methanogenic bacteria

In the final stage, methanogenic bacteria form methane, which can then be used as a fuel source.

The activity of methanogenic bacteria is inhibited in acidic environments.

When sulphate availability is limited, methanogenic bacteria may then predominate.

Between 30 and 50% of people in western countries harbour methanogenic bacteria in their colons.

Methanogenic bacteria, as outlined earlier, operate in a strictly defined pH range.

Methanogenic bacteria tend to predominate in a sulphate depleted environment, however.

Methanogenic bacteria require stable pH and temperature to optimise their performance.

Emissions related to methanogenic bacteria in the tailings ponds continue to be studied by the operators.

Methane gas is produced in the rumen by methanogenic bacteria as a metabolic end product.

This post-depositional isotopic enrichment is attributed to the metabolism of methanogenic bacteria.

We conclude that bromoethanesulfonate is a specific and effective inhibitor of methanogenic bacteria, even when used at this high concentration.

Methanogenic bacteria counts and breath CH 4 recovered after sulphate addition was stopped.

Viable counts of methanogenic bacteria were enumerated using the Hungate roll tube technique.

Producing rice in paddies is harmful for the environment due to the release of methane by methanogenic bacteria.

In an anaerobic system, the majority of the chemical energy contained within the starting material is released by methanogenic bacteria as methane.

Carbon dioxide, for example, is reduced to methane (CH) by methanogenic bacteria.

The hydrogen is used by anaerobic methanogenic bacteria to dechlorinate the solvents and to produce methane.

Methanogenic bacteria displayed a gram-positive cell wall that varied considerably among different cell types.

No strict anaerobic cellulolytic, homoacetogenic, or methanogenic bacteria were enriched from the gut.

A methanogenic bacterium, strain FR, was isolated from this acclimated consortium.

Ether polar lipids of methanogenic bacteria: structures, comparative aspects, and biosyntheses.

These results further indicate that the formation of the siderite concretions is not associated with the activity of methanogenic bacteria.

The formation of CH4 is uncommon in Canada because methanogenic bacteria grow very slowly below 20oC.

Methanoplanus petrolearius sp. nov., a novel methanogenic bacterium from an oil-producing well.

The predominant bacteria become anaerobes, principally sulfate reducers and methanogenic bacteria.