TY - CONF

T1 - COMSOL SIMULATION OF THE ELECTROKINETIC EFFECT IN GIDROGEOLOGY

AU - Narbut, M.A.

AU - Titov, K.V.

AU - Konosavsky, P.K.

PY - 2015

Y1 - 2015

N2 - The groundwater flow is accompanied by the electric field with potential called usually the streaming potential or the Self-Potential (SP) to be measured on the ground surface We studied numerically the SP signals associated with pumping test experiments in layered aquifers using COMSOL Multiphysics and GWFGEM program developed by one of the authors (Titov et al., 2005). The cases of conductive (metallic) tube in the pumping well and the insulating one were considered. The work is supported by Saint Petersburg University grant 6.37.171.2014.

AB - The groundwater flow is accompanied by the electric field with potential called usually the streaming potential or the Self-Potential (SP) to be measured on the ground surface We studied numerically the SP signals associated with pumping test experiments in layered aquifers using COMSOL Multiphysics and GWFGEM program developed by one of the authors (Titov et al., 2005). The cases of conductive (metallic) tube in the pumping well and the insulating one were considered. The work is supported by Saint Petersburg University grant 6.37.171.2014.

KW - streaming potential

KW - pumping test experiments

KW - layered aquifers?numerical methods

M3 - Abstract

T2 - European COMSOL Conference 2015 Grenoble

Y2 - 13 October 2015 through 15 October 2015

ER -