Long-term relaxation of orientational disorder and structural modifications in molecular nitrogen at high pressure

Up to 17 GPa, the crystalline phases of N2 are characterized by pronounced orientational disorder, whereas the higher-pressure phases of molecular N2 are ordered. This raises the question about long-term relaxation of orientational disorder within the low- to intermediate-pressure regime. Here, this question is addressed by comparing synthetic with natural, chemically pure, solid N2 that resides as inclusions in diamonds at 300 K for about 108 years at pressures up to 11 GPa. It is shown that disorder prevails at 8.7 GPa, 300 K, where both synthetic and natural N2 assume the same structure. However, at 10.8 GPa, natural solid N2 exhibits monoclinic distortion and partial orientational ordering of the molecules, both of which are not observed in synthetic material. This difference is interpreted as the result of long-term structural relaxation. The ordering mechanism is examined and placed into the context of the δ- to ε-N2 transition. We present explanations for the absence of complete ordering of δ-N2.

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Publication Details

Journal
The Journal of Chemical Physics
Published
2024-11-27
DOI
https://doi.org/10.1063/5.0219186
Citations
2
Primary Topic
High-pressure geophysics and materials
Type
article
Field-Weighted Citation Impact
1.07

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article

Long-term relaxation of orientational disorder and structural modifications in molecular nitrogen at high pressure

Oded Navon, Yael Kempe, Oliver Tschauner, Vitali B. Prakapenka et al.
2 citations
The Journal of Chemical Physics
High-pressure geophysics and materials
1.07
article

Long-term relaxation of orientational disorder and structural modifications in molecular nitrogen at high pressure

Oded Navon, Yael Kempe, Oliver Tschauner, Vitali B. Prakapenka, Stella Chariton, Sergei Remennik, Yaakov Weiss, Christian Schmidt, Wenjun Liu, Richard Wirth
article en
2 citations

Abstract

Up to 17 GPa, the crystalline phases of N2 are characterized by pronounced orientational disorder, whereas the higher-pressure phases of molecular N2 are ordered. This raises the question about long-term relaxation of orientational disorder within the low- to intermediate-pressure regime. Here, this question is addressed by comparing synthetic with natural, chemically pure, solid N2 that resides as inclusions in diamonds at 300 K for about 108 years at pressures up to 11 GPa. It is shown that disorder prevails at 8.7 GPa, 300 K, where both synthetic and natural N2 assume the same structure. However, at 10.8 GPa, natural solid N2 exhibits monoclinic distortion and partial orientational ordering of the molecules, both of which are not observed in synthetic material. This difference is interpreted as the result of long-term structural relaxation. The ordering mechanism is examined and placed into the context of the δ- to ε-N2 transition. We present explanations for the absence of complete ordering of δ-N2.

The Journal of Chemical PhysicsVol. 161(20)
Argonne National Laboratory (US), University of Nevada, Las Vegas (US), Hebrew University of Jerusalem (IL), University of Chicago (US), GFZ Helmholtz Centre for Geosciences (DE), Instituto de Ciências da Terra
National Science Foundation, Israel Science Foundation, Office of Science
Openalex Percentile: Top 23%
High-pressure geophysics and materials
1.07
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