Methane hydrate (referred to as MH hereafter) has come to be seen as a future energy source and as such research and development is being conducted in order to prepare for production of it. The MH reservoirs are located in the deep sea bed at over 1000m in sea depth. In Japan, the reservoirs are found in the Nankai Trough on the Pacific Ocean side of main island. MH mostly exists in the void space of the sand layers in the turbidite. In order to produce MH from the MH bearing layers, it is important to first make clear and understand the mechanical properties of the host sands of MH bearing sands in order to understand the MH bearing layer. A series of mechanical tests were performed on MH bearing sediments with various host sands by using temperature controlled high stress triaxial shear testing apparatus. A high pressure and low temperature plane strain testing apparatus was also developed for visualizing the deformation of methane hydrate bearing sand due to methane hydrate production. Using this testing apparatus, plane strain compression and methane hydrate dissociation by depressurization tests were performed with the measurement of localized deformation. On the basis of the experimental results, an elastoplastic constitutive model for methane hydrate-bearing sand was developed. The bonding effect due to the cementation by methane hydrate was introduced into the model. The simulation was performed on triaxial behaviour of methane-hydrate bearing sand under various pressure and temperature condition.
Read full abstract