P. Weng et al., Groundwater circulations between alluvial aquifer and underlying senonian chalk in the Seine Valley, PHYS CH P B, 24(1-2), 1999, pp. 151-154
Citations number
9
Categorie Soggetti
Earth Sciences
Journal title
PHYSICS AND CHEMISTRY OF THE EARTH PART B-HYDROLOGY OCEANS AND ATMOSPHERE
Hundred kilometres upstream from Paris, on the confluence of the Seine and
Aube rivers, riverine wetlands expand every year, resulting of flooding and
/or upward movement of water in aquifers. In this region, the groundwater s
ystem is made up of an alluvial aquifer (alluvial deposits are Neogene-Quat
ernary) that fits into an underlying senonian chalky aquifer. In the alluvi
al aquifer, the water level is 2 m below the soil during the major part of
the year but has been recorded far from the surface and sometimes above the
surface in winter. This paper report the water circulations between those
aquifers on an interannual scale. We thus pointed up a contribution of wate
r of 400 Mm(3).yr(-1) from the Senonian aquifer to the alluvial aquifer, an
d a residence time of water in the alluvial deposits of about 2 years. Fina
lly, those values have been corroborated by a modelisation of the Senonian
aquifer using MODFLOW. (C) 1998 Elsevier Science Ltd. All rights reserved.