Work Description

Title: Coupled feldspar dissolution and secondary mineral precipitation in batch systems: 6. labradorite dissolution and calcite and clay precipitation Open Access Deposited

http://creativecommons.org/licenses/by-nc/4.0/
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Abstract
  • Current knowledge of geochemical kinetics is primarily based on the dissolution rates of single minerals far from equilibrium. However, geologic systems that store CO₂, such as soils and aquifers, are multi-mineral systems. This study extends our previous isotope doping studies of single minerals to multiple isotope tracer studies of coupled reactions. We conducted experiments on labradorite dissolution, calcite precipitation, and clay precipitation in batch reactor systems.
Methodology
  • We collected the data using ICP-OES, MC-ICP-MS, pH meter and titrator.
Description
  • The measured data for Exp. C and D is listed in Table S2 and Table S3.
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Contact information
Funding agency
  • National Science Foundation (NSF)
Keyword
Date coverage
  • 2024-06-18
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Resource type
Last modified
  • 07/03/2024
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DOI
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To Cite this Work:
Mingkun Chen, Chen Zhu Coupled feldspar dissolution and secondary mineral precipitation in batch systems: 6. labradorite dissolution and calcite and clay precipitation [Data set]. Indiana University - DataCORE. https://doi.org/10.5967/56ck-gp62

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2024.06.18_Supplementary_Materia...E.pdf 2024-06-18 2024-06-18 369 KB Open Access

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