LOCATING AND ESTIMATING SUBMARINE FRESH-W ATER DISCHARGE FROM AN INTERSTITIAL CONFINED COASTAL AQUIFER BY MEASUREMENTS AT SEA - EXAMPLE FROM THE LOWER VAR VALLEY, FRANCE
Y. Guglielmi et L. Prieur, LOCATING AND ESTIMATING SUBMARINE FRESH-W ATER DISCHARGE FROM AN INTERSTITIAL CONFINED COASTAL AQUIFER BY MEASUREMENTS AT SEA - EXAMPLE FROM THE LOWER VAR VALLEY, FRANCE, Journal of hydrology, 190(1-2), 1997, pp. 111-122
At the mouth of the river Var (Mediterranean Sea, France), the aquifer
which is contained within recent alluvial deposits becomes confined a
s it flows under impermeable sediments of a small coastal delta. To st
udy the water balance of the alluvial aquifer, we used a method of loc
alization and in situ quantification of freshwater discharge into the
sea. Vertical profiles of both salinity and temperature and systematic
chemical analyses of seawater were made at 40 stations located on two
concentric half-circle shaped routes linking the eastern bank of the
river mouth to the southern one. Anomalies appear at some stations on
the two routes, where, at depths of 20-60 m, profiles show a temperatu
re elevation of 0.1-0.2 degrees C and a salinity decrease of 0.05-0.1
PSU compared with the average value (PSU is an abbreviation for 'Pract
ical Scale Unit', defined by SCORE-UNESCO as the new salinity unit; th
is unit corresponds to parts per thousand (per mille), which is equiva
lent to 1 g of salt for 1 kg of seawater). In addition, lower than ave
rage values of seawater ionic concentrations of Mg2+, Ca2+ and K+ and
higher than average content of silica, a local groundwater tracer, con
firm the existence of freshwater discharge areas. These marine outlets
are located where the deltaic impermeable sedimentary cover is thin o
r even nonexistent. An attempt to evaluate the flow rate is made by es
timating the dynamic diffusion of the salt flux over the whole dischar
ge area, The results range from 180 to 4001 s(-1), in agreement with v
alues indirectly deduced from water balance calculations. The importan
t uncertainty of the measurement is due to the choice of the dynamic d
iffusion coefficient (ranging from 10 to 20 m(2) day(-1)), the approxi
mation of salinity variations (ranging from 0.05 to 0.1 PSU) and the t
hickness of the discharge area (ranging from 20 to 40 m).