin, Anastasia Pirogova and Pavel Shchuplov
The paper discusses the problem of localizing zones of high pore pressure in sub-bottom sediments (first tens of meters under the seafloor). Prediction of the overpressure zones in the near-surface is required for the mitigation of risks at the early sta...
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Seong-Kyu Yun, Jiseong Kim, Eun-Sang Im and Gichun Kang
This study deals with the utilization of the pore pressure meter for evaluating the stability of a dam through the correlation between the porewater pressure installed in the fill dam and the water level of the dam. To this end, principal components anal...
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Khusmia Karin,. Sudarmaji
Pág. 117 - 128
Block F3 North Sea is a block with pore pressure values that vary over time due to complex geological conditions such as burial and various sedimentation zones. Pore pressure is one of the important aspects that need to be analyzed as a basis for the ide...
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Zsolt Nagy, Mátyás Krisztián Baracza and Norbert Péter Szabó
The overpressure formation in the Pannonian basin, Hungary, was investigated but has not been properly understood for the last 40 years because at least two different explanations were delineated. The first explanation considers the hydrocarbon generatio...
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Thilanki Dahigamuwa, Manjriker Gunaratne and Mingyang Li
The infiltration of rainwater into soil slopes leads to an increase of porewater pressure and destruction of matric suction, which causes a reduction in soil shear strength and slope instability. Hence, surface moisture and infiltration properties must b...
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Raül Oorthuis, Marcel Hürlimann, Alessandro Fraccica, Antonio Lloret, José Moya, Càrol Puig-Polo and Jean Vaunat
Slope mass-wasting like shallow slides are mostly triggered by climate effects, such as rainfall, and soil?vegetation?atmosphere (SVA) interactions play a key role. SVA interactions are studied by a full-scale embankment with different orientations (Nort...
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