Isotope fractionation and mass fractionation laws of Fe and Ni during evaporation

High-temperature evaporation is a fundamental process shaping the chemical and isotopic signatures of planetary materials, yet the specific physical laws governing isotopic fractionation during evaporation remain debated. We investigated the mass-dependent isotope fractionation of Fe and Ni during vacuum evaporation of metallic melts. The residues exhibit large isotope fractionation, reaching up to 11.4 ‰ for δ 56/54 Fe and 2.9 ‰ for δ 60/58 Ni. Determining the isotope fractionation factors for Fe and Ni [ 𝛼 = ( 𝑚 𝑖 ⁢ 1 / 𝑚 𝑖 ⁢ 2 ) 𝛽 ] using the Rayleigh distillation model yielded a 𝛽 value of 0.5 for both Fe and Ni. Further, the evaporation coefficients of Fe and Ni were found to be similar ( 𝛾 F e ≃ 𝛾 N i ). These results suggest that Fe and Ni evaporation from metallic melts is ideal and uninhibited by kinetic barriers. We used high-precision three-isotope plots to constrain the mass fractionation law governing the evaporation process. Both Fe and Ni in the evaporation residue strictly follow the law of 𝑛 = − 0 . 5 , distinct from the exponential law ( 𝑛 = 0 ) typically assumed for kinetic processes. We propose a theoretical framework to reconcile this observation with kinetic gas theory: while the intrinsic instantaneous isotope fractionation between vapor and melt follows the exponential law, the apparent law observed in the residue is shifted by the Rayleigh distillation process. We derive a general relationship showing that the divergence between the apparent law and the intrinsic law during a Rayleigh distillation process is controlled by the magnitude of isotope fractionation ( 𝛽 ), 𝑛 a p p r ≃ [ 1 + 𝛽 𝑖 ⁢ 2 / 𝑖 ⁢ 1 2 ⁢ l n ⁡ ( 𝑚 𝑖 ⁢ 1 𝑚 𝑖 ⁢ 2 ) ] ⁢ 𝑛 i n s t − 𝛽 𝑖 ⁢ 2 / 𝑖 ⁢ 1 . This framework unifies conflicting observations regarding mass fractionation laws in previous evaporation experiments. The implications of these results for the evaporation history of Type-I cosmic spherules and for identifying nucleosynthetic isotopic anomalies are discussed.

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Publication Details

Journal
Earth and Planetary Science Letters
Published
2026-09-11
DOI
https://doi.org/10.1016/j.epsl.2026.120321
Primary Topic
Planetary Science and Exploration
Type
article
Field-Weighted Citation Impact
0.00

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article

Isotope fractionation and mass fractionation laws of Fe and Ni during evaporation

Zhe J. Zhang, Nicole X. Nie, Damanveer S. Grewal
Earth and Planetary Science Letters
Planetary Science and Exploration
article

Isotope fractionation and mass fractionation laws of Fe and Ni during evaporation

Zhe J. Zhang, Nicole X. Nie, Damanveer S. Grewal
article en

Abstract

High-temperature evaporation is a fundamental process shaping the chemical and isotopic signatures of planetary materials, yet the specific physical laws governing isotopic fractionation during evaporation remain debated. We investigated the mass-dependent isotope fractionation of Fe and Ni during vacuum evaporation of metallic melts. The residues exhibit large isotope fractionation, reaching up to 11.4 ‰ for δ 56/54 Fe and 2.9 ‰ for δ 60/58 Ni. Determining the isotope fractionation factors for Fe and Ni [ 𝛼 = ( 𝑚 𝑖 ⁢ 1 / 𝑚 𝑖 ⁢ 2 ) 𝛽 ] using the Rayleigh distillation model yielded a 𝛽 value of 0.5 for both Fe and Ni. Further, the evaporation coefficients of Fe and Ni were found to be similar ( 𝛾 F e ≃ 𝛾 N i ). These results suggest that Fe and Ni evaporation from metallic melts is ideal and uninhibited by kinetic barriers. We used high-precision three-isotope plots to constrain the mass fractionation law governing the evaporation process. Both Fe and Ni in the evaporation residue strictly follow the law of 𝑛 = − 0 . 5 , distinct from the exponential law ( 𝑛 = 0 ) typically assumed for kinetic processes. We propose a theoretical framework to reconcile this observation with kinetic gas theory: while the intrinsic instantaneous isotope fractionation between vapor and melt follows the exponential law, the apparent law observed in the residue is shifted by the Rayleigh distillation process. We derive a general relationship showing that the divergence between the apparent law and the intrinsic law during a Rayleigh distillation process is controlled by the magnitude of isotope fractionation ( 𝛽 ), 𝑛 a p p r ≃ [ 1 + 𝛽 𝑖 ⁢ 2 / 𝑖 ⁢ 1 2 ⁢ l n ⁡ ( 𝑚 𝑖 ⁢ 1 𝑚 𝑖 ⁢ 2 ) ] ⁢ 𝑛 i n s t − 𝛽 𝑖 ⁢ 2 / 𝑖 ⁢ 1 . This framework unifies conflicting observations regarding mass fractionation laws in previous evaporation experiments. The implications of these results for the evaporation history of Type-I cosmic spherules and for identifying nucleosynthetic isotopic anomalies are discussed.

Earth and Planetary Science LettersVol. 695
Planetary Science Institute (US), Yale University (US), Massachusetts Institute of Technology (US)
National Aeronautics and Space Administration, Yale University, Massachusetts Institute of Technology
Openalex Percentile: Top 11%
Planetary Science and Exploration
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