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The impulse imparted by charge exchange neutral impacts is at least six orders of magnitude smaller than that provided by the induced drag caused by gas expulsion.
Thermal models and dynamic models of stratospheric airships during ascent are developed, including solar radiation, infrared radiation, convection heat transfer and gas expulsion equation.
As the exact date of the eruption cannot be determined, the recent morphology of the pockmarks depicts the combined effect of gas expulsion and successive scouring of the initial defects in the seafloor.
These conditions facilitate oil and gas expulsion.
This accounts for 28% 42% % of total gas expulsion from source rocks.
This simulates the uplift and pressure drop process, and the gas desorption and gas expulsion processes were observed.
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This paper presents (a) a simple oil-expulsion model based on the principles of sedimentary compaction and the flow difference between oil and water, and (b) a simple gas-expulsion model via mass balance.
It is thus proposed that the pockmarks originated from a shallow source and result from relatively recent and short-duration gas or water expulsion events.
The presence of LSP increased the solubility of nitrogen in liquid titanium leading to gas recombination and expulsion on the surface.
These geochemical parameters decreased with increasing maturity, as a result of losing hydrogen and carbon during the oil and gas generation and expulsion.
Thermal evolution history shows that substantial gas generation and expulsion occurred in the source rocks of the two basins in the geological history.
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