C13 and O18 compositions in some fresh-water carbonates associated with ultramafic rocks and serpentinites: Western United States
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The observed DIC carbon isotope signature may reflect kinetic 13C depletion during diffusion of atmospheric CO2 into solution.
“The observed carbon isotopic signature of DIC in process and tailings water may reflect (1) kinetic depletion of 13 C during diffusion of atmospheric CO 2 into solution”
From Offsetting of CO2 emissions by air capture in mine tailings at the Mount Keith Nickel Mine, Western Australia: Rates, controls and prospects for carbon neutral mining (2014) · cites this paper as O'Neil and Barnes, 1971
Ca-carbonates precipitating from the ultrabasic waters have unusually low δ13C and δ18O values.
“and that Ca-carbonates precipitating from the ultrabasic waters have unusually low δ 13 C and δ 18 O values (O'Neil and Barnes, 1971).”
From Isotopic fractionation accompanying CO2 hydroxylation and carbonate precipitation from high pH waters at The Cedars, California, USA (2021) · cites this paper as O'Neil and Barnes, 1971
Ca-carbonates formed in hyperalkaline springs exhibit some of the largest and most systematic variations of δ13C and δ18O.
“Ca-carbonates formed in hyperalkaline springs exhibit some of the largest and most systematic variations of δ 13 C and δ 18 O”
From Isotopic fractionation accompanying CO2 hydroxylation and carbonate precipitation from high pH waters at The Cedars, California, USA (2021) · cites this paper as O'Neil and Barnes, 1971
We observed aragonite in all samples examined with XRPD or SEM, as did Meister et al. (2011) and O'Neil and Barnes (1971), including in pool rims, pool snow, pool floes and precipitates from mixed spring/creek waters.
“We observed aragonite in all of our samples examined with XRPD or SEM, as did Meister et al. (2011) and O'Neil and Barnes, (1971), including in pool rims, pool snow, pool floes and precipitates from mixed spring/creek waters”
From Isotopic fractionation accompanying CO2 hydroxylation and carbonate precipitation from high pH waters at The Cedars, California, USA (2021) · cites this paper as O'Neil and Barnes, (1971)
The oxygen isotope exchange equations of Aharon (1988) and O'Neil and Barnes (1971) are internally consistent, closely resemble experimental data, and yield d18Ofluid compositions that correspond to possible natural fluid sources.
“We note that the oxygen isotope exchange equations of Aharon (1988) and O'Neil and Barnes (1971) are internally consistent, closely resemble experimental data, and yield d 18 Ofluid compositions that correspond to possible natural fluid sources.”
From Clumped-isotope thermometry of magnesium carbonates in ultramafic rocks (2016) · cites this paper as O'Neil and Barnes, 1971
Evapoconcentration and uptake of atmospheric CO2 into tailings pore waters can result in the precipitation of hydrated Mg-carbonate minerals such as hydromagnesite.
“Evapoconcentration and uptake of atmospheric CO 2 into tailings pore waters can result in the precipitation of hydrated Mg-carbonate minerals (Equation (1); e.g., hydromagnesite), which are common low-temperature weathering products of natural serpentine minerals and brucite (e.g., [43,44]).”
From Strategizing carbon-neutral mines: A case for pilot projects (2014) · cites this paper as [44]
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- Authors
- O'Neil, J. R., & Barnes, I.
- Affiliations
- United States Geological Survey (US)
- Venue
- Geochimica et Cosmochimica Acta
- Publisher
- Elsevier BV
- Published
- 1971-07
- Volume
- 35
- Issue
- 7
- Pages
- 687-697
- ISSN
- 0016-7037 (ISSN-L)
- OpenAlex
- W2072501578
- Semantic Scholar
- 00266bb88cf068f087452cde994c973081f36758
- Cited by
- 136
- References
- 7
- Citations by year
- 2026: 1 · 2025: 3 · 2024: 3 · 2023: 4 · 2022: 7 · 2021: 10 · 2020: 6 · 2019: 2 · 2018: 9 · 2017: 10 · 2016: 7 · 2015: 3 · 2014: 4 · 2013: 6 · 2012: 9
- FWCI
- 2.40
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Geochimica et Cosmochimica Acta (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Groundwater and Isotope Geochemistry
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Keywords
- stable carbon isotopes, stable oxygen isotopes, ultramafic rocks, serpentinite, hydromagnesite, nesquehonite, travertine, hydrothermal veins, carbonate origin, American West
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