Solution

ID: past-exam-of-the-physics-a-course-of-the-university-of-cambridge/2015/paper-2/section-b/b6/a/solution

For , define . The two characteristic roots are real and negative:
This is overdamping: there is no repeated oscillation, and the slow root controls late-time return. A generic initial velocity can still cause a single crossing of equilibrium, so “nonoscillatory” need not mean monotone for all initial data. For large , the slow root approaches .

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