In this Chapter, I provided a theoretical tool for estimating the
amount of hydrate and gas from seismic interval velocity. I developed
rock-physics models that link the elastic wave velocity in high-porosity
marine sediment to density, porosity, effective pressure, mineralogy,
and water, gas and hydrate saturation. Three micromechanical models of
hydrate deposition in the pore space were examined: (A) hydrate is part of
the pore fluid, (B) hydrate becomes part of the solid frame, and (C) hydrate
cements grain contacts. Using the interval velocities obtained from the
stacking
velocity analysis described in Chapter 2, I calculated lateral maps of
hydrate and gas saturation. The calculations were based both on an averaging
approach and a trace-by-trace approach, resulting in an upper and lower
bound for the possible hydrate saturation. I find considerably large lateral
variations in hydrate saturation. Model A results in a maximum
hydrate saturation between 21% and 26% and model B between 15% and 20%.
In case of hydrate cementing the sediments, only 1% of hydrate is required in
the pore space to increase the velocity corresponding to that observed
in the seismic data. The estimated gas saturation is approximately 1%-2%.
Subsequently, I evaluated the robustness of these hydrate and gas saturation
estimates with respect to the velocity errors that were determined
in Chapter 2. The analysis
suggests that the maximum errors introduced into the hydrate saturation
estimates can be up to
14%, while the gas saturation shows
maximum uncertainties of
2%. The uncertainty estimates are upper
bounds on possible errors. The comparison with VSP data
(see Chapter 2, section 2.3.2)
and other seismic velocity
investigations Katzman et al. (1994); Korenaga et al. (1997); Wood et al. (1994) suggests
that the error in interval velocity is smaller than those upper bounds which
would shrink the uncertainties on the hydrate saturation.
Using additional velocity and porosity
information from well-logs 994 and 995, I evaluated the validity of the
proposed
technique and the used models. This investigation suggests that the technique
is quantitatively accurate.