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gassy
Pressure waves in a porous medium saturated with a gassy fluid
      
Experimental data on the evolution of pressure waves in a consolidated porous medium saturated with a gassy fluid are obtained.
      
Structure and dynamics of finite-amplitude pressure perturbations in a porous medium saturated with gassy fluid
      
Experimental data on the structure and dynamics of pressure perturbations of moderate intensity in a porous medium saturated with a gassy fluid are obtained and generalized on the basis of a theoretical analysis.
      
Steady temperature field associated with the flow of gassy oil in a porous medium
      
The steady thermal field associated with the flow of gassy oil through a porous medium is investigated with allowance for the Joule-Thomson and degassing effects.
      
Influence of Adsorption and Desorption of Gas Micronuclei on the Nature of the Flow of a Gassy Liquid through a Porous Medium
      
The problem of gassy liquid flow through a porous medium is considered theoretically.
      
Calculations of the Effective and Apparent Joule-Thomson Coefficients upon Gassy Liquid Filtration
      
The equations of a continuous medium upon filtration of a gassy liquid have been analyzed, and on this basis the equation of energy with effective coefficients has been obtained.
      
The examples show a close relationship between mining seismicity and gas outburst in high gassy coal mines.
      
Fourteen patients were labelled 'gassy' and no added information was provided following abdominal ultrasound.
      
The accuracy was 91.7 % when the 'gassy' patients were excluded and 81.3 % overall.
      
Fluid and gassy hydrocarbons rise through the sediment column and along faults causing the formation of gas hydrates, gassy sediments, mud volcanoes and mounds, chemosynthetic communities and authigenic carbonates, reefs, and hardgrounds.
      
Gassy sediment occurrence and properties: Northern Gulf of Mexico
      
Gassy sediment patches are between 250 and 500 m in horizontal size.
      
Often the gassy layers are within 100 m from the sea floor and are only a few meters thick.
      
Gassy sediment geoacoustic parameter values are not well constrained because of a lack of concurrent measurements of acoustic properties and sediment gas content.
      
For Gulf of Mexico gassy sediment, some reportedin situ values of sound speed are reduced by an order of magnitude below values for water saturated sediments.
      
Physical samples and observations within this unique seismic facies show gassy sediments, sometimes in hydrated form and, in places, as chemosynthetic communities.
      
 

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