Page 160 - Analysis and Design of Energy Geostructures
P. 160

132   Analysis and Design of Energy Geostructures


                  ff. The energy conservation equation reads in this case:
                                               _ q cond  2 _q conv 2 _q rad  5 0

                                                                             2
                      where _q cond 52 λ  ΔT  is the conductive heat flux [W/m ], with λ the
                                       t slab
                      thermal conductivity of the medium [W/(m C)], ΔT the temperature


                      difference through the slab [ C] and t slab is the slab thickness [m];
                                                                             2
                         _ q conv  5 h c ðT s 2 T N Þ is the convective heat flux [W/m ], with h c the
                      convective heat transfer coefficient [W/(m 2   C)], T s the temperature of
                      the surface exposed to the fluid and T N the bulk temperature, both
                      expressed in [ C]; and

                                          4
                         _ q rad  5 Eσ SB ðT 2 T Þ is the radiative heat flux [W/m ], with E the
                                     4
                                                                              2
                                          sur
                                     s
                      emissivity of the body [ ], σ SB is the Stefan Boltzmann constant [W/
                            4
                      (m 2   C )] and T sur is the surrounding environment temperature [ C].

                 gg. In heat transfer analysis the ratio of the thermal conductivity λ [W/

                      (m C)] to the volumetric heat capacity ρc p [J/(m 3   C)] is termed the
                                              2
                      thermal diffusivity α d [m /s] and reads
                                                          λ
                                                    α d 5
                                                          ρc p
                 hh. Soils of large thermal diffusivity respond:
                       i. Quickly to variations in their thermal environment
                      ii. Slowly to variations in their thermal environment
                      iii. Irrespectively of the variations of their thermal environment
                      iv. Depending on the thermal conductivity
                                                                         2
                  ii. The thermal diffusivity is defined as α d 5 λ=ðρc p Þ [m /s].
                  Material   Thermal conductivity,  Volumetric heat     Thermal diffusivity, α d
                                                                                2
                                 λ [W/(m C)]         capacity, ρc p           [m /s]

                                                      [MJ/(m 3   C)]
                             Dry       Saturated  Dry      Saturated  Dry        Saturated
                  Clay       0.2 0.3   1.1 1.6   0.3 0.6   2.1 3.2    0.5 0.67   0.5 0.52
                  Silt       0.2 0.3   1.2 2.5   0.6 1.0   2.1 2.4    0.3 0.33   0.57 1.04
                  Sand       0.3 0.4   1.7 3.2   1.0 1.3   2.2 2.4    0.3 0.31   0.77 1.33
                  Gravel     0.3 0.4   1.8 3.3   1.2 1.6   2.2 2.4    0.25       0.82 1.375
                  Concrete        0.9 2.0              1.8 2.0                0.5 1
                  Water             0.57                4.186                  0.14
                  Air              0.025               0.0012                 20.83

                   jj. In general, the different values of thermal diffusivity for different materials
                      cannot be neglected: differences in thermal conductivity, density and spe-
                      cific heat are observed between the different materials and affect the heat
                      transfer.
   155   156   157   158   159   160   161   162   163   164   165