Permeability and porosity of hydrate-bearing sediments in the northern Gulf of Mexico

Daigle, Hugh; Cook, Ann; Malinverno, Alberto

doi:10.1016/j.marpetgeo.2015.10.004

Title: Permeability and porosity of hydrate-bearing sediments in the northern Gulf of Mexico

Journal Article · Wed Oct 14 00:00:00 EDT 2015 · Marine and Petroleum Geology

DOI:https://doi.org/10.1016/j.marpetgeo.2015.10.004· OSTI ID:1223537

Daigle, Hugh ^[1]; Cook, Ann ^[2]; Malinverno, Alberto ^[3]

Univ. of Texas at Austin, Austin, TX (United States)
The Ohio State Univ., Columbus, OH (United States)
Lamont-Doherty Earth Observatory of Columbia Univ., Palisades, NY (United States)

Hydrate-bearing sands are being actively explored because they contain the highest concentrations of hydrate and are the most economically recoverable hydrate resource. However, relatively little is known about the mechanisms or timescales of hydrate formation, which are related to methane supply, fluid flux, and host sediment properties such as permeability. We used logging-while-drilling data from locations in the northern Gulf of Mexico to develop an effective medium theory-based model for predicting permeability based on clay-sized sediment fraction. The model considers permeability varying between sand and clay endpoint permeabilities that are defined from laboratory data. We verified the model using permeability measurements on core samples from three boreholes, and then used the model to predict permeability in two wells drilled in Walker Ridge Block 313 during the Gulf of Mexico Gas Hydrate Joint Industry Project Leg II expedition in 2009. We found that the cleanest sands (clay-sized fraction <0.05) had intrinsic (hydrate-free) permeability contrasts of 5-6 orders of magnitude with the surrounding clays, which is sufficient to provide focused hydrate formation due to advection of methane from a deep source or diffusion of microbial methane from nearby clay layers. In sands where the clay-sized fraction exceeds 0.05, the permeability reduces significantly and focused flow is less pronounced. In these cases, diffusion of dissolved microbial methane is most likely the preferred mode of methane supply for hydrate formation. In conclusion, our results provide important constraints on methane supply mechanisms in the Walker Ridge area and have global implications for evaluating rates of methane migration and hydrate formation in hydrate-bearing sands.

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Research Organization:: Univ. of Texas, Austin, TX (United States)

Sponsoring Organization:: USDOE Office of Fossil Energy (FE)

Grant/Contract Number:: FE0013919

OSTI ID:: 1223537

Alternate ID(s):: OSTI ID: 1249817

Journal Information:: Marine and Petroleum Geology, Vol. 68, Issue PA; ISSN 0264-8172

Publisher:: ElsevierCopyright Statement

Country of Publication:: United States

Language:: English

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Cited by: 32 works

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