Variation of Mg isotopes during mineral dissolution at pH = 1 and T = 25 °C: Part 2. Olivine and pyroxene
Abstract Background The high reactivity of mafic minerals, such as olivine and pyroxene, plays a crucial role in controlling the global magnesium (Mg) flux and its isotopic composition. This study investigates the mechanisms and extent of Mg isotope fractionation during the dissolution of these mine...
Saved in:
| Main Author: | Jong-Sik Ryu |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
SpringerOpen
2025-02-01
|
| Series: | Journal of Analytical Science and Technology |
| Subjects: | |
| Online Access: | https://doi.org/10.1186/s40543-025-00479-z |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Similar Items
-
Variation of Mg isotopes during mineral dissolution at pH = 1 and T = 25 °C: Part 1. Hornblende and chlorite
by: Jong-Sik Ryu
Published: (2025-02-01) -
Oxygen Isotopic Compositions of San Carlos Olivine Standard NMNH 111312–42
by: Kezhen Qu, et al.
Published: (2025-02-01) -
Trace element composition of silicate minerals from Kunashak Meteorite (L6)
by: Kristina G. Sukhanova, et al.
Published: (2024-12-01) -
The alkalinity generation potential of olivine and oyster shell for laboratory experiments: testing the effects of ocean alkalinity enhancement
by: Cale A Miller, et al.
Published: (2025-01-01) -
δ26Mg, δ44Ca and 87Sr/86Sr isotope ratios constrain Mg and Ca input–output mass balances in a heavily acidified headwater catchment
by: Martin Novak, et al.
Published: (2024-12-01)