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 those of the upper mantle. The hydrogen storage in the lower mantle is not well known.
Copyright Statement
Download count: 0
Details
Contributors
- Chen, Huawei (Author)
- Shim, Sang-Heon (Thesis advisor)
- Garnero, Edward (Committee member)
- Bose, Maitrayee (Committee member)
- Li, Mingming (Committee member)
- Leinenweber, Kurt (Committee member)
- Arizona State University (Publisher)
Date Created
The date the item was original created (prior to any relationship with the ASU Digital Repositories.)
2019
Resource Type
Collections this item is in
Note
- Doctoral Dissertation Natural Science 2019