Solution

ID: past-exam-of-the-year-2-of-the-earth-sciences-geology-course-of-the-university-of-oxford/2024/paper-3/5/a/solution

Put and suppose , so there are interior grid points , . Write . The fixed ends impose homogeneous Dirichlet boundary conditions,
For a sufficiently smooth displacement field, the two Taylor series at fixed time give
where all displayed derivatives on the right are evaluated at . Adding cancels the odd terms, leaving the second-order central difference
Substitute this finite difference into the wave equation and retain continuous time. The resulting method of lines gives coupled second-order ordinary differential equations,
In particular, the first and last equations are and for . With the interior displacement vector only,
Equivalently, , , and all other entries vanish. This entrywise definition also covers small , including when . The matrix is a symmetric matrix and a tridiagonal matrix. The spatial approximation has error in Big O notation; time has not yet been discretized.

New to topics? Read the docs here!