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BP's annual report last year referred to a "comprehensive review of the subsurface gas release" having taken place and remedial work being carried out.
Shale gas release is entirely different, requiring the blasting open of rocks across vast distances at close quarters, making vertical wells useless.
This can be a delicate phase given the potential for an uncontrolled gas release that could lead to what is called a blowout.
The mechanisms responsible for fission gas release events are discussed.
At higher acoustic pressure, local gas release took place.
The fission gas release increased with the increase of burnup.
There seems to be no evolution in the rate of gas release.
The current strategy is based on the combination of Kirkendall effect, volume loss, and gas release.
Explosive gas release occurred in 1984 and 1986 at Lake Monoun and Lake Nyos (Cameroon), respectively.
If the gas release is disturbed, foam forms in the digesta.
The possible retardation of the gas release from the liquid proves to be a decisive factor.
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