Citation: | Lin Lin, Jun Cao, Jin Qian, Jiu-jing Shang, Wei Zhang, Jin-gan Lu, Jin-qiang Liang, 2022. Velocity-porosity relationships in hydrate-bearing sediments measured from pressure cores, Shenhu Area, South China Sea, China Geology, 5, 267-275. doi: 10.31035/cg2022006 |
Evaluating velocity-porosity relationships of hydrate-bearing marine sediments is essential for characterizing natural gas hydrates below seafloor as either a potential energy resource or geohazards risks. Four sites had cored using pressure and non-pressure methods during the gas hydrates drilling project (GMGS4) expedition at Shenhu Area, north slope of the South China Sea. Sediments were cored above, below, and through the gas-hydrate-bearing zone guided with logging-while-drilling analysis results. Gamma density and P-wave velocity were measured in each pressure core before subsampling. Methane hydrates volumes in total 62 samples were calculated from the moles of excess methane collected during depressurization experiments. The concentration of methane hydrates ranged from 0.3% to 32.3%. The concentrations of pore fluid (25.44% to 68.82%) and sediments (23.63% to 54.28%) were calculated from the gamma density. The regression models of P-wave velocity were derived and compared with a global empirical equation derived from shallow, unconsolidated sediments data. The results were close to the global trend when the fluid concentration is larger than the critical porosity. It is concluded that the dominant factor of P-wave velocity in hydrate-bearing marine sediments is the presence of the hydrate. Methane hydrates can reduce the fluid concentration by discharging the pore fluid and occupying the original pore space of sediments after its formation.
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Location of pressure-core recovered sites at Shenhu Area during GMGS4.
Gamma density and P-wave velocity measured by PCATS for core 05A at Site 1, and LWD results from the same interval.
Methane phase diagrams of all four sites used to identify the possible status of pressure-core samples.
The concentration of methane hydrates, pore water, and sediments measured and calculated from pressure-core samples.
Cross plot of P-wave velocity and concentration of sediments (a), methane hydrates (b), and pore-fluid (c). Color represents the methane hydrates saturation of pore space.
Comparison between the predicted saturation of the methane hydrates and the measured data.