Page 475 - Enhanced Oil Recovery in Shale and Tight Reservoirs
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Air injection                                                439


              Table 13.8 Reservoir and thermal parameters used in the lab scale
              simulation model.
              Parameter                                        Value
              Reference depth (cm)                             0
              Porosity (dimensionless)                         0.41
              Horizontal permeability (mD)                     12,700
              kv/kh (dimensionless)                            1
              Oil saturation (dimensionless)                   0.882
              Reference pressure (kPa)                         4100
              Original reservoir temperature ( C)              100

              Rock volumetric heat capacity (J/(cm $ C))       2.35
                                           3
              Rock thermal conductivity (J/(cm$min$ C))        1

              Water thermal conductivity (J/(cm$min$ C))       0.36

              Oil thermal conductivity (J/(cm$min$ C))         0.077

              Gas thermal conductivity (J/(cm$min$ C))         0.083

              Temperature of injected gas ( C)                 100

              can history-match TG/DSC experiments with limited experimental time
              and heat loss. Using this history-matched model, slow reactions and
              adiabatic conditions can be simulated, and the feasibility of spontaneous
              ignition may be studied. A laboratory-scale model may be upscaled to a field
              model so that spontaneous ignition in field can be studied.
                 Huang and Sheng (2018) built a 1D laboratory-scale base model of grids
              of 36   1   1. The total grid block size was set at 5.08, 9.94, and 9.94 cm in
              the x, y, z directions, respectively. Air is injected at block (36 1 1) and the
              production end is at block (1 1 1). The main reservoir properties and thermal
              properties were taken from Belgrave et al. (1993), presented in Table 13.8.
              The kinetic parameters and the reaction scheme which contains three reac-
              tions with 11 components are from Huang and Sheng (2017c), as presented
              in Table 13.6. In the base laboratory-scale model, the over/underburden
              volumetric heat capacity of 2.350 J/(cm $ C) and thermal conductivity of
                                                3
              formation adjacent to the reservoir of 1.038 J/(cm$min$ C) are used.

                 Fig. 13.22 shows the temperature profiles at grids (6 1 1), (18 1 1), and
              (35 1 1) in the base case model and the adiabatic case (Huang and Sheng,
              2018). The temperature increase from the original reservoir temperature
              of 100 C is around 10 C in the base case and around 25 C in the adiabatic



              case due to LTO reactions. Such temperature increases are close to those
              reported by Jia et al. (2012a) and Abu-Khamsin et al. (2001). Such low
              temperature may not lead to spontaneous ignition. Note that in the adiabatic
              case, the temperatures near the production end (blocks (18 1 1) and (6 1 1))
              maintain at the peak temperatures because of no heat loss, while the
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