Niculae Mandache

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with C−1 ≤ ρ ≤ C, C > 1. When n = 3 it describes the evolution of temperature u in a medium where the thermal conductivity is constant and the heat capacity is ρ. It also applies to diffusion in porous rocks, where ρ is the specific storage, if the hydraulic conductivity is constant. We consider the problem of the determination of ρ in Ω from boundary(More)
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