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242                                               Managing Global Warming

         reserved energy which can alleviate the energy crisis to certain extent [8,9]. Therefore,
         how to exploit MH safely and efficiently has become a worldwide focus.


         7.2   Production methods

         The exploitation methods mainly include the chemical and physical methods. For
         chemical methods such as chemical injection method, the diffusion of chemicals is
         inhibited due to the low permeability of methane hydrate-bearing sand (MHBS)
         [10], leading to low gas production rate. Moreover, the costs of chemical method
         are high and not suitable for large-scale exploitation. These two defects make
         researchers seek other more efficient methods. Physical exploitation methods, which
         include thermal recovery and depressurization methods, have the advantage of low
         cost and high gas productivity [11]. The aim of these two methods is to change the
         environment of MH by either increasing the temperature or reducing the confining
         pressure until the temperature-confining pressure condition is such that MH dissoci-
         ates into methane gas and water, as illustrated in Fig. 7.5 [12,13].


         7.2.1 Thermal recovery method
         In this method, a well is drilled into the methane hydrate-bearing layer, and the meth-
         ane hydrate is dissociated by heating, using a fluid (hot water or steam) heated at the
         surface in a boiler or similar device and circulated down through the well, as illus-
         trated in Fig. 7.6. This causes methane hydrate to dissociate and generate methane gas.

         Fig. 7.5 The base condition to  0
         form MH.                                                   Seawater
                                      200


                                      400        Phase
                                                 boundary
                                      600     Temperature
                                    Depth D (m)  800




                                      1000

                                                                    Seabed
                                      1200
                                              Formation area of
                                              methane hydrate
                                      1400
                                                           BSR
                                                    (Bottom simulating reflector)
                                      1600
                                        −30   −20  −10     0    10    20   30
                                                    Temperature T (°C)
   277   278   279   280   281   282   283   284   285   286   287