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Jacques Locat

Researcher at Laval University

Publications -  175
Citations -  5615

Jacques Locat is an academic researcher from Laval University. The author has contributed to research in topics: Landslide & Submarine landslide. The author has an hindex of 37, co-authored 171 publications receiving 5062 citations. Previous affiliations of Jacques Locat include University of Lausanne.

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Slope failure dynamics and impacts from seafloor and shallow sub-seafloor geophysical data: case studies from the COSTA project

TL;DR: A review and update from original data and literature reports the current state of knowledge of Storegga, Traenadjupet and Finneidfjord slides from the mid-Norwegian margin, Afen Slide from the Faeroe-Shetland Channel, BIG'95 Slide and Central Adriatic Deformation Belt (CADEB) from continental slope and inner continental shelf settings off the Ebro and Po rivers in the Mediterranean Sea, Canary Slide west of the westernmost, youngest Canary Islands and Gebra Slide off the northern tip of the Antarctic Peninsula
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Laboratory investigations on the lime stabilization of sensitive clays: shear strength development

TL;DR: In this paper, a laboratory investigation on the quicklime stabilization of sensitive clays has shown that significant strength increase can be obtained if enough water content above the liquid limit is added to the clays.
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Influence of the nature of organic compounds on fine soil stabilization with cement

TL;DR: In this paper, it is known that organic matter may affect the cementing process in soils, but what happens when cement is added to an organic soil? Both the organic matter content and the nature of this orga...
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Viscosity, yield stress, remolded strength, and liquidity index relationships for sensitive clays

TL;DR: The rheological behavior of some sensitive clays has shown that there are positive relationships between plastic viscosity, yield stress, remolded shear strength, and liquidity index as mentioned in this paper.
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Distinguishing sediment waves from slope failure deposits: Field examples, including the 'humboldt slide', and modelling results

TL;DR: A reassessment of these features strongly suggests that numerous turbidity currents, separated by intervals of ambient hemipelagic sedimentation, deposited the wave fields over thousands of years as discussed by the authors.