Le code de la santé publique et notamment l’arrêté du 11 janvier 2007, relatif auxlimites et références de qualité des eaux brutes et des eaux destinées à la consommationhumaine, fixe quatre indicateurs de la qualité radiologique des eaux du robinet(l’activité αglobale, l’activité β globale, l’activité du tritium et la dose totaleindicative), ainsi que des valeurs guides et des références de qualité. Les chroniquesissues de la surveillance des eaux filtrées du Rhône aval montrent que, si laradioactivité d’origine naturelle demeure bien évidemment constante au cours du temps, lesniveaux de contamination radioactive d’origine artificielle ont fortement diminué à partirdu début des années 90, de 10 à 100 fois suivant les radionucléides. Les donnéessoulignent également qu’aucune des limites d’activités α globale, β globale et en tritium n’aété dépassée dans l’eau filtrée du Rhône aval au cours de l’ère industrielle nucléaire.Les doses totales indicatives (DTI) calculées à partir des prélèvements d’eau filtrée duRhône aval (canal Philippe Lamour – Réseau hydraulique régional propriété de la régionLanguedoc Roussillon géré par BRL), de l’Orb et de l’Hérault effectués en 2011 sont trèsinférieures à la valeur de référence de 100 μSv/an. La contribution à la DTI des radionucléidesartificiels détectés dans ces hydrosystèmes est en outre négligeable (<0,01 %).

The Rhône watershed extends over almost one hundred thousands square kilometers, i.e. one fifth of the metropolitan French territory. The Rhône is the major River entering the Western Mediterranean Sea as it generates the main source of sediments and freshwater (50%) to the sea, with an average water discharge of 1700 m3 s-1. The River input affects primary production significantly in the north-western Mediterranean area and plays a leading role on the marine ecosystem functioning in the whole Gulf of Lion. Almost twenty nuclear reactors are situated along the Rhône valley, representing Europe’s biggest concentration of nuclear power plants. Down flow all these installations the spent fuel reprocessing plant of Marcoule released over many years most of the liquid radioactive wastes including plutonium isotopes in the Rhône river. Artificial radionuclides also originate from the weathering of the catchment basin labeled by both the global and the Chernobyl accident atmospheric fallout. These radioactive inputs have led to a permanent contamination of the Rhône river waters. Long-term chronological series of artificial radionuclide activities within the waters at the lower reaches of the Rhône river were acquired from 1979 to 2002. These data give evidence for various radioecological responses of the aquatic system over years. Based on these observations several major radioecological sensitivity factors for river waters are identified.

The macrobenthic fauna of the Rhône River below Lake Geneva was studied between 1983 and 1993 to describe patterns of longitudinal and temporal community changes. Sampling was based upon the use of artificial substrates in 11 stations. The confluence with the Arve (an alpine tributary) is the first source of faunal discontinuity, both in terms of species and feeding group composition. The Verbois hydropower plant is the second longitudinal disruption. From a temporal point of view, the construction of the Seujet hydropower plant was a major source of faunal fluctuation. After this event, and until the end of the study, lenitophilous taxa increased to the detriment of rheophilous taxa.

In running water, the main natural factor of disturbance is hydraulic. Investigation of its biological impact is currently complicated by the increase of anthropogenic disturbances which tend to mask the natural functioning of rivers. Monitoring of the impacts of the artificial alterations undergone by the Middle Rhone River for some decades took place in the mid-1980s. Discharge and temperature could constitute the major events controlling the biological dynamics in terms of variations in species richness, diversity, and abundance. The between-years changes of the structure and diversity of macroinvertebrate communities were connected with the amplitude of discharge fluctuations. This was in accordance with the disturbance-diversity concept and it seems to confirm the intermediate disturbance hypothesis. The fish community mainly depended on hydroclimatic factors that influenced breeding success. Variations in nutrient input played a secondary role in controlling changes in some communities (particularly the periphyton). Therefore it appears that the study of long-term changes in river systems, including the dynamics of their biological communities, requires continuous observations and data collection that only medium- to long-term studies can provide, implying the setting up of ecological monitoring centres for the natural environment such as the Long Term Ecological Research (LTER) sites in United.

The application of fisheries acoustics in shallow waters opens new fields of observation and allows new methods for abundance estimates. In this paper we deal with echocounting of migrating fish crossing the Beaucaire-Vallabrègues lock, the first obstacle encountered on the Rhône, using a SIMRAD EY500 split-beam sounder, 70 kHz frequency. Two transducers sampled a section of water and evaluated approximately 35% of the lock section, based on a calibration sphere. The number of fish crossing the lock was calculated for each fish lock. Crossing data for the fish were recorded (dates, position, exit time). The present analysis did not allow the identification of the two major species that cross the dam: shad (Alosa fallax) and mullet (Mugil cephalus). The number of fish counted was positively correlated with the catches per unit effort (CPUE) by recreating fishermen below the dam and with increasing water temperature.

1. The importance of microhabitat characteristics for macroinvertebrate microdistribution was studied within a reach of themain channel of the Upper Rhône River (France). 9 locations (3 on the left hand side, 3 across the middle, and 3 on the righthand side) were sampled twice on two dates (as duplicates in June and July 1982). From 19 variables, including substratum andhydraulic parameters, 14 were selected to describe the physical habitat of each location. 47 macroinvertebrate species were collectedby means of dredging with a modified Rallier du Baty dredge. The habitat-fauna co-structure was studied using co-inertiaanalysis.2. The river reach was transversally asymmetrical : shallow on one side (up to 2.80 m) with coarse sediments rich in periphyton,and much deeper on the other side (up to 4.80 m) with a gravel bottom rich in organic particles. In the middle of thechannel these conditions were intermediate, but the current was stronger. Velocity and the other hydraulic parameters variedindependently of the substratum characteristics. This independence is a consequence of old man-made impoundments (inheritedstructures) and perhaps of present paving of the substratum also.3. The macroinvertebrate fauna was closely linked to this transverse asymmetry of the reach, with the highest richness andabundance to the shallow side of the channel and the lowest species richness in the rapid central part. The most significant faunisticdifferences were linked i) to water depth, acting on both hydraulic parameters and periphyton (by light transmission), ii)to the inherited old bottom substratum, and iii) to a lesser extent, to the present current velocity.