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1.Beijing National Laboratory for Molecular Sciences, State Key Laboratory of Rare Earth Materials Chemistry and Applications, PKU-HKU Joint Laboratory in Rare Earth Materials and Bioinorganic Chemistry, College of Chemistry and Molecular Engineering, Peking University, Beijing 100871, China
2.College of Science, Nanjing Forestry University, Nanjing 210037, China
3.College of Materials Science and Engineering, Nanjing Forestry University, Nanjing 210037, China
4.School of Physical Science and Technology, Inner Mongolia Key Lab of Nanoscience and Nanotechnology, Inner Mongolia University, Hohhot 010021, China
5.Analytical Instrumentation Center of Peking University, Beijing 100871, China
6.School of Chemical and Environmental Engineering, Shanghai Institute of Technology, Shanghai 201418, China
Ling-Dong Sun (sun@pku.edu.cn)
Chun-Hua Yan (yan@pku.edu.cn)
Received:04 November 2024,
Revised:28 February 2025,
Accepted:06 March 2025,
Published Online:13 May 2025,
Published:31 July 2025
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Xiao, Y. et al. Tracing the origin of near-infrared emissions emanating from manganese (Ⅱ). Light: Science & Applications, 14, 1989-2000 (2025).
Xiao, Y. et al. Tracing the origin of near-infrared emissions emanating from manganese (Ⅱ). Light: Science & Applications, 14, 1989-2000 (2025). DOI: 10.1038/s41377-025-01816-y.
The enduring enigma surrounding the near-infrared (NIR) emiss
ion of Mn
2+
continues to ignite intense academic discussions. Numerous hypotheses have emerged from extensive research endeavors to explain this phenomenon
such as the formation of Mn
2+
–Mn
2+
ion pairs
Mn
2+
occupying cubically coordinated sites
as well as conjectures positing the involvement of Mn
3+
oxidized from Mn
2+
or defects. Despite these diverse and valuable insights
none of the hypotheses have yet achieved broad consensus. In this study
we have observed prolonged fluorescence lifetimes (~10 ms) for the NIR emissions of Mn
2+
ions
hinting at these ions occupying the high-symmetry octahedral sites inherent to the garnet lattice. This inference is supported by the corroborating results from X-ray absorption fine structure analysis and first-principles calculations. The intense crystal field of octahedral sites
similar to that of AlO
6
facilitates the splitting of
d
–
d
energy levels
thereby inducing a red-shift in the emission spectrum to the NIR region due to the transition
4
T
1
(
4
G) →
6
A
1
(
6
S) of isolated Mn
2+
. Our findings not only offer a plausible rationale for the NIR emission exhibited by other Mn
2+
-activated garnet phosphors but also pave a definitive route towards understanding the fundamental mechanisms responsible for the NIR emission of Mn
2+
ions.
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