All Stories

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