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Model 2 - Hydrate is part of the solid

In this case, we assume that hydrate becomes part of the solid sediment frame. This has two effects: porosity reduction and change of the elastic frame moduli. The reduced porosity $\phi_r$ can be expressed as:  
 \begin{displaymath}
\phi_r \:=\: \phi\:(1-S_h),\end{displaymath} (7)

where Sh is the hydrate saturation of the pore space. The bulk and shear moduli of the solid phase are now a mixture of the sediment solid and the hydrate and can be calculated from the Hill average:

\begin{eqnarray}
&K& =\:{1\over2}(f_h\:K_h\:+\:(1-f_h)\:K_s\:+\:[f_h/K_h\:+\:(1-...
 ...er2}(f_h\:G_h\:+\:(1-f_h)\:G_s\:+\:[f_h/G_h\:+\:(1-f_h)/G_s]^{-1};\end{eqnarray}

where Ks and Gs are the bulk and shear moduli of the sediment without hydrate and fh is the volume fraction of hydrate in the solid phase. It can be calculated as follows:
\begin{displaymath}
f_h\:=\:{{\phi\:S_h}\over{1-\phi\:(1-S_h)}}\end{displaymath} (9)

The dry and saturated moduli can then be determined using equations 3, 4, 5 and 6.


previous up next print clean
Next: Model 3 - Hydrate Up: Rock-physics Theory Previous: Model 1 - Hydrate
Stanford Exploration Project
10/9/1997