Gas
hydrates are large energy resources with estimated global reserves
of approximately 500–10 000 Gt of carbon, which can
be extracted from underground reservoirs. In addition, such reservoirs
can potentially catastrophically release greenhouse gases (such as
methane or carbon dioxide). Classically, rock wettability is one of
the key factors in predicting fluid flow behavior, fluid distribution,
reserves, and productivities. However, the effect of wettability on
the electric resistivity of hydrate formations is poorly understood.
Thus, to evaluate the influence of rock wettability on the electrical
resistivity (note that resistivity logging is a key well logging tool)
of hydrate-bearing sandstone, nuclear magnetic resonance experiments
were conducted. Clearly, the effective porosity and liquid saturation
increased with increasing temperature, due to hydrate dissociation.
Furthermore, the resistivity index and rock resistivity (R
t) increased with increasing hydrate saturation, and the
formation factor demonstrated a positive correlation with hydrate
saturation, though the formation factor for oil-wet (OW) sandstone
was higher than that for water-wet (WW) sandstone. This work will
thus significantly improve the fundamental understanding of the petrophysical
properties of gas hydrate reservoirs so that energy production can
be optimized, geohazards can be avoided, and the hydrate gun hypothesis
can be better assessed.