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This post-failure behavior agrees with the real rock response better than the approach based on the linear elastic fracture mechanics. Interestingly, in the wetting path, the differences between the strain gauges are much less. These developments provide a promising starting point for further simulations that allow for high fidelity investigations of coupled processes in clayrock. So in all three cases the microfractures from the sample preperation were closing slowly, as a first step towards healing. For both quantities recorded at all four points, the order of convergence in space averages out to be 1.