4.5 Article

Quantitative analysis of COH fluids synthesized at HP-HT conditions: an optimized methodology to measure volatiles in experimental capsules

Journal

GEOFLUIDS
Volume 16, Issue 5, Pages 841-855

Publisher

WILEY-HINDAWI
DOI: 10.1111/gfl.12191

Keywords

capsule-piercing QMS technique; COH fluids; HP-HT experiments; mass spectrometry; piston-cylinder

Funding

  1. Italian Ministry of Education, University and Research (MIUR) program [PRIN2012R33ECR]
  2. Deep Carbon Observatory (DCO)

Ask authors/readers for more resources

The quantitative assessment of COH fluids is crucial in modeling geological processes. The composition of fluids, and in particular their H2O/CO2 ratio, can influence the melting temperatures, the location of hydration or carbonation reactions, and the solute transport capability in several rock systems. In the scientific literature, COH fluids speciation has been generally assumed on the basis of thermodynamic calculations using equations of state of simple H2O-nonpolar gas systems (e.g., H2O-CO2-CH4). Only few authors dealt with the experimental determination of high-pressure COH fluid species at different conditions, using diverse experimental and analytical approaches (e.g., piston cylinder + capsule piercing + gas chromatography/mass spectrometry; cold seal + silica glass capsules + Raman). In this contribution, we present a new methodology for the synthesis and the analysis of COH fluids in experimental capsules, which allows the quantitative determination of volatiles in the fluid by means of a capsule-piercing device connected to a quadrupole mass spectrometer. COH fluids are synthesized starting from oxalic acid dihydrate at P = amb and T = 250 degrees C in single capsules heated in a furnace, and at P = 1 GPa and T = 800 degrees C using a piston-cylinder apparatus and the double-capsule technique to control the redox conditions employing the rhenium-rhenium oxide oxygen buffer. A quantitative analysis of H2O, CO2, CH4, CO, H-2, O-2, and N-2 along with associated statistical errors is obtained by linear regression of the m/z data of the sample and of standard gas mixtures of known composition. The estimated uncertainties are typically <1% for H2O and CO2, and <5% for CO. Our results suggest that the COH fluid speciation is preserved during and after quench, as the experimental data closely mimic the thermodynamic model both in terms of bulk composition and fluid speciation.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.5
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available