Fate of trace metals in anaerobic digestion

© Springer International Publishing Switzerland 2015. A challenging, and largely uncharted, area of research in the field of anaerobic digestion science and technology is in understanding the roles of trace metals in enabling biogas production. This is a major knowledge gap and a multifaceted problem involving metal chemistry; physical interactions of metal and solids; microbiology; and technology optimization. Moreover, the fate of trace metals, and the chemical speciation and transport of trace metals in environments— often agricultural lands receiving discharge waters from anaerobic digestion processes— simultaneously represents challenges for environmental protection and opportunities to close process loops in anaerobic digestion.The authors acknowledge funding within the framework of the COST Action 1302 (‘European Network on Ecological Roles of Trace Metals in Anaerobic Biotechnologies’). GC is supported by a European Research Council Starting Grant (‘3C-BIOTECH; No. 261330).Peer Reviewe

Clostridium quinii sp. no., a new saccharolytic anaerobic bacterium isolated from granular sludge.

International audienceA new species of sporulating saccharolytic anaerobe, designated as Clostridium quinii sp. nov., is described. A gram-positive strain BS1, was isolated from the granular metanogenic sludge (UASB) from a waste-water treatment plant at a sugar refinery. The strain exhibits a series of morphological stages, developing from a spore to a small rod to a motile rod (peritrichous flagella) in the exponential growth phase, and then swelling to form cigar-shaped cells, exhibiting tumbling movements, in the late exponential growth phase before finally becoming large nonmotile ovoid cells in the stationary phase. Swelling occurs as a result of glucose being taken up and stored as a glycogen-like substance. The main fermentation products when growing on glucose is H2, CO2, formate, acetate and ethanol as well as small amounts of butyrate during exponential growth. Lactate is formed during the stationary phase, when glucose is abundant. Optimal conditions for growth is 40–45°C and pH of around 7.4. The type strain BS1 contains 28.0% mol G+C

Characterization of dissolved organic matter in full scale continuous stirred tank biogas reactors using ultrahigh resolution mass spectrometry: A qualitative overview.

Dissolved organic matter (DOM) was characterized in eight full scale continuous stirred tank biogas reactors (CSTBR) using solid-phase extraction and electrospray ionization Fourier transform ion cyclotron resonance mass spectrometry (ESI-FT-ICR-MS). An overview of the DOM molecular complexity in the samples from biogas reactors with conventional operational conditions and various substrate profiles is provided by assignments of unambiguous exact molecular formulas for each measured mass peak. Analysis of triplicate samples for each reactor demonstrated the reproducibility of the solid-phase extraction procedure and ESI-FT-ICR-MS which allowed precise evaluation of the DOM molecular differences among the different reactors. Cluster analysis on mass spectrometric data set showed that the biogas reactors treating sewage sludge had distinctly different DOM characteristics compared to the codigesters treating a combination of organic wastes. Furthermore, the samples from thermophilic and mesophilic codigesters had different DOM composition in terms of identified masses and corresponding intensities. Despite the differences, the results demonstrated that compositionally linked organic compounds comprising 28-59% of the total number of assigned formulas for the samples were shared in all the reactors. This suggested that the shared assigned formulas in studied CSTBRs might be related to common biochemical transformation in anaerobic digestion process and therefore, performance of the CSTBRs

Rewiring of peatland plant–microbe networks outpaces species turnover

Interactions between plant and microbial communities in peatlands are complex, yet pivotal for the functioning of these carbon-dense ecosystems. Our understanding of how climate change affects important peatland processes such as carbon dynamics is often based on assumed fixed relationships between above-and belowground communities. Our work shows that the turnover in plant–microbial interactions along enviro–climatic gradients is faster than species turnover within both communities, resulting in a mismatch in alpha diversity between plant and microbial communities. Notably, warming and increased nutrient deposition weakens plant–microbe linkages, which may consequentially decrease the overall robustness of peatland ecosystem processes to future anthropogenic pressures