SPE Journal
Volume 16,
Number 1,
March 2011,
pp. 78-94
Summary
Methane hydrate was formed in two moist sands and a sand/silt mixture under
a confining stress in an X-ray-transparent pressure vessel. Three initial water
saturations were used to form three different methane-hydrate saturations in
each medium. X-ray computed tomography (CT) was used to observe
location-specific density changes caused by hydrate formation and flowing
water. Gas-permeability measurements in each test for the dry, moist, frozen,
and hydrate-bearing states are presented. As expected, the effective
permeabilities (intrinsic permeability of the medium multiplied by the relative
permeability) of the moist sands decreased with increasing moisture content. In
a series of tests on a single sample, the effective permeability typically
decreased as the pore space became more filled, in the order of dry, moist,
frozen, and hydrate-bearing. In each test, water was flowed through the
hydrate-bearing medium and we observed the location-specific changes in water
saturation using CT scanning. We compared our data to a number of models, and
our relative permeability data compare most favorably with models in which
hydrate occupies the pore bodies rather than the pore throats. Inverse modeling
(using the data collected from the tests) will be performed to extend the
relative permeability measurements.
© 2010. Society of Petroleum Engineers
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History
- Original manuscript received:
15 February 2008
- Meeting paper published:
6 May 2008
- Revised manuscript received:
6 April 2010
- Manuscript approved:
16 April 2010
- Published online:
7 October 2010
- Version of record:
15 March 2011