The performance of an aerated horizontal subsurface flow treatment wetland was investigated before, during and after a simulated aeration failure. Conventional wastewater parameters (e.g., carbonaceous biological oxygen demand, total nitrogen, and Escherichia coli) as well as selected micropollutants (caffeine, ibuprofen, naproxen, benzotriazole, diclofenac, acesulfame, and carbamazepine) were investigated. Furthermore, the removal of biological effects was investigated using in vitro bioassays. The six bioassays selected covered environmentally relevant endpoints (indicative of activation of aryl hydrocarbon receptor, AhR; binding to the peroxisome proliferator-activated receptor gamma, PPARγ; activation of estrogen receptor alpha, ERα; activation of glucocorticoid receptor, GR; oxidative stress response, AREc32; combined algae test, CAT). During the aeration interruption phase, the water quality deteriorated to a degree comparable to that of a conventional (non-aerated) horizontal subsurface flow wetland. After the end of the aeration interruption, the analytical and biological parameters investigated recovered at different time periods until their initial treatment performance. Treatment efficacy for conventional parameters was recovered within a few days, but no complete recovery of treatment efficacy could be observed for bioassays AhR, AREc32 and CAT in the 21 days following re-start of the aeration system. Furthermore, the removal efficacy along the flow path for most of the chemicals and bioassays recovered as it was observed in the baseline phase. Only for the activation of AhR and AREc32 there was a shift of the internal treatment profile from 12.5% to 25% (AhR) and 50% (AREc32) of the fractional length.

Le but de ce travail est de tester une approche multi-traceurs permettant de caractériser l'origine (éléments majeurs, Sr, Br, 87Sr/86Sr, δ18O, δ2H) et les temps de résidence (3H/3He, CFC, SF6) des eaux, pour identifier l'origine et évaluer le devenir des contaminants dans une nappe alluviale superficielle et peu profonde, la nappe de la Vistrenque. Les molécules étudiées sont les triazines, le métolachlore, le diuron, la carbamazépine, le sulfaméthoxazole, le diclofénac et l'ibuprofène. L'aquifère étudié est alimenté par une recharge directe, occasionnant le lessivage des pesticides des sols, et une recharge latérale provenant de l'aquifère karstique adjacent entraînant une dilution des eaux de la nappe en triazines. Localement, une contribution des eaux de surface (cours d'eau locaux, eau importée du Rhône) à la recharge de la nappe est mise en évidence entraînant également une dilution des eaux de la nappe en triazines mais au contraire une contamination en COE, quoique, en faibles concentrations. Les âges apparents des eaux alluviales échantillonnées, déterminés principalement par le couple 3H/3He, varient entre 1.4 et 22 ans. Le couplage de l'âge des eaux à leurs teneurs en triazines montre une persistance de ces molécules dans le milieu souterrain, et une atténuation de leur signal d'entrée soulignant l'efficacité de leur interdiction en 2003. Finalement, les eaux de la nappe alluviale montrent des rapports de dégradation des triazines variant entre 0,3 pour les eaux influencées par les eaux de surface et 4,8 pour celles montrant des âges apparents de 22 ans, suggérant une augmentation de ce rapport avec le temps de transfert des pesticides dans le système. / The aim of this work is to test a multi-tracer approach allowing the characterization of groundwater origin and residence time in a shallow alluvial aquifer, the Vistrenque aquifer, in order to identify the origin and the fate of contaminants therein. The selected compounds for the study are triazines, metolachlor, diuron, carbamazepine, sulfamethoxazole, diclofenac, and ibuprofen. The studied aquifer is mainly fed by 1) a direct recharge inducing pesticides leaching from soil layers and unsaturated zone and 2) by a lateral recharge from the karst adjacent aquifer, which induces triazines dilution in the alluvial aquifer. A local contribution of surface water (local streams and imported Rhône River water) was evidenced in the alluvial groundwater inducing also triazines dilution but EOCs contamination nevertheless at low concentrations. The apparent age of the alluvial groundwater samples varies between 1.4 and 22 years. Linking groundwater age to triazines contents allowed to highlight, first, the persistence of these compounds in the alluvial groundwater and, second, the decreasing of their input signal in relatively recent groundwater samples in accordance with their forbidding in 2003. Finally, the Vistrenque alluvial groundwater showed triazines degradation ratios varying from 0.3 for groundwater influenced by surface water infiltration to 4.8 for groundwater characterized by relatively older apparent residence time on the order of 22 years. This suggests an increasing ratio with the transfer time of these compounds in the alluvial aquifer system.