Solution

ID: past-exam-of-the-year-2-of-the-earth-sciences-geology-course-of-the-university-of-oxford/2025/paper-3/7/f/solution

Diffusion smooths and broadens the hot spot while conserving its integral. For an isolated two-dimensional initial profile , the Gaussian hot spot under diffusion is
Here and , giving a width parameter of and a peak of in the initial temperature units. The periodic-grid calculation agrees to displayed precision because the periodic copies are far away. Running the endpoint-inclusive listing as written instead gives a sampled initial peak near and final peak near ; the difference is consistent with the coordinate-grid issue, rather than a different diffusion law.
Increasing positive thermal diffusivity at fixed time produces a wider, lower peak. Each nonconstant Fourier mode decays faster, while the spatial mean of a periodic heat equation remains fixed. The profiles approach a uniform mean at long times under these periodic boundary conditions.
Figure 1.
Diffusion of a Gaussian hot spot, with and without a spatially uniform decaying heat source
. Original calculations on an endpoint-excluded periodic grid. The cross-sections use a common temperature scale; the source contribution is a uniform offset. The dashed initial profile and the two final profiles are calculated rather than copied from the supplied examination figure. Details.

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