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Domain decomposition methods to model heat exchanges between a well and a rock mass

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Figure 1: Axisymmetric diagram of the well-rock mass coupled problem - cavern (dotted line) will be considered in section 5
Figure 2: Both |G RR (k)| and |G DN (k)| (top) and 1 − |G DN (k)| (bottom) as a function of k ∈ [0, k max ] obtained with Q n = 30000 nm 3 .h −1 , ∆t = 6 h and with β ff = h, β rock = DtN [ rock (0), θ given by (16)
Figure 4: |G RR (k)| as a function of k ∈ [0, k max ] obtained with the Robin coefficients given by a numerical approximation of the min-max problem, by the choice β rock = DtN [ rock (0), β ff = h (denoted DtN0-h) and by the choice β rock = DtN [ rock (0)
Figure 5: Convergence rate (defined as the maximum of |G RR (k)| in k ∈ [0, k max ]) as a function of the normal flow rate Q n for the Robin coefficients obtained by a numerical approximation of the min-max problem (min-max), by the choice β rock = DtN [ r
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