Proceedings of the ... International Conference on Offshore Mechanics and Arctic Engineering, Volume 18, Part 5American Society of Mechanical Engineers, 1999 - Arctic regions |
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Page 48
... heat budget equation ( Nikolayeva & Shesterikov , 1970 ) : dT 2. = dz pk dh dt ( 5 ) where & is the heat conductivity of ice , k is specific heat of ice melting , p is ice density , T is ice temperature , h is ice thickness . The ...
... heat budget equation ( Nikolayeva & Shesterikov , 1970 ) : dT 2. = dz pk dh dt ( 5 ) where & is the heat conductivity of ice , k is specific heat of ice melting , p is ice density , T is ice temperature , h is ice thickness . The ...
Page 251
... heat of the phase transfer in the unit volume of rocks . The boundary conditions has the following view : ar W a ( T ... Heat capacity of the gas hydrate bearing formation was to be equal to 2400 kJ per mxK , and heat capacity of the ...
... heat of the phase transfer in the unit volume of rocks . The boundary conditions has the following view : ar W a ( T ... Heat capacity of the gas hydrate bearing formation was to be equal to 2400 kJ per mxK , and heat capacity of the ...
Page 258
... heat capacity and heat conductivity of the frozen soil , and the latent heat of the ice in the fill during phase change were included in the simulations of the temperature . In the present work , the time - dependent temperature ...
... heat capacity and heat conductivity of the frozen soil , and the latent heat of the ice in the fill during phase change were included in the simulations of the temperature . In the present work , the time - dependent temperature ...
Contents
OMAE99PA1135 | 19 |
OMAE99PA1141 | 39 |
PROPELLERICE INTERACTION | 53 |
Copyright | |
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