Mineralogical composition and physical properties of the tight sandstone specimen determined by XRD analysis.
| Sample diameter, d (mm) | 38 |
| Sample length, L (mm) | 70 |
| Sample's porosity, |$\phi $| (per cent) | 8.2 |
| Sample's helium permeability, |$\kappa $| (|$\times {10^{ - 15}}$| |${\mathrm{ m}^2}$|) | 0.052 |
| Bulk modulus of solid grains, |${K_{\rm{g}}}$| (GPa) | 38 |
| Density of solid grains, |$\rho $| (kg m−3) | 2640 |
| Quartz (per cent) | 76.3 |
| Feldspar (per cent) | 7.6 |
| Calcite (per cent) | 5.5 |
| Clay (per cent) | 3.4 |
| Error on measured low-frequency K and |$\mu $| (per cent) | |$\pm 2.6$| |
| Sample diameter, d (mm) | 38 |
| Sample length, L (mm) | 70 |
| Sample's porosity, |$\phi $| (per cent) | 8.2 |
| Sample's helium permeability, |$\kappa $| (|$\times {10^{ - 15}}$| |${\mathrm{ m}^2}$|) | 0.052 |
| Bulk modulus of solid grains, |${K_{\rm{g}}}$| (GPa) | 38 |
| Density of solid grains, |$\rho $| (kg m−3) | 2640 |
| Quartz (per cent) | 76.3 |
| Feldspar (per cent) | 7.6 |
| Calcite (per cent) | 5.5 |
| Clay (per cent) | 3.4 |
| Error on measured low-frequency K and |$\mu $| (per cent) | |$\pm 2.6$| |
Mineralogical composition and physical properties of the tight sandstone specimen determined by XRD analysis.
| Sample diameter, d (mm) | 38 |
| Sample length, L (mm) | 70 |
| Sample's porosity, |$\phi $| (per cent) | 8.2 |
| Sample's helium permeability, |$\kappa $| (|$\times {10^{ - 15}}$| |${\mathrm{ m}^2}$|) | 0.052 |
| Bulk modulus of solid grains, |${K_{\rm{g}}}$| (GPa) | 38 |
| Density of solid grains, |$\rho $| (kg m−3) | 2640 |
| Quartz (per cent) | 76.3 |
| Feldspar (per cent) | 7.6 |
| Calcite (per cent) | 5.5 |
| Clay (per cent) | 3.4 |
| Error on measured low-frequency K and |$\mu $| (per cent) | |$\pm 2.6$| |
| Sample diameter, d (mm) | 38 |
| Sample length, L (mm) | 70 |
| Sample's porosity, |$\phi $| (per cent) | 8.2 |
| Sample's helium permeability, |$\kappa $| (|$\times {10^{ - 15}}$| |${\mathrm{ m}^2}$|) | 0.052 |
| Bulk modulus of solid grains, |${K_{\rm{g}}}$| (GPa) | 38 |
| Density of solid grains, |$\rho $| (kg m−3) | 2640 |
| Quartz (per cent) | 76.3 |
| Feldspar (per cent) | 7.6 |
| Calcite (per cent) | 5.5 |
| Clay (per cent) | 3.4 |
| Error on measured low-frequency K and |$\mu $| (per cent) | |$\pm 2.6$| |
This PDF is available to Subscribers Only
View Article Abstract & Purchase OptionsFor full access to this pdf, sign in to an existing account, or purchase an annual subscription.
