125 results on '"Müller, Tobias M."'
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2. Rock Physics Modeling and Seismic AVAZ Responses of Fractured Reservoirs with Different Azimuths
3. Rock-Physics Template Based on Differential Diagenesis for the Characterization of Shale Gas Reservoirs
4. A patchy-saturated rock physics model for tight sandstone based on microscopic pore structures
5. Period‐ and Pressure‐Dependent Hydraulic Properties of a Fractured Granite Inferred From Periodic Pumping Tests
6. Shear wave transmissivity and wave-induced vorticity diffusion through conversion scattering to slow-shear diffusion wave
7. Decoupled acoustoelasticity equations and stable FD modeling for wave propagation in prestressed media
8. Energy dissipation of P- and S-waves in fluid-saturated rocks: An overview focusing on hydraulically connected fractures
9. Wettability-dependent wave velocities and attenuation in granular porous media
10. Acoustoelastic FD Simulation of Elastic Wave Propagation in Prestressed Media
11. Brittle mineral prediction based on rock-physics modelling for tight oil reservoir rocks
12. Acoustics of Partially Saturated Rocks: Theory and Experiments
13. Introduction
14. List of Contributors
15. Correct description of S-wave propagation across material discontinuities in poroelasticity
16. Comparison of P-wave attenuation models of wave-induced flow
17. Seismic attenuation and velocity dispersion in fractured rocks: The role played by fracture contact areas
18. Wettability-dependent Wave Velocities and Attenuation in Granular Porous Media
19. Pore Size Distribution Controls Dynamic Permeability
20. Negative Unjacketed Pore Modulus in Limestones? Critical Examination of a Peculiar Laboratory Observation
21. Path dispersion of elastic waves in granular matter
22. Temperature Effect on the Velocity‐Porosity Relationship in Rocks
23. Drained pore modulus and Biot coefficient from pore-scale digital rock simulations
24. Wettability dependent P-wave scattering and velocity saturation relation in granular medium
25. Pore Size Distribution Controls Dynamic Permeability
26. Drained‐to‐undrained transition of bulk modulus in fluid‐saturated porous rock induced by dead volume variation
27. Permeability inversion using induced microseismicity: A case study for the Longmaxi shale gas reservoir
28. Diffusion in deformable porous media: Incompressible flow limit and implications for permeability estimation from microseismicity
29. Wettability effect on wave propagation in saturated porous medium
30. Effect of porosity gradient on the permeability tensor
31. Elastic waves in porous media saturated with non-wetting fluid
32. Stoneley wave attenuation and dispersion and the dynamic permeability correction
33. Elastic potential energy in linear poroelasticity
34. Compensating elastic transmission losses for P‐wave attenuation estimation from sonic logs
35. Effect of porosity gradient on the permeability tensor.
36. Modeling Forced Imbibition Processes and the Associated Seismic Attenuation in Heterogeneous Porous Rocks
37. Robustness of Q estimates from borehole data: Spectral ratio versus statistical averaging
38. Deciphering fractured rock properties from seismic wavefields — Introduction
39. Modeling Forced Imbibition Processes and the Associated Seismic Attenuation in Heterogeneous Porous Rocks
40. Seismic attenuation: effects of interfacial impedance on wave-induced pressure diffusion
41. Chapter 3 - Acoustics of Partially Saturated Rocks: Theory and Experiments
42. Chapter 1 - Introduction
43. Macroscopic Deformation Moduli of Porous Rocks: Insights from Digital Image Pore-Scale Simulations
44. On Elastic Potential Energy for Deformable Porous Media
45. Slow P -Wave Attenuation Due to Conversion Scattering into Slow S -Wave in the Biot High-Frequency Range
46. Sonic QP/QS ratio as diagnostic tool for shale gas saturation
47. Fracture connectivity can reduce the velocity anisotropy of seismic waves
48. Numerical upscaling in 2‐D heterogeneous poroelastic rocks: Anisotropic attenuation and dispersion of seismic waves
49. An energy-based approach to estimate seismic attenuation due to wave-induced fluid flow in heterogeneous poroelastic media
50. Biot coefficient is distinct from effective pressure coefficient
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