The DOI matches its Crossref record; 56 of the 58 references it cites were found in a registry or an index.
Stability of ammonia in the primitive terrestrial atmosphere
Abstract
A one‐dimensional photochemical model is used to calculate the rate at which ammonia would have been destroyed in the earth's atmosphere for assumed NH3 mixing ratios of 10−8 to 10−4. The calculated NH3 destruction rates are then compared with possible abiotic and biotic sources for ammonia. Abiotic sources were probably sufficient to maintain the NH3 mixing ratio of 10−8 needed for life to have evolved but were too small to sustain the mixing ratios of 10−5 or more necessary to produce significant greenhouse warming. The atmospheric ammonia concentration may have increased during the Archean as a result of biological activities but probably remained below the level required to generate measurable thermal effects.
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“Ammonia (NH3) levels of 10 to 100 ppmv would provide a greenhouse effect to counteract the faint young Sun (FYS) (14), but these levels of NH3 cannot be sustained against UV photolysis (161).”
From The Archean atmosphere (2020) · cites this paper as [161]
In the citing paper
“Highly reduced gases such as CH 4 or NH 3 are also dissociated by photolysis due to the high XUV flux of the young Sun and by reactions with OH and O radicals produced from the photolysis of H 2 O and CO 2 molecules (Kuhn and Atreya 1979; Kasting 1982; Kasting 1993; Zahnle et al. 2010; Wordsworth 2016).”
From The young Sun's XUV-activity as a constraint for lower CO2-limits in the Earth's Archean atmosphere (2021) · cites this paper as Kasting 1982
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“2020;6 : eaax1420 26 February 2020 Ammonia (NH3) levels of 10 to 100 ppmv would provide a greenhouse effect to counteract the faint young Sun (FYS) (14), but these levels ofNH3 cannot be sustained againstUVphotolysis (161).”
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Metadata
- Authors
- Kasting, J. F.
- Affiliations
- Ames Research Center (US)
- Corresponding author
- Kasting, James F.
- ORCID
- Kasting, James F.
- Venue
- Journal of Geophysical Research: Oceans
- Publisher
- American Geophysical Union (AGU)
- Published
- 1982-04-20
- Volume
- 87
- Issue
- C4
- Pages
- 3091-3098
- ISSN
- 0148-0227 (ISSN-L)
- OpenAlex
- W2033191700
- Cited by
- 140
- References
- 58
- Citations by year
- 2026: 4 · 2025: 7 · 2024: 6 · 2023: 4 · 2022: 3 · 2021: 4 · 2020: 8 · 2019: 8 · 2018: 6 · 2017: 4 · 2016: 1 · 2015: 4 · 2014: 4 · 2013: 5 · 2012: 3
- FWCI
- 10.25
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Journal of Geophysical Research Atmospheres (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Origins and Evolution of Life
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Atmospheric chemistry and aerosols
- Keywords
- ammonia, early Earth atmosphere, atmospheric chemistry, global warming, Archean atmosphere, early Earth, photochemical modeling, atmospheric mixing ratios
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
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