Show simple item record

dc.contributor.authorTang, X. M.
dc.contributor.authorCheng, C. H.
dc.contributor.otherMassachusetts Institute of Technology. Earth Resources Laboratoryen_US
dc.date.accessioned2012-11-29T19:35:43Z
dc.date.available2012-11-29T19:35:43Z
dc.date.issued1988
dc.identifier.urihttp://hdl.handle.net/1721.1/75101
dc.description.abstractThe attenuation of Stoneley waves by a borehole fracture are closely related to fluid flow in the fracture. We consider the dynamic response of a viscous fluid in a horizontal fracture to the oscillating pressure excitation of Stoneley waves at the fracture opening. A dynamic model has been developed to describe the fluid motion in the fracture. This model relates both viscous shear effects at the fracture surface and the acoustic wave propagation in the fracture fluid. The dynamic conductivity is derived to characterize the fluid conduction in the fracture. This model is applied to study Stoneley wave attenuation across a borehole fracture, and is found to agree well with laboratory fracture modeling data.en_US
dc.description.sponsorshipMassachusetts Institute of Technology. Full Waveform Acoustic Logging Consortiumen_US
dc.description.sponsorshipUnited States. Dept. of Energy (Grant DE-FG02-86ER13636)en_US
dc.publisherMassachusetts Institute of Technology. Earth Resources Laboratoryen_US
dc.relation.ispartofseriesEarth Resources Laboratory Industry Consortia Annual Report;1988-06
dc.titleA Dynamic Model For Fluid Flow In A Borehole Fractureen_US
dc.typeTechnical Reporten_US
dc.contributor.mitauthorTang, X. M.
dc.contributor.mitauthorCheng, C. H.
dspace.orderedauthorsTang, X. M.; Cheng, C. H.en_US


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record