The research to be conducted by Georgia Tech will advance the understanding of the behavior of
gas hydrates hosted in fine - grained sediments such as clay or silt, and will evaluate extraction methods relevant to the potential to produce gas from such sediments.
Not exact matches
The Arctic ocean floor
hosts vast amounts of methane trapped as
hydrates, which are ice - like, solid mixtures of
gas and water.These
hydrates are stable under high pressure and cold temperatures.
An abrupt warming of oceanic intermediate waters could have initiated the thermal destabilization of sediment -
hosted methane
gas hydrates and potentially triggered sediment slumps and slides.
In addition, deep fresh water lakes may
host gas hydrates as well, e.g. the fresh water Lake Baikal, Siberia.
Here in Oregon we are the somewhat unwitting
hosts of a great deal of methane
hydrate research by Oregon State University, some Texas university people (and backing by the good old Houston - based
gas industry), of deposits on and near the ocean floor on the Gorda Ridge just off our coast, which is a consequence of the subduction zone geomorphology of the area.