Altitude Profile and Isotopic Composition for N <sub>2</sub> From Pioneer Venus Mass Spectra

Abstract We report the highest resolution altitude profile and isotopic composition for N 2 at Venus, to date. These results were obtained through re‐analysis of data acquired by the Pioneer Venus Large Probe Neutral Mass Spectrometer (LNMS). The N 2 is non‐uniformly mixed across the clouds and sub‐cloud atmosphere (∼59–15 km) yet uniformly mixed across the deep lower atmosphere (DLA, &lt;15 km). The volume percent for N 2 decreases by ∼2.1‐fold between the clouds (5.21 ± 0.18 vol%; ∼59–51 km) and DLA (2.49 ± 0.10 vol%; &lt;15 km) with concomitant increases in the atmospheric molecular masses. Using the cloud N 2 , we extracted the 15 N/ 14 N ratio (2.93 × 10 −3 ± 0.13 × 10 −3 ) and a corresponding δ 15 N (−204 ± 35‰). Together, the LNMS results suggest that (a) N 2 is not well‐mixed &gt;15 km, (b) the atmosphere is unstable at &lt;15 km, and (c) the cloud δ 15 N falls between the solar wind and Earth's atmosphere.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-11-28
DOI
https://doi.org/10.1029/2025gl118909
Primary Topic
Planetary Science and Exploration
Type
article
Field-Weighted Citation Impact
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article

Altitude Profile and Isotopic Composition for N 2 From Pioneer Venus Mass Spectra

M. J. Way, Rakesh Mogul, S. S. Limaye
Geophysical Research Letters
Planetary Science and Exploration
article

Altitude Profile and Isotopic Composition for N 2 From Pioneer Venus Mass Spectra

M. J. Way, Rakesh Mogul, S. S. Limaye
article en

Abstract

Abstract We report the highest resolution altitude profile and isotopic composition for N 2 at Venus, to date. These results were obtained through re‐analysis of data acquired by the Pioneer Venus Large Probe Neutral Mass Spectrometer (LNMS). The N 2 is non‐uniformly mixed across the clouds and sub‐cloud atmosphere (∼59–15 km) yet uniformly mixed across the deep lower atmosphere (DLA, &lt;15 km). The volume percent for N 2 decreases by ∼2.1‐fold between the clouds (5.21 ± 0.18 vol%; ∼59–51 km) and DLA (2.49 ± 0.10 vol%; &lt;15 km) with concomitant increases in the atmospheric molecular masses. Using the cloud N 2 , we extracted the 15 N/ 14 N ratio (2.93 × 10 −3 ± 0.13 × 10 −3 ) and a corresponding δ 15 N (−204 ± 35‰). Together, the LNMS results suggest that (a) N 2 is not well‐mixed &gt;15 km, (b) the atmosphere is unstable at &lt;15 km, and (c) the cloud δ 15 N falls between the solar wind and Earth's atmosphere.

Geophysical Research LettersVol. 52(23)
Goddard Institute for Space Studies (US), Uppsala University (SE), University of Wisconsin–Madison (US), Blue Marble Space (US), Astronomy and Space (AU), Blue Marble Space Institute of Science (US), California State Polytechnic University (US)
National Aeronautics and Space Administration, Indian Council of Agricultural Research, Nuclear Safety and Security Commission, Goddard Space Flight Center
Openalex Percentile: Top 75%
Planetary Science and Exploration
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Altitude Profile and Isotopic Composition for N <sub>2</sub> From Pioneer Venus Mass Spectra — M. J. Way, Rakesh Mogul, et al. · Geophysical Research Letters (2025) | TGRS Research Map | TGRS