Description

The transport of hydrogen to the Earth’s deep interior remains uncertain. The upper mantle minerals have very low hydrogen solubilities (hundreds of ppm). The hydrogen storage capability in the transition zone minerals (2 wt%) is high compared to

The transport of hydrogen to the Earth’s deep interior remains uncertain. The upper mantle minerals have very low hydrogen solubilities (hundreds of ppm). The hydrogen storage capability in the transition zone minerals (2 wt%) is high compared to those of the upper mantle. The hydrogen storage in the lower mantle is not well known.

Downloads
pdf (9.5 MB)

Download count: 0

Details

Contributors
Date Created
2019
Resource Type
  • Text
  • Collections this item is in
    Note
    • Doctoral Dissertation Natural Science 2019

    Machine-readable links