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- W2555366324 abstract "RESUME Les argiles Champlain recouvrent les basses terres de la vallee du Saint-Laurent au Quebec, dans l’est du Canada. Ces argiles ont ete deposees il y a approximativement 12000 a 8500 ans dans la mer Champlain, tard dans la periode du Quaternaire. Les argiles Champlain jouent un role crucial dans le controle des ecoulements souterrains. Ces argiles controlent et protegent les aquiferes sous-jacents des contaminants en provenance de la surface ou des couches plus permeables pres de la surface. La conductivite hydraulique (K) est un parametre fondamental pour estimer la vitesse d’ecoulement, la vitesse de migration des contaminants et la consolidation des argiles. Du point de vue de la geotechnique, des valeurs representatives des parametres elastiques de l’argile applicables a de tres faibles deformations sont necessaires pour comprendre le comportement de l’argile sous des sollicitations dynamiques.----------ABSTRACT Champlain clays cover the lowlands of the Saint Lawrence River valley in Quebec, in eastern Canada. The clays were deposited approximately from 12000 to 8500 BP (before present) in the Champlain Sea, during the late Quaternary Period. Champlain clay aquitards play a crucial role in defining groundwater regimes; they control recharge and protect underlying aquifers from surface contamination. The clay K value is a fundamental parameter to estimate flow velocity, the rates of contaminant migration, and time-dependent clay deformation. From a geotechnical standpoint, representative values of the clay elastic parameters for very small-strain are needed to understand the dynamic behaviour of clay deposits." @default.
- W2555366324 created "2016-11-30" @default.
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- W2555366324 date "2016-04-01" @default.
- W2555366324 modified "2023-09-26" @default.
- W2555366324 title "Natural Pore Pressure Fluctuations in a Champlain Clay Deposit" @default.
- W2555366324 hasPublicationYear "2016" @default.
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