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Updated: Jul 12, 2026

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Measurement of the Potential Rates of Dissimilatory Nitrate Reduction to Ammonium Based on 14NH4+/15NH4+ Analyses via Sequential Conversion to N2O
Published on: October 7, 2020
What has caused the secular increase in solar nitrogen-15?
Summary
Nitrogen isotope ratios in lunar samples reveal a surprising change in the solar wind over billions of years. This solar evolution mystery challenges current solar physics understanding.
Area of Science:
- * Planetary Science
- * Solar Physics
- * Geochemistry
Background:
- * Lunar surface samples exhibit variations in nitrogen isotope ratios.
- * These variations suggest changes in the solar wind composition over geological timescales.
- * The solar wind is the stream of charged particles released from the upper atmosphere of the Sun.
Purpose of the Study:
- * To investigate the cause of the observed variations in the nitrogen isotope ratio ((15)N/(14)N) in lunar samples.
- * To understand the implications of these variations for solar evolution.
- * To identify potential challenges to the current solar paradigm.
Main Methods:
- * Analysis of nitrogen isotope ratios ((15)N/(14)N) in lunar regolith and soil samples.
- * Comparison of isotopic data with models of solar wind evolution.
- * Examination of solar processes, specifically the solar convective zone.
Main Results:
- * A secular increase in the (15)N/(14)N ratio in the solar wind over the past few billion years is documented.
- * The source of this isotopic change appears to be linked to the solar convective zone.
- * The observed phenomenon is currently inexplicable within the framework of existing solar models.
Conclusions:
- * The variation in lunar nitrogen isotopes points to a significant, unexplained change in solar wind composition.
- * This finding presents a major challenge to our understanding of solar processes, comparable to the solar neutrino problem.
- * Further research into solar physics is required to reconcile these observations with current theories.
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