scholarly journals Organic matter diagenesis in freshwater sediments: The alkalinity and total CO2 balance and methane production in the sediments of Lake Washington1,2

1984 ◽  
Vol 29 (6) ◽  
pp. 1218-1230 ◽  
Author(s):  
Kathryn M. Kuivila ◽  
James W. Murray
Keyword(s):  
Organic Matter ◽  
Methane Production ◽  
Freshwater Sediments ◽  
Co2 Balance

Algal blooms modulate organic matter remineralization in freshwater sediments: A new insight on priming effect

2021 ◽  
pp. 147087
Author(s):  
Yarui Wang ◽  
Muhua Feng ◽  
Jianjun Wang ◽  
Xinfang Chen ◽  
Xiangchao Chen ◽  
...  
Keyword(s):  
Organic Matter ◽  
Algal Blooms ◽  
Priming Effect ◽  
Freshwater Sediments

scholarly journals Antibiotics as a silent driver of climate change? A case study investigating methane production in freshwater sediments

2021 ◽  
Vol 228 ◽  
pp. 113025
Author(s):  
E. Bollinger ◽  
J.P. Zubrod ◽  
F.Y. Lai ◽  
L. Ahrens ◽  
S. Filker ◽  
...  
Keyword(s):  
Climate Change ◽  
Methane Production ◽  
Freshwater Sediments

scholarly journals Effects of sulfonamide antibiotics on digestion performance and microbial community during swine manure anaerobic digestion

2020 ◽  
Vol 26 (1) ◽  
Author(s):  
Shaona Wang ◽  
Kang Du ◽  
Rongfang Yuan ◽  
Huilun Chen ◽  
Fei Wang ◽  
...  
Keyword(s):  
Organic Matter ◽  
Anaerobic Digestion ◽  
Dissolved Organic Matter ◽  
Methane Production ◽  
Volatile Fatty Acids ◽  
High Throughput Sequencing ◽  
Batch Reactor ◽  
Inhibition Mechanism ◽  
Sulfonamide Antibiotics ◽  
High Concentration

The effects of four types of sulfonamide antibiotics (SAs), including sulfaquinoxaline, sulfamethoxazole, sulfamethoxydiazine and sulfathiazole, on the digestion performance during anaerobic digestion process were studied using a lab-scale anaerobic sequencing batch reactor, and the changes of the community structure in the presence of SAs were investigated with the help of high throughput sequencing. The results indicated that when SAs were added, the hydrolytic acidification process was inhibited, and the accumulation of volatile fatty acids (VFAs) was induced, resulting in the suppression of methane production. However, the inhibition mechanism of different SAs was quite different. The inhibitory effect of high concentration of SAs on the hydrolysis of solid particulate matter into dissolved organic matter followed the order of sulfaquinoxaline > sulfamethoxydiazine > sulfathiazole > sulfamethoxazole. SAs have obvious inhibitory effects on acidification and methanation of dissolved organic matter, especially sulfathiazole. The richness and the community composition of the microorganism including bacteria and archaea in the digestion system were affected by SAs. Under the effect of SAs, the relative abundance of many microorganisms is negatively correlated with methane production, among which Methanobrevibacter, a kind of Archaea, had the greatest influence on methane production.

Methanogenesis in sediments from deep lakes at different temperatures (2–70°C)

1997 ◽  
Vol 36 (6-7) ◽  
pp. 57-64 ◽  
Author(s):  
Alla N. Nozhevnikova ◽  
C. Holliger ◽  
A. Ammann ◽  
A. J. B. Zehnder
Keyword(s):  
Organic Matter ◽  
Microbial Communities ◽  
Methane Production ◽  
Low Temperatures ◽  
Main Question ◽  
Deep Lakes ◽  
Temperature Range ◽  
Wide Range ◽  
Thermophilic Conditions ◽  
Different Temperatures

Methanogenic degradation of organic matter occurs in a wide temperature range from psychrophilic to extreme thermophilic conditions. Mesophilic and thermophilic methanogenesis is relatively well investigated, but little is known about low temperature methanogenesis and psychrophilic methanogenic communities. The aim of the present work was to study methanogenesis in a wide range of temperatures with samples from sediments of deep lakes. These sediments may be considered deposits of different types of microorganisms, which are constantly exposed to low temperatures. The main question was how psychrophilic methanogenic microbial communities compare to mesophilic and thermophilic ones. Methanogenesis in a temperature range of 2–70°C was investigated using sediment samples from Baldegger lake (65 m) and Soppen lake (25 m), Switzerland. Methane production from organic matter of sediments occurred at all temperatures tested. An exponential dependence of methane production rate was found between 2 and 30°C. Methanogenesis occurred even at 70°C. At the same time stable methane production from organic matter of sediments was observed at temperatures below 10°C. Methanogenic microbial communities were enriched at different temperatures. The communities enriched at 4–8°C had the highest activity at low temperatures indicating that a specific psychrophilic community exists. Addition of substrates such as cellulose, volatile fatty acids (butyrate, propionate, acetate), methanol and H2/CO2 stimulated methane production at all temperatures. H2/CO2 as well as methanol were directly converted to methane under thermophilic conditions. At low temperatures these substrates were converted to methane by a two-step process. First acetate was formed, followed by methane production from acetate. When acetate concentrations were high, acetoclastic methanogenesis was inhibited at low temperatures. This reaction appears to be one of the “bottle neck” in psychrophilic methanogenesis.

scholarly journals In vitro fermentation, digestibility and methane production of tropical perennial grass species

2014 ◽  
Vol 65 (5) ◽  
pp. 479 ◽  
Author(s):  
Belete Shenkute Gemeda ◽  
Abubeker Hassen
Keyword(s):  
Organic Matter ◽  
Methane Production ◽  
Rumen Fluid ◽  
Perennial Grass ◽  
Gas Production ◽  
Automated System ◽  
Grass Species ◽  
Tropical Conditions ◽  
Acid Detergent Fibre

This study characterised 16 tropical perennial grass species in terms of in vitro methane output and related their digestibility and rumen fermentation with methane output. The grass samples were collected, dried in a forced oven, and ground and analysed for nutrient composition. In vitro gas production and organic matter digestibility (IVOMD) were determined using rumen fluid collected, strained and anaerobically prepared. A semi-automated system was used to measure gas production through in vitro incubation at 39°C. Anthephora argentea and Stipagrostis ciliate produced the highest concentration of methane in terms of g kg–1 digestible dry matter (DDM) and g kg–1 digestible organic matter (IVOMD). Cenchrus ciliaris, Setaria verticillata and Panicum coloratum produced the lowest (P < 0.05) methane when expressed in terms of g kg–1 DDM and g kg–1 IVOMD. Ash, ether extract, non-fibrous carbohydrate, neutral and acid detergent insoluble nitrogen, and crude protein were negatively correlated with methane production. Methane production positively correlated with neutral and acid detergent fibre, cellulose and hemicellulose. It is important to focus on screening and selecting perennial grass with higher nitrogen content and low methane production to mitigate methane production under tropical conditions.

Organic matter biodegradation and metal behaviour in contaminated freshwater sediments

2010 ◽  
Vol 12 (1) ◽  
pp. 85 ◽  
Author(s):  
Socorro Pedroza Benitez ◽  
Anne Laure Bussy ◽  
Icela D. Barcelo Quintal ◽  
Edgar Lopez Galvan ◽  
Pedro Avila Perez
Keyword(s):  
Organic Matter ◽  
Freshwater Sediments

Anaerobic Digestion of Solid Wastes Needs Research to Face an Increasing Industrial Success

2008 ◽  
Vol 6 (1) ◽  
Author(s):  
Pierre Buffiere ◽  
Liliana Delgadillo Mirquez ◽  
Jean Philippe Steyer ◽  
Nicolas Bernet ◽  
Jean Philippe Delgenes
Keyword(s):  
Organic Matter ◽  
Anaerobic Digestion ◽  
Methane Production ◽  
Biochemical Parameters ◽  
Energy Production ◽  
Solid Wastes ◽  
High Complexity ◽  
Intrinsic Kinetics ◽  
Anaerobic Biodegradability ◽  
Kinetics Of

Anaerobic digestion of solid wastes is an emerging solution for both waste management and energy production. The high complexity of the process is mostly attributed to the absence of descriptors for the design and the prediction of such a process. This paper presents an approach for the description of organic matter based on several biochemical parameters, established on 22 different organic wastes. The lignocellulosic content is the most important parameter for the prediction of anaerobic biodegradability and methane production; in addition, the knowledge of the carbohydrate, lipid and protein contents is also crucial and makes possible a prediction of the intrinsic kinetics of the reaction.

scholarly journals Belowground in situ redox dynamics and methanogenesis recovery in a degraded fen during dry-wet cycles and flooding

2012 ◽  
Vol 9 (8) ◽  
pp. 11655-11704 ◽  
Author(s):  
C. Estop-Aragonés ◽  
K.-H. Knorr ◽  
C. Blodau
Keyword(s):  
Organic Matter ◽  
Water Table ◽  
Methane Production ◽  
Solid Phase ◽  
Electron Flow ◽  
Organic Matter Content ◽  
Matter Content ◽  
Electron Acceptors ◽  
Oxygen Penetration ◽  
Ch4 Production

Abstract. Climate change induced drying and flooding may alter the redox conditions of organic matter decomposition in peat soils. The seasonal and intermittent changes in pore water solutes (NO3−, Fe2+, SO42−, H2S, acetate) and dissolved soil gases (CO2, O2, CH4, H2) under natural water table fluctuations were compared to the response under a reinforced drying and flooding in fen peats. Oxygen penetration during dryings led to CO2 and CH4 degassing and to a regeneration of dissolved electron acceptors (NO3−, Fe3+ and SO42−). Drying intensity controlled the extent of the electron acceptor regeneration. Iron was rapidly reduced and sulfate pools ~ 1 mmol L−1 depleted upon rewetting and CH4 did not substantially accumulate until sulfate levels declined to ~ 100 μmoll−1. The post-rewetting recovery of soil methane concentrations to levels ~ 80 μmoll−1 needed 40–50 days after natural drought. This recovery was prolonged after experimentally reinforced drought. A greater regeneration of electron acceptors during drying was not related to prolonged methanogenesis suppression after rewetting. Peat compaction, solid phase content of reactive iron and total reduced inorganic sulfur and organic matter content controlled oxygen penetration, the regeneration of electron acceptors and the recovery of CH4 production, respectively. Methane production was maintained despite moderate water table decline of 20 cm in denser peats. Flooding led to accumulation of acetate and H2, promoted CH4 production and strengthened the co-occurrence of iron and sulfate reduction and methanogenesis. Mass balances during drying and flooding indicated that an important fraction of the electron flow must have been used for the generation and consumption of electron acceptors in the solid phase or other mechanisms. In contrast to flooding, dry-wet cycles negatively affect methane production on a seasonal scale but this impact might strongly depend on drying intensity and on the peat matrix, whose structure and physical properties influence moisture content.

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