Experimental geoscientist · CNR, Italy

Sumith
Abeykoon

I recreate the conditions of planetary interiors in the laboratory to study what they are made of, how silicates, metals, sulphur and fluids behave and move within them, and how magma rises to feed volcanoes.

First light on an alpine summit First light on the Mont Blanc massif
Electron microscope image of a metal sphere surrounded by silicate melt A planet, 1 mm across
Recent

Latest from the laboratory

All research highlights
    Tungsten carbide cubes of a multi-anvil press, arranged around the sample Multi-anvil press assembly — eight tungsten carbide cubes close on a sample the size of a grain of rice
    The method

    Cook and look

    We cannot drill more than fifteen kilometres into the Earth, so we make the deep Earth in the laboratory instead. A press squeezes a tiny sample from all sides while a heater takes it to magmatic temperatures; then we take it out and look at it with every instrument we can get our hands on — electron probe, Raman, calorimetry, neutron and X-ray diffraction, tomography. At a synchrotron, we sometimes watch it while it is still cooking.

    Half of the job is physics. The other half is a workshop: building the assemblies, commissioning the presses, and writing the software that runs them.

    How it works, for anyone

    “ Science is the training. Becoming a good person is the work.
    Sumith Abeykoon Contact

    Students, collaborators, and the curious

    I co-supervise master's and PhD students and I am open to collaboration — on high-pressure experiments, melt rheology, volcanic materials, glass and ceramics, metals and alloys, or a sample you have and no way to measure. If you read something here and want to talk about it, write.