Sustainable Solutions for Environmental Pollution, Volume 2. Группа авторов

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alt="images"/> Fe(III), Mn(IV), images and CO2. Adapted from Bertrand et al. (2011; p. 573), Diaz and Rosenberg (2008), and Hargrave et al. (2008).

      If aerobic micro-organisms breathe O2 as terminal electron acceptor (TEA), anaerobic micro-organisms breathe other TEAs, as images or OM, producing noxious gases such as CO2, CH4, N20, H2S, and NH3 (Bertrand et al., 2011). These TEAs yield lower energy than O2, so anaerobic respiration is less energy efficient and anaerobes grow slower than aerobes. Low TEA availability (presence and mobility) often limits self-purification process.

      NBSs of bioremediation aim at optimizing the TEA input needed to on-site self-purification. To do that, they implement three nested logics: action on form or physical structuration of the environment; action on fluxes of water and substances through it; and action on biocenosis living in the ecosystem. Thus, NBSs act on the geomorphology, hydrology, and physical-chemical characteristics of the environment such as in constructed wetlands (CWs) or filtering banks (FBs); on living organisms such as plants in phytoremediation; or on microbial consortia by passive control of the redox potential by supplying electrochemical inexhaustible TEAs in electro-bioremediation.

       1.2.2.2 Photo-Degradation

      Until the end of the 21st century, urban wastewater was extensively discharged into water bodies such as rivers and lakes, without any treatment: the self-purification taking place in these water bodies was supposed to be sufficient. However, microbiology was still in infancy at that time, and drinking water resources, such as surface waters, were often contaminated by waterborne disease agents, such as protozoa (Giardia intestinalis, first described by Antoni van Leeuwenhoek in 1681, Cryptosporidium) and bacteria (Shigella (discovered in 1897 by K. Shiga and causing dysentery), Salmonella enterica (causing typhoid), Vibrio cholerae (cholera agent discovered by Pacini in 1854 and rediscovered by Koch in 1885).

      One of the first “treatments” of urban wastewater was indeed nature-based as it consists to spread wastewater in agricultural fields where it could act as a fertilizer. This practice has lasted for about 100 years in Paris and Reims (France). The contamination of soils by micropollutants (in particular metals such as lead) has led to the abandoning of vegetable crops for non-food crops.

      Because of rapid urbanization, climate change, and extreme weather events induced, water-related issues, such as flooding, groundwater over-exploitation, water shortages, and wastage, and water pollution, are becoming a global concern (Simperler et al., 2020). The development of the concept of sponge cities (Sun et al., 2020) aiming at improving the response of cities to rainfall should take into account the risks of dissemination of micro-pollutants. Constructed Wetlands (CWs) are essential NBS infrastructures in urban water management in the sponge city concept, in order to control the growing menace of urban flooding. With green spaces, rooftop gardens and permeable streets, CWs both “buffer” water flows and reduce flood during storms and purify the pollution carried by rainwater. In fact, they act like a sponge to absorb and treat water before a flood occurs and limit urban heat islands in city (Nguyen et al., 2019b).

      Nowadays, eco-engineering practices attempting to improve bioremediation in rivers receiving untreated or treated municipal and industrial wastewater as well as agricultural or urban runoff focus on physical actions through hydro-geomorphological modifications as constructed swales or riffles across urban creeks (Kasahara et al., 2006; Mendoza-Lera and Datry, 2017). Hydrogeomorphic manipulation of riverbed aims to increase pollution interception and bioprocessing inside the bed and to restore and enhance the river self-purification capacity.

      In running waters, redox processes are not so gradually structured according to depth as described in lake sediments (Bertrand et al., 2011) where a stratified redox gradient, from oxic condition in surface, to suboxic and anoxic conditions is formed (Figure 1.1). Preliminary results show a high sediment functioning heterogeneity according to water flow, geomorphology, hyporheic, and nutrient fluxes due to hydraulic conductivity and hydraulic gradient (Namour et al., 2015). The redox cycling of organic C and N not only drives the micro- and macro-biological communities, but also has implications for global nutrient balances and climate change.

      Structures harboring purifying capacities must selectively trap dissolved pollutants in order to concentrate them and make them available to biomass. Therefore, the zones with the highest assimilation and purification capacities are the zones where the immobilization of pollutants is the highest; this pollutant trapping is a prerequisite at any biodegradation and assimilation. Inside these filtering structures where a large heterotrophic biomass will develop and will be the most active self-purification zones, Sensu lato, we can define four main types of filtering structures:

      1 Mechanical filters, where steric obstruction retains particulates and associated pollutants;

      2 Physical filters which retain dissolved chemical compounds by adsorption;

      3 Physical-chemical filters, in which changes in pH or rH,

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