S. Santiago et al., NUTRIENT, HEAVY-METAL AND ORGANIC POLLUTANT COMPOSITION OF SUSPENDED AND BED SEDIMENTS IN THE RHONE RIVER, Aquatic sciences, 56(3), 1994, pp. 220-242
Citations number
48
Categorie Soggetti
Water Resources",Limnology,"Marine & Freshwater Biology
The environmental quality of the Rhone River (Switzerland-France) has
been assessed with a geochemical survey of the pollutants bound to sus
pended sediments. Ten samples were collected between Lake Geneva and t
he Mediterranean Sea in November 1989 by continuous flow centrifugatio
n and analysed for grain size distribution, carbonate, organic C, N, f
orms of particulate P, trace metals, and organic compounds (chlorobenz
enes, organochlorine pesticides, PCBs, and PAHs). Four bed sediment sa
mples win also studied for comparative purposes. The suspended solids
provide lower variance by parameter than the bed sediments and are cle
arly most suitable for synoptic monitoring. The Upper Rhone River carr
ies a glacial derived sediment with a low nutrient content, the stretc
h from Geneva to Lyon provides a sediment dominated by carbonate, and
in the Lower Rhone the organic matter and phosphorus are relatively in
creased, mainly due to wastewater effluents and to an industrial P sou
rce. High concentrations of metals and organic micropollutants downstr
eam of Lyon indicate a multiple contamination in the Lower Rhone, wher
eas mon specific inputs are located downstream of Geneva and Arles. Th
e comparison with data from other polluted major systems, the Rhine, t
he Niagara and the Detroit rivers, shows on overall similarity confirm
ing that the Rhone quality is degraded downstream of Lyon. The levels
of particular concern are for Hg, DDT metabolites which reveal a recen
t release in the basin, PCBs with a likely high chlorine content, and
PAHs. The statistical evaluation of the compositional variables indica
tes a limited number of well defined associations, suggesting that the
contamination of the suspended sediments results from the combination
of numerous and intermittent point and diffuse sources in the Rhone R
iver basin.