Methane hydrate formation and dissociation in a partially saturated sand

• Main Authors: Kneafsey, Timothy J., Tomutsa, Liviu, Taylor, Charles E., Gupta, Arvind, Moridis, George, Freifeld, Barry, Seol, Yongkoo
• Language: unknown
• Published: 2008
• Subjects: 03 NATURAL GAS; 58 GEOSCIENCES; COMPUTERIZED TOMOGRAPHY; DEPRESSURIZATION; DISSOCIATION; ECONOMICS; GAS HYDRATES; NATURAL GAS; SAND; SEDIMENTS; SILICA; SIMULATORS; STIMULATION; THERMODYNAMIC PROPERTIES; WATER; Methane hydrate
• Online Access: http://www.osti.gov/servlets/purl/841112; https://www.osti.gov/biblio/841112

To predict the behavior of hydrate-bearing sediments and the economic extractability of natural gas from reservoirs containing gas hydrates, we need reservoir simulators that properly represent the processes that occur, as well as accurate parameters. Several codes are available that represent some or all of the expected processes, and values for some parameters are available. Where values are unavailable, modelers have used estimation techniques to help with their predictions. Although some of these techniques are well respected, measurements are needed in many cases to verify the parameters. We have performed a series of experiments in a partially water saturated silica sand sample. The series included methane hydrate formation, and dissociation by both thermal stimulation and depressurization. The sample was 7.6 cm in diameter and 25 cm in length. In addition to measuring the system pressure and temperatures at four locations in the sample, we measured local density within the sample using x-ray computed tomography. Our goals in performing the experiment were to gather information for estimating thermal properties of the medium and to examine nonequilibrium processes.