title: Diffusion-relaxation distribution functions of sedimentary rocks in different saturation states.
abstract: We present diffusion-relaxation distribution functions measured on four rock cores that were prepared in a succession of different saturation states of brine and crude oil. The measurements were performed in a static gradient field at a Larmor frequency of 1.76 MHz. The diffusion-relaxation distribution functions clearly separate the contributions from the two fluid phases. The results can be used to identify the wetting and non-wetting phase, to infer fluid properties of the phases, and to obtain additional information on the geometrical arrangement of the phases. We also observe effects due to restricted diffusion and susceptibility induced internal gradients.
authors.affiliation: Schlumberger-Doll Research, Ridgefield, CT, USA. hurliman@slb.com
authors.forename: M D
authors.initials: MD
authors.lastname: Hürlimann
authors.forename: M
authors.initials: M
authors.lastname: Flaum
authors.forename: L
authors.initials: L
authors.lastname: Venkataramanan
authors.forename: C
authors.initials: C
authors.lastname: Flaum
authors.forename: R
authors.initials: R
authors.lastname: Freedman
authors.forename: G J
authors.initials: GJ
authors.lastname: Hirasaki
mesh_terms: D004058:Diffusion; D019015:Geologic Sediments; D009682:Magnetic Resonance Spectroscopy / Q000379:methods*; D016062:Porosity