Fluid pressure diffusion effects on the seismic reflectivity of a single fracture.

When seismic waves travel through a fluid-saturated porous medium containing a fracture, fluid pressure gradients are induced between the compliant fracture and the stiffer embedding background. The resulting equilibration through fluid pressure diffusion (FPD) produces a frequency dependence of the stiffening effect of the fluid saturating the fracture. As the reflectivity of a fracture is mainly controlled by the stiffness contrast with respect to the background, these frequency-dependent effects are expected to affect the fracture reflectivity.

Frequency-dependent effective hydraulic conductivity of strongly heterogeneous media.

The determination of the transport properties of heterogeneous porous rocks, such as an effective hydraulic conductivity, arises in a range of geoscience problems, from groundwater flow analysis to hydrocarbon reservoir modeling. In the presence of formation-scale heterogeneities, nonstationary flows, induced by pumping tests or propagating elastic waves, entail localized pressure diffusion processes with a characteristic frequency depending on the pressure diffusivity and size of the heterogeneity. Then, on a macroscale, a homogeneous equivalent medium exists, which has a frequency-dependent effective conductivity.

Developmental studies of the lethal gene Bld in the mouse. I. Post-implantation development of the lethal homozygote.

In matings of Bld/+ x Bld/+ mice a characteristic type of abnormal embryo is found on days 6 and 7 after impregnation which dies at 8 days and accounts for about 25% of all living embryos. These embryos are regarded as the fethal Bld/Bld homozygotes. Before 6 days the embryos appear slightly retarded.