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Sequential Methods for Coupled Geomechanics and Multiphase Flow

Sequential Methods for Coupled Geomechanics and Multiphase Flow

Sequential Methods for Coupled Geomechanics and Multiphase Flow

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Chapter 4<br />

Convergence of the Drained <strong>and</strong><br />

Undrained Splits<br />

4.1 Error Estimation<br />

<strong>Sequential</strong> implicit solution schemes <strong>for</strong> coupled geomechanics <strong>and</strong> flow entail solutions of<br />

two implicit problems, one <strong>for</strong> mechanics <strong>and</strong> one <strong>for</strong> flow, in sequence. In such schemes, one<br />

often per<strong>for</strong>ms a single pass or a few iterations, <strong>and</strong> it is crucial to assess the convergence<br />

behavior of the sequential coupling strategy. In this Chapter, two sequential schemes are<br />

investigated: the drained <strong>and</strong> undrained splits. The backward Euler time discretization is<br />

used, <strong>and</strong> the linear coupled problem is considered <strong>for</strong> simplicity. We employ matrix <strong>and</strong><br />

spectral methods to analyze the behavior of the error as a function of iteration.<br />

4.1.1 Error estimation of the drained split by matrix algebra<br />

For a sequential solution strategy, we can write<br />

<br />

<br />

e n+1,niter<br />

ts<br />

<br />

<br />

≤ x n+1<br />

<br />

<br />

t − xn+1<br />

f +<br />

<br />

<br />

= O(∆t) +<br />

x n+1<br />

f<br />

81<br />

x n+1<br />

f<br />

− xn+1,niter<br />

s<br />

<br />

<br />

− xn+1,niter s <br />

<br />

<br />

, (4.1)

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