Pore-Scale Controls on Permeability, Fluid Flow, and Methane Hydrate Distribution in Fine-Grained Sediments
Permeability in fine-grained sediments is governed by the surface area exposed to fluid flow and tortuosity of the pore network. I modify an existing technique of computing permeability from nuclear magnetic resonance (NMR) data to extend its applicability beyond reservoir-quality rocks to the fine-...
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| Format: | Others |
| Language: | English |
| Published: |
2012
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| Online Access: | http://hdl.handle.net/1911/64415 |