%0 Journal Article
%9 ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES
%A Larose, E.
%A Carrière, S.
%A Voisin, Christophe
%A Bottelin, P.
%A Baillet, L.
%A Gueguen, P.
%A Walter, F.
%A Jongmans, D.
%A Guillier, Bertrand
%A Garambois, S.
%A Gimbert, F.
%A Massey, C.
%T Environmental seismology : what can we learn on earth surface processes with ambient noise ?
%D 2015
%L fdi:010064165
%G ENG
%J Journal of Applied Geophysics
%@ 0926-9851
%K Environmental seismology ; Engineering seismology ; Ambient noise ; Hydrology ; Thermo-mechanics
%M ISI:000353425500007
%P 62-74
%R 10.1016/j.jappgeo.2015.02.001
%U https://www.documentation.ird.fr/hor/fdi:010064165
%> https://www.documentation.ird.fr/intranet/publi/2015/05/010064165.pdf
%V 116
%W Horizon (IRD)
%X Environmental seismology consists in studying the mechanical vibrations that originate from, or that have been affected by external causes, that is to say causes outside the solid Earth. This includes for instance the coupling between the solid Earth and the cryosphere, or the hydrosphere, the anthroposphere and the specific sources of vibration developing there. Environmental seismology also addresses the modifications of the wave propagation due to environmental forcing such as temperature and hydrology. Recent developments in data processing, together with increasing computational power and sensor concentration have led to original observations that allow for the development of this new field of seismology. In this article, we will particularly review how we can track and interpret tiny changes in the subsurface of the Earth related to external changes from modifications of the seismic wave propagation, with application to geomechanics, hydrology, and natural hazard. We will particularly demonstrate that, using ambient noise, we can track 1) thermal variations in the subsoil, in buildings or in rock columns; 2) the temporal and spatial evolution of a water table; 3) the evolution of the rigidity of the soil constituting a landslide, and especially the drop of rigidity preceding a failure event.
%$ 066