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Fidele YrroInstitut National de la Recherche Scientifique | INRS · Eau Terre Environnement Centre
Fidele Yrro
Postdoctoral researcher at INRS-ETE (Québec city) CANADA
About
8
Publications
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Introduction
Fidele Yrro currently works at the Department of Civil, Geological and Mining Engineering, Polytechnique Montréal. Fidele does research in Hydrogeology, Geostatistics and Geology. Their most recent publication is 'A METHOD FOR INTEGRATING GROUND AND HELIBORNE TIME-DOMAIN ELECTROMAGNETIC DATA USING A GRADUAL DEFORMATION METHOD OVER ST-LAWRENCE LOWLANDS (QUEBEC, CANADA).'
Publications
Publications (8)
Mining is a major concern for the availability of groundwater resources due to the continual pumping out for pit dewatering. The objective of the study is to assess the impact of mining on the functioning of the aquifer system of the Yaoure Gold Project area. The methodology adopted was to first caracterize the aquifer system by producing the fract...
Sharp-interface seawater intrusion models present shorter run times than variable density codes, which makes them practical for regional, decision-support groundwater modeling. Although parameter estimation and uncertainty analyses are essential steps for model-based decision making, their implementation in seawater intrusion models has remained li...
We propose a new approach for integrating ground-based and heliborne time-domain electromagnetic data over the St-Lawrence Lowlands (Quebec, Canada) that allows recovering the resistivity model of the subsurface satisfying both collected data. The approach uses discrete and continuous geostatistical simulations and the gradual deformation method (G...
High-resolution seismic and sediment core data from the ‘Grand Lac’ basin of Lake Geneva reveal traces of repeated slope instabilities with one main slide-evolved mass-flow (minimum volume 0.13 km3) that originated from the northern lateral slope of the lake near the city of Lausanne. Radiocarbon dating of organic remains sampled from the top of th...
Similarly to steep oceanic continental margins, lake slopes can
collapse, producing large sublacustrine landslides and tsunamis. Lake
sediments are excellent natural archives of such mass movements and
their study allows the reconstructions of these prehistoric events, such
as the 563 AD large tsunami over Lake Geneva (Kremer et al, 2012). In
Lake...
Recent seismic studies in the central part of Lake Geneva have revealed
the presence a series of Holocene sedimentary layers with either
well-organized reflections or with chaotic or transparent seismic
character. While the former correspond to lacustrine sediments deposited
as hemipelagic or turbidite layers, the latter are interpreted to be
relat...