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Related Concept Videos

Microbes and Methanogenesis01:26

Microbes and Methanogenesis

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Methanogenesis is a critical microbial process in anaerobic ecosystems responsible for the biological production of methane, a potent greenhouse gas and valuable biofuel. This metabolic pathway is primarily facilitated by methanogenic archaea, which thrive in anoxic environments such as wetlands, sediments, and animal gastrointestinal tracts. The absence of oxygen in these habitats prevents aerobic respiration, thereby favoring alternative biochemical pathways for organic matter degradation.In...
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Radical Substitution: Halogenation of Alkanes and Alkyl Substituents01:27

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In the presence of heat or light, alkanes react with molecular halogens to form alkyl halides by a substitution reaction called radical halogenation. This reaction has three steps: initiation, propagation, and termination, as seen in the radical chlorination of methane to produce methyl chloride.
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Metabolism of Chemolithotrophs01:15

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Chemolithotrophs are microorganisms that obtain energy by oxidizing inorganic molecules such as hydrogen gas (H₂), ammonia (NH₃), reduced sulfur compounds (H₂S, S²⁻), and ferrous iron (Fe²⁺). Unlike heterotrophic organisms that rely on organic carbon, chemolithotrophs transfer electrons from these inorganic donors to the electron transport chain (ETC), generating a proton motive force (PMF) that drives ATP synthesis through oxidative phosphorylation.
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Radical Substitution: Allylic Chlorination01:31

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Typically, when alkenes react with halogens at low temperatures, an addition reaction occurs. However, upon increasing the temperature or under reaction conditions that form radicals, providing a low but steady concentration of halogen radicals, allylic substitution reaction is favored. This is because allylic hydrogens are very reactive as the formed intermediate is resonance stabilized. For example, when propene is treated with chlorine in the gas phase at 400 °C, it undergoes allylic...
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Radical Halogenation: Thermodynamics01:34

Radical Halogenation: Thermodynamics

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The thermodynamic favorability of a reaction is determined by the change in Gibbs free energy (ΔG). ΔG has two components- enthalpy (ΔH) and entropy (ΔS). The entropy component is negligible for alkane halogenation because the number of reactants and product molecules are equal. In this case, the ΔG is governed only by the enthalpy component. The most crucial factor that determines ΔH is the strength of the bonds. ΔH can be determined by comparing the energy...
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Radical Anti-Markovnikov Addition to Alkenes: Mechanism01:17

Radical Anti-Markovnikov Addition to Alkenes: Mechanism

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The reaction of hydrogen bromide with alkenes in the presence of hydroperoxides or peroxides proceeds via anti-Markovnikov addition. The radical chain reaction comprises initiation, propagation, and termination steps.
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Visualizing Methane-Cycling Microbial Dynamics in Coastal Wetlands
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Methane oxidation linked to chlorite dismutation.

Laurence G Miller1, Shaun M Baesman1, Charlotte I Carlström2

  • 1United States Geological Survey Menlo Park, CA, USA.

Frontiers in Microbiology
|July 3, 2014
PubMed
Summary
This summary is machine-generated.

Methane oxidation coupled to oxygen from chlorite dismutation was observed. Perchlorate and chlorate reduction did not yield oxygen for methane oxidation, suggesting limited oxygen release from these processes.

Keywords:
chloratechloritemethaneoxidationperchlorate

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Area of Science:

  • Environmental microbiology
  • Biogeochemical cycles
  • Anaerobic oxidation

Background:

  • Methane (CH4) oxidation is crucial for mitigating greenhouse gas emissions.
  • Oxygen is typically required for aerobic methane oxidation.
  • Alternative oxygen sources for anaerobic methane oxidation are being investigated.

Purpose of the Study:

  • To investigate if methane oxidation can be coupled with oxygen from the dissimilatory reduction of perchlorate (ClO(-) 4), chlorate (ClO(-) 3), or chlorite (ClO(-) 2) dismutation.
  • To determine the potential of different oxyanions as oxygen donors for methane oxidation in anaerobic environments.

Main Methods:

  • Incubation of anaerobic mixed cultures and soil slurries with different oxyanions (ClO(-) 4, ClO(-) 3, ClO(-) 2).
  • Monitoring of chloride ion accumulation as an indicator of oxyanion reduction.
  • Quantification of methane (CH4) consumption using gas chromatography.
  • Experiments with physically separated cultures and soil to assess oxygen transfer.

Main Results:

  • Dissimilatory reduction of ClO(-) 4 and ClO(-) 3 was inferred from chloride accumulation but did not stimulate methane oxidation.
  • Chlorite (ClO(-) 2) amendment effectively stimulated methane oxidation in both pure cultures and soil enrichments.
  • Methane removal was observed when Dechloromonas agitata CKB was co-incubated with methanotrophs and ClO(-) 2, requiring physical separation for oxygen partitioning.

Conclusions:

  • Chlorite (ClO(-) 2) dismutation can provide oxygen for methane oxidation in anaerobic environments.
  • Perchlorate (ClO(-) 4) and chlorate (ClO(-) 3) reduction do not appear to supply sufficient oxygen for coupled methane oxidation.
  • The enzymatic release of oxygen during perchlorate reduction is likely negligible or unavailable to aerobic methanotrophs.