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Methane hydrate as a “new energy”                                 249

           and the membrane was installed as shown in Fig. 7.8C. Because the specimens in the
           tests were subjected to low temperature and high pressure, rubber membranes conven-
           tionally used in triaxial tests were avoided; instead, silicon-type membranes were used
           because of their flexibility under low temperature/high pressure conditions and butyl
           rubber was used in long-term tests, such as MH dissociation because silicone is to
           some degree permeable to methane gas. The inner cell set up is shown in Fig. 7.8D.



           7.3.3 Generation of MH and experimental procedure

           After forming the specimen, it was subjected to a series of processes under specific
           temperatures and pressures, as depicted in Fig. 7.10. First of all, the frozen specimen
           (a) was thawed to room temperature inside the triaxial cell (b). Then, the back pressure
           was gradually increased to 4 MPa while methane was injected into the specimen
           (c) thus filling the pores of the specimen with methane. At this time, the gas pressure
           was increased over a period of time so that the specimen’s moisture content would not
           become nonuniform as a result of the pressurized injection. Next, the temperature in
           the triaxial cell was lowered to 1°C where the MH was stable, and the specimen envi-
           ronment was kept under constant temperature and pressure conditions for 24 h. By
           keeping the gas pressure constant in the connection between the specimen and the
           syringe pump and by observing the amount of gas flowing at various times, the trans-
           formation of water within the pores into hydrate was judged to be complete if there
           was no marked change in the amount of gas, as indicated in the Fig. 7.11. Note that the
           plots in the figure show some irregularities because in inducing the gas to flow into the





























           Fig. 7.10 State paths for pressure and temperature to produce MH-bearing sand [18].
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