All Stories

  1. Stoneley wave attenuation and dispersion and the dynamic permeability correction
  2. Elastic potential energy in linear poroelasticity
  3. Compensating elastic transmission losses for P-wave attenuation estimation from sonic logs
  4. Drained pore modulus and Biot coefficient from pore-scale digital rock simulations
  5. Seismic modeling in porous media using the viscosity-extended Biot framework
  6. Shared advances in exploration and fundamental geophysics – Introduction
  7. Deciphering fractured rock properties from seismic wavefields — Introduction
  8. Modeling Forced Imbibition Processes and the Associated Seismic Attenuation in Heterogeneous Porous Rocks
  9. Macroscopic Deformation Moduli of Porous Rocks: Insights from Digital Image Pore-Scale Simulations
  10. On Elastic Potential Energy for Deformable Porous Media
  11. Slow P -Wave Attenuation Due to Conversion Scattering into Slow S -Wave in the Biot High-Frequency Range
  12. Sonic attenuation of shale
  13. Fracture connectivity can reduce the velocity anisotropy of seismic waves
  14. Numerical upscaling in 2-D heterogeneous poroelastic rocks: Anisotropic attenuation and dispersion of seismic waves
  15. An energy-based approach to estimate seismic attenuation due to wave-induced fluid flow in heterogeneous poroelastic media
  16. Biot coefficient is distinct from effective pressure coefficient
  17. Introduction to the special issue ‘Advances in Rock Physics’
  18. Numerical upscaling of frequency-dependent P- and S-wave moduli in fractured porous media
  19. Saturation scale effect on time-lapse seismic signatures
  20. Generalized poroelasticity framework for micro-inhomogeneous rocks
  21. Velocity-saturation relation in partially saturated rocks: Modelling the effect of injection rate changes
  22. Representative elementary volumes for evaluating effective seismic properties of heterogeneous poroelastic media
  23. Energy dissipation of P- and S-waves in fluid-saturated rocks: An overview focusing on hydraulically connected fractures
  24. Including poroelastic effects in the linear slip theory
  25. Comparison ofP-wave attenuation models of wave-induced flow
  26. Solid-phase bulk modulus and microinhomogeneity parameter from quasistatic compression experiments
  27. Seismic attenuation: effects of interfacial impedance on wave-induced pressure diffusion
  28. Pore pressure stress coupling in 3D and consequences for reservoir stress states and fault reactivation
  29. Quantifying the effect of capillarity on attenuation and dispersion in patchy-saturated rocks
  30. Wave attenuation in partially saturated porous rocks — New observations and interpretations across scales
  31. Forced imbibition into a limestone: measuring P-wave velocity and water saturation dependence on injection rate
  32. Seismoacoustic signatures of fracture connectivity
  33. Seismic wave attenuation and dispersion due to wave-induced fluid flow in rocks with strong permeability fluctuations
  34. Frequency-dependent effective hydraulic conductivity of strongly heterogeneous media
  35. Effect of fracture fill on seismic attenuation and dispersion in fractured porous rocks
  36. Do seismic waves sense fracture connectivity?
  37. Porosity perturbations and poroelastic compressibilities
  38. In-situ stresses in the Southern Perth Basin at the GSWA Harvey-1 well site
  39. Constraints on seismic reflections and mode conversions at bottom simulating reflectors associated with gas hydrates
  40. Computational elastic up-scaling of sandstone on the basis of X-ray micro-tomographic images
  41. Stochastic theory of dynamic permeability in poroelastic media
  42. Time-lapse sonic logs reveal patchy CO2saturation in-situ
  43. Anisotropic P-SV-wave dispersion and attenuation due to inter-layer flow in thinly layered porous rocks
  44. Fast compressional wave attenuation and dispersion due to conversion scattering into slow shear waves in randomly heterogeneous porous media
  45. Porous medium acoustics of wave-induced vorticity diffusion
  46. Poroelastic contribution to the reservoir stress path
  47. Seismic wave attenuation and dispersion resulting from wave-induced flow in porous rocks — A review
  48. Anisotropic dispersion and attenuation due to wave-induced fluid flow: Quasi-static finite element modeling in poroelastic solids
  49. A model for strong attenuation and dispersion of seismic P-waves in a partially saturated fractured reservoir
  50. Fluid-induced microseismicity in pre-stressed rock masses
  51. Microseismic signatures of non-linear pore-fluid pressure diffusion
  52. Finite-difference modeling of wave propagation and diffusion in poroelastic media
  53. Green's functions and radiation patterns in poroelastic solids revisited
  54. Statistical characterization of gas-patch distributions in partially saturated rocks
  55. P-wave dispersion and attenuation in fractured and porous reservoirs - poroelasticity approach
  56. Simulating three-dimensional seismograms in 2.5-dimensional structures by combining two-dimensional finite difference modelling and ray tracing
  57. Velocity-saturation relation for partially saturated rocks with fractal pore fluid distribution
  58. Attenuation of Seismic Waves Due to Wave‐Induced Flow and Scattering in Randomly Heterogeneous Poroelastic Continua
  59. Direct laboratory observation of velocity‐saturation relation transition during rocks saturation
  60. Characteristic frequencies of seismic attenuation due to wave-induced fluid flow in fractured porous media
  61. Comparative review of theoretical models for elastic wave attenuation and dispersion in partially saturated rocks
  62. Spatiotemporal pore pressure evolution due to fluid-mass point sources in dynamic poroelasticity
  63. Effective hydraulic conductivity and diffusivity of randomly heterogeneous porous solids with compressible constituents
  64. Seismic attenuation due to wave-induced flow: WhyQin random structures scales differently
  65. Wave-induced fluid flow in random porous media: Attenuation and dispersion of elastic waves
  66. A first-order statistical smoothing approximation for the coherent wave field in random porous media
  67. Estimating statistical parameters of an elastic random medium from traveltime fluctuations of refracted waves
  68. One‐dimensional random patchy saturation model for velocity and attenuation in porous rocks
  69. Amplitude corrections for randomly distributed heterogeneities above a target reflector
  70. True amplitude migration in the presence of a statistically heterogeneous overburden
  71. Most probable seismic pulses in single realizations of two- and three-dimensional random media