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Showing 1–2 of 2 results
Advanced filters: Author: T. R. Boehly Clear advanced filters

  • Measurements of the melting point of diamond at pressures of around 10 million atm suggest it could be present in crystalline form in the interiors of giant planets. At even higher pressures and temperatures about 50,000 K, diamond melts to form an unexpectedly complex, polymer-like fluid phase.

    • J. H. Eggert
    • D. G. Hicks
    • G. W. Collins
    Research
    Nature Physics
    Volume: 6, P: 40-43

  • Warm dense silica is a key component in rocky planets’ mantles, but reproducing the relevant conditions in experiments is challenging. Here the authors use a double-shock technique to achieve such conditions and measure the reflectivity in situ, providing insight into the conductivity and its possible impact on dynamo processes in super-Earths’ mantles.

    • M. Guarguaglini
    • F. Soubiran
    • A. Ravasio
    ResearchOpen Access
    Nature Communications
    Volume: 12, P: 1-8