Atténuation | EPFL Graph Search

En électronique, l’atténuation ou affaiblissement est la diminution relative de la puissance d'un signal au cours de sa transmission. C'est la quantité par laquelle il faut multiplier la valeur du signal à la sortie pour obtenir celle à l'entrée de la section considérée. vignette|upright=0.5|Sonde L'atténuation, que ce soit dans une ligne de transmission ou dans un faisceau hertzien, est une grandeur importante dans les télécommunications, dont elle est un facteur limitatif. Ce concept sert aussi en acoustique, notamment en acoustique environnementale pour le calcul de l'isolation phonique. Dans les circuits électroniques, les montages atténuateurs servent pour l'adaptation du niveau du signal entre des parties d'un appareil, sans en modifier d'autre part les caractéristiques. Définitions L'atténuation est Ce rapport s'exprime souvent en décibels. Dans ce cas, la grandeur pertinente est implicitement la puissance et on considère la valeur efficace. L'atténuation est l'i

On-site biostimulation evaluation of a remediated perchloroethene-contaminated acquifer located in Jablunkov, Czech Republic

Isabelle Fäh

Chlorinated ethenes solvents (CEs) are one of the most common contaminants identified in groundwater ecosystems. Long used as a degreaser in industry, perchloroethene (PCE) and trichloroethene (TCE) are particularly persistent in the environment as recalcitrant to oxic degradation, and classified as unhealthy and dangerous for the environment. Under anaerobic conditions, CEs can be degraded naturally in the environment by organohalide respiring bacteria (OHRB) through dehalogenase enzymes reducing them into ethene, a non-hazardous end product. However, toxicity of the intermediate daughter compounds of the degradation (TCE, DCE and VC) is higher than PCE. As this natural attenuation is a slow process, intermediate compounds accumulate in the environment and biostimulation is often used to enhance the complete degradation of CEs. Substrates are added to the contaminated aquifer and used by fermentative bacteria releasing by-product such as H2 that is essential for the dehalorespiration of CEs. Biostimulation has been studied in a PCE contaminated-aquifer located in Jablunkov (Czech Republic). Cheese whey (CW) has been injected into the groundwater in November 2012 and June 2013. The objective of the current project is to evaluate the efficiency of the CW applications by analysing microbiologic and physico-chemical parameters describing the aquifer at six sampling dates from September 2012 to December 2013 within six wells allocated over the aquifer. Global bacterial community structures were analysed in laboratory using Polymerase Chain Reaction (PCR) and T-RFLP (Terminal Restriction Fragment Length Polymorphism). OHRB were analysed as well by specific PCR targeting 16S rRNA and dehalogenase genes of bacteria known to degrade completely the CEs. Then, contaminants and ethene concentrations as well as others Terminal Electron Acceptors implicated in the respiratory processes (Terminal Electron Accepting Processes – TEAPs) were measured to give information about the redox conditions within the aquifer. Finally, others hydrogeological parameters such as pH and temperature were measured. All data were analysed using Multiple Factor Analysis (MFA) in the R software. Interpretations provided a global model indicating the characteristics and functioning of the aquifer. The successive CW applied on-site have a gradual impact on the environmental conditions and on the structures of bacterial communities. After the two CW applications, the aquifer has partly changed to conditions favourable for complete dechlorination. It was the case for three wells over six. Two CW injections have been necessary to allow the production of ethene for two wells whereas only one was needed for the other one. Biostimulation were efficient but not sufficient to completely degrade the CEs on the whole aquifer. In one well, the accumulation of DCE were more important than the production of ethene. In two other wells, ethene was not produced but the statistical analysis showed that they tend toward complete dechlorination conditions. New CW applications would be necessary to completely remediate this aquifer.

2014

Effects of entrance conditions on tidal hydrodynamics in idealized prismatic estuaries under sea level rise

Steve Hottinger

Understanding tidal hydrodynamics response to sea level rise (SLR) in estuaries is essential to predict future potential issues such as shoreline erosion, more frequent and intense flooding, coastal wetland threatening, and their economic and ecological associated losses. By going beyond the classic static or “bathtub” approach, this study uses the RMA-2 modelling software to capture the full energy dynamic resulting from SLR and changes in entrance conditions. Indeed, entrance restrictions are seen as a key factor controlling tidal propagation within the entire system and only little knowledge exists on their effects on the flow under SLR. An innovative numerical approach using idealized prismatic estuaries is undertook to fill this gap. More than 150 simulation cases are performed, varying the channels geometry, restrictions dimensions and tidal forcing to capture most of existing prismatic estuarine dynamics. The resulting tidal flow is described using tidal ranges (TR), but also flow velocity, tidal asymmetry, wave types, tidal prism, etc. to find out potential interesting trends. In short channels, tidal reflection is found to be the dominant process influencing tidal propagation while in long channels the flow is mostly controlled by bottom friction. TR are amplified up to 10% per metre SLR, exacerbating the future flooding problematics linked to a higher mean sea level. However, strong TR attenuation is observed when entrance restrictions are implemented, leading to potential insights on SLR effects mitigation using narrower inlets. SLR acts on the flow velocities distribution and on the tidal asymmetry by increasing medium velocities and decreasing flood dominance. Both will impact sediment transport, leading to stronger coastal erosion. This increases therefore the pressure on sensitive ecosystem already struggling to stay in pace with SLR. SLR can bring the channels closer or further from their natural period of sway. This change in tidal resonance can lead to modifications of the flow parameters behaviour. When channels become more resonant with SLR, amplification of the above phenomena are usually seen, while when they are brought away from resonance, attenuation or even reverse effects can be observed. All these issues are not captured by the bathtub approach and arise from changes in tidal dynamics. Furthermore, instead of focusing on specific estuaries as most of the previous studies, this project is using an idealized approach allowing a global evaluation of the future tidal hydrodynamics. Understanding tidal response to sea level rise in estuaries is crucial to develop efficient coastal management plans able to mitigate this threat on estuarine ecosystems and populated areas. In particular, over 130 port cities having a population higher than 1 million people are concerned by SLR issues in estuaries.

2019

Characterization of Groundwater Microbial Communities, Dechlorinating Bacteria, and In Situ Biodegradation of Chloroethenes Along a Vertical Gradient

Pierre Rossi, Noam Shani

The variability of hydrogeochemical conditions can affect groundwater microbial communities and the natural attenuation of organic chemicals in contaminated aquifers. It is suspected that in situ biodegradation in anoxic plumes of chloroethenes depends on the spatial location of the contaminants and the electron donors and acceptors, as well as the patchiness of bacterial populations capable of reductive dechlorination. However, knowledge about the spatial variability of bacterial communities and in situ biodegradation of chloroethenes in aquifers is limited. Here, we show that changes of the bacterial communities, the distribution of putative dechlorinating bacteria and in situ biodegradation at the border of a chloroethenes plume (Bitterfeld, Germany) are related to local hydrogeochemical conditions. Biotic reductive dechlorination occurred along a 50 m vertical gradient, although significant changes of the hydrogeochemistry and contaminant concentrations, bacterial communities and distribution of putative dechlorinating bacteria (Dehalobacter spp., Desulfitobacterium spp., Dehalococcoides spp., and Geobacter spp.) were observed. The occurrence and variability of in situ biodegradation of chloroethenes were revealed by shifts in the isotope compositions of the chloroethenes along the vertical gradient (δ13C ranging from −14.4‰ to −4.4‰). Our results indicate that habitat characteristics were compartmentalized along the vertical gradient and in situ biodegradation occurred with specific reaction conditions at discrete depth. The polyphasic approach that combined geochemical and biomolecular methods with compound-specific analysis enabled to characterize the spatial variability of hydrochemistry, bacterial communities and in situ biodegradation of chloroethenes in a heterogeneous aquifer.

2011