Thermal Process of Rock Crystal: Cause of Infrared Absorption Band at 3585 cm<sup<−1</sup<
Synthetic rock crystals often show a typical infrared (IR) absorption band at 3585 cm<sup<−1</sup<. However, the authors recently found this band in a natural rock crystal with blue coating. The origin of this IR band is controversial as yet. In this paper, the infrared spectra of severa...
Ausführliche Beschreibung
Autor*in: |
Jianjun Li [verfasserIn] Yuyu Zheng [verfasserIn] Xuesong Liu [verfasserIn] Guihua Li [verfasserIn] Xiaoyan Yu [verfasserIn] Yue Wang [verfasserIn] Hejun Li [verfasserIn] Haibin Liu [verfasserIn] Guangqi Shan [verfasserIn] Ting Li [verfasserIn] Xiuyun Ding [verfasserIn] Xiaoxue Zhao [verfasserIn] Zhun Huang [verfasserIn] Ran Du [verfasserIn] Minmin Tian [verfasserIn] Fei Yan [verfasserIn] Bing Sun [verfasserIn] |
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E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2021 |
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Übergeordnetes Werk: |
In: Crystals - MDPI AG, 2011, 11(2021), 9, p 1083 |
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Übergeordnetes Werk: |
volume:11 ; year:2021 ; number:9, p 1083 |
Links: |
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DOI / URN: |
10.3390/cryst11091083 |
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Katalog-ID: |
DOAJ086629204 |
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10.3390/cryst11091083 doi (DE-627)DOAJ086629204 (DE-599)DOAJdaf2b38a4deb4388adce32b027ca7676 DE-627 ger DE-627 rakwb eng QD901-999 Jianjun Li verfasserin aut Thermal Process of Rock Crystal: Cause of Infrared Absorption Band at 3585 cm<sup<−1</sup< 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Synthetic rock crystals often show a typical infrared (IR) absorption band at 3585 cm<sup<−1</sup<. However, the authors recently found this band in a natural rock crystal with blue coating. The origin of this IR band is controversial as yet. In this paper, the infrared spectra of several natural and synthetic rock crystal samples which were heated to 673 K and 1073 K were measured after these samples returned to room temperature. Comparing the infrared spectra of samples before and after heating, we found the absorption band at 3585 cm<sup<−1</sup< was induced by the thermal process, which indicates that this band cannot be used as diagnostic evidence for synthetic rock crystal alone. In addition, the LiOH bands decreased while AlOH bands increased upon thermal processing. And the negative correlation between the LiOH bands and the 3585 cm<sup<−1</sup< band was also distinct. The above results reveal that the thermal process destroyed the LiOH defects, leading to the formation of a new AlLi defect. And the isolated OH<sup<−</sup< defect inside dislocations generated upon thermal processing is considered to be the exact cause of the 3585 cm<sup<−1</sup< band. rock crystal thermal process origin of the 3585 cm<sup<−1</sup< infrared band Crystallography Yuyu Zheng verfasserin aut Xuesong Liu verfasserin aut Guihua Li verfasserin aut Xiaoyan Yu verfasserin aut Yue Wang verfasserin aut Hejun Li verfasserin aut Haibin Liu verfasserin aut Guangqi Shan verfasserin aut Ting Li verfasserin aut Xiuyun Ding verfasserin aut Xiaoxue Zhao verfasserin aut Zhun Huang verfasserin aut Ran Du verfasserin aut Minmin Tian verfasserin aut Fei Yan verfasserin aut Bing Sun verfasserin aut In Crystals MDPI AG, 2011 11(2021), 9, p 1083 (DE-627)718303067 (DE-600)2661516-2 20734352 nnns volume:11 year:2021 number:9, p 1083 https://doi.org/10.3390/cryst11091083 kostenfrei https://doaj.org/article/daf2b38a4deb4388adce32b027ca7676 kostenfrei https://www.mdpi.com/2073-4352/11/9/1083 kostenfrei https://doaj.org/toc/2073-4352 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 11 2021 9, p 1083 |
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10.3390/cryst11091083 doi (DE-627)DOAJ086629204 (DE-599)DOAJdaf2b38a4deb4388adce32b027ca7676 DE-627 ger DE-627 rakwb eng QD901-999 Jianjun Li verfasserin aut Thermal Process of Rock Crystal: Cause of Infrared Absorption Band at 3585 cm<sup<−1</sup< 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Synthetic rock crystals often show a typical infrared (IR) absorption band at 3585 cm<sup<−1</sup<. However, the authors recently found this band in a natural rock crystal with blue coating. The origin of this IR band is controversial as yet. In this paper, the infrared spectra of several natural and synthetic rock crystal samples which were heated to 673 K and 1073 K were measured after these samples returned to room temperature. Comparing the infrared spectra of samples before and after heating, we found the absorption band at 3585 cm<sup<−1</sup< was induced by the thermal process, which indicates that this band cannot be used as diagnostic evidence for synthetic rock crystal alone. In addition, the LiOH bands decreased while AlOH bands increased upon thermal processing. And the negative correlation between the LiOH bands and the 3585 cm<sup<−1</sup< band was also distinct. The above results reveal that the thermal process destroyed the LiOH defects, leading to the formation of a new AlLi defect. And the isolated OH<sup<−</sup< defect inside dislocations generated upon thermal processing is considered to be the exact cause of the 3585 cm<sup<−1</sup< band. rock crystal thermal process origin of the 3585 cm<sup<−1</sup< infrared band Crystallography Yuyu Zheng verfasserin aut Xuesong Liu verfasserin aut Guihua Li verfasserin aut Xiaoyan Yu verfasserin aut Yue Wang verfasserin aut Hejun Li verfasserin aut Haibin Liu verfasserin aut Guangqi Shan verfasserin aut Ting Li verfasserin aut Xiuyun Ding verfasserin aut Xiaoxue Zhao verfasserin aut Zhun Huang verfasserin aut Ran Du verfasserin aut Minmin Tian verfasserin aut Fei Yan verfasserin aut Bing Sun verfasserin aut In Crystals MDPI AG, 2011 11(2021), 9, p 1083 (DE-627)718303067 (DE-600)2661516-2 20734352 nnns volume:11 year:2021 number:9, p 1083 https://doi.org/10.3390/cryst11091083 kostenfrei https://doaj.org/article/daf2b38a4deb4388adce32b027ca7676 kostenfrei https://www.mdpi.com/2073-4352/11/9/1083 kostenfrei https://doaj.org/toc/2073-4352 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 11 2021 9, p 1083 |
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10.3390/cryst11091083 doi (DE-627)DOAJ086629204 (DE-599)DOAJdaf2b38a4deb4388adce32b027ca7676 DE-627 ger DE-627 rakwb eng QD901-999 Jianjun Li verfasserin aut Thermal Process of Rock Crystal: Cause of Infrared Absorption Band at 3585 cm<sup<−1</sup< 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Synthetic rock crystals often show a typical infrared (IR) absorption band at 3585 cm<sup<−1</sup<. However, the authors recently found this band in a natural rock crystal with blue coating. The origin of this IR band is controversial as yet. In this paper, the infrared spectra of several natural and synthetic rock crystal samples which were heated to 673 K and 1073 K were measured after these samples returned to room temperature. Comparing the infrared spectra of samples before and after heating, we found the absorption band at 3585 cm<sup<−1</sup< was induced by the thermal process, which indicates that this band cannot be used as diagnostic evidence for synthetic rock crystal alone. In addition, the LiOH bands decreased while AlOH bands increased upon thermal processing. And the negative correlation between the LiOH bands and the 3585 cm<sup<−1</sup< band was also distinct. The above results reveal that the thermal process destroyed the LiOH defects, leading to the formation of a new AlLi defect. And the isolated OH<sup<−</sup< defect inside dislocations generated upon thermal processing is considered to be the exact cause of the 3585 cm<sup<−1</sup< band. rock crystal thermal process origin of the 3585 cm<sup<−1</sup< infrared band Crystallography Yuyu Zheng verfasserin aut Xuesong Liu verfasserin aut Guihua Li verfasserin aut Xiaoyan Yu verfasserin aut Yue Wang verfasserin aut Hejun Li verfasserin aut Haibin Liu verfasserin aut Guangqi Shan verfasserin aut Ting Li verfasserin aut Xiuyun Ding verfasserin aut Xiaoxue Zhao verfasserin aut Zhun Huang verfasserin aut Ran Du verfasserin aut Minmin Tian verfasserin aut Fei Yan verfasserin aut Bing Sun verfasserin aut In Crystals MDPI AG, 2011 11(2021), 9, p 1083 (DE-627)718303067 (DE-600)2661516-2 20734352 nnns volume:11 year:2021 number:9, p 1083 https://doi.org/10.3390/cryst11091083 kostenfrei https://doaj.org/article/daf2b38a4deb4388adce32b027ca7676 kostenfrei https://www.mdpi.com/2073-4352/11/9/1083 kostenfrei https://doaj.org/toc/2073-4352 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 11 2021 9, p 1083 |
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10.3390/cryst11091083 doi (DE-627)DOAJ086629204 (DE-599)DOAJdaf2b38a4deb4388adce32b027ca7676 DE-627 ger DE-627 rakwb eng QD901-999 Jianjun Li verfasserin aut Thermal Process of Rock Crystal: Cause of Infrared Absorption Band at 3585 cm<sup<−1</sup< 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Synthetic rock crystals often show a typical infrared (IR) absorption band at 3585 cm<sup<−1</sup<. However, the authors recently found this band in a natural rock crystal with blue coating. The origin of this IR band is controversial as yet. In this paper, the infrared spectra of several natural and synthetic rock crystal samples which were heated to 673 K and 1073 K were measured after these samples returned to room temperature. Comparing the infrared spectra of samples before and after heating, we found the absorption band at 3585 cm<sup<−1</sup< was induced by the thermal process, which indicates that this band cannot be used as diagnostic evidence for synthetic rock crystal alone. In addition, the LiOH bands decreased while AlOH bands increased upon thermal processing. And the negative correlation between the LiOH bands and the 3585 cm<sup<−1</sup< band was also distinct. The above results reveal that the thermal process destroyed the LiOH defects, leading to the formation of a new AlLi defect. And the isolated OH<sup<−</sup< defect inside dislocations generated upon thermal processing is considered to be the exact cause of the 3585 cm<sup<−1</sup< band. rock crystal thermal process origin of the 3585 cm<sup<−1</sup< infrared band Crystallography Yuyu Zheng verfasserin aut Xuesong Liu verfasserin aut Guihua Li verfasserin aut Xiaoyan Yu verfasserin aut Yue Wang verfasserin aut Hejun Li verfasserin aut Haibin Liu verfasserin aut Guangqi Shan verfasserin aut Ting Li verfasserin aut Xiuyun Ding verfasserin aut Xiaoxue Zhao verfasserin aut Zhun Huang verfasserin aut Ran Du verfasserin aut Minmin Tian verfasserin aut Fei Yan verfasserin aut Bing Sun verfasserin aut In Crystals MDPI AG, 2011 11(2021), 9, p 1083 (DE-627)718303067 (DE-600)2661516-2 20734352 nnns volume:11 year:2021 number:9, p 1083 https://doi.org/10.3390/cryst11091083 kostenfrei https://doaj.org/article/daf2b38a4deb4388adce32b027ca7676 kostenfrei https://www.mdpi.com/2073-4352/11/9/1083 kostenfrei https://doaj.org/toc/2073-4352 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 11 2021 9, p 1083 |
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10.3390/cryst11091083 doi (DE-627)DOAJ086629204 (DE-599)DOAJdaf2b38a4deb4388adce32b027ca7676 DE-627 ger DE-627 rakwb eng QD901-999 Jianjun Li verfasserin aut Thermal Process of Rock Crystal: Cause of Infrared Absorption Band at 3585 cm<sup<−1</sup< 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Synthetic rock crystals often show a typical infrared (IR) absorption band at 3585 cm<sup<−1</sup<. However, the authors recently found this band in a natural rock crystal with blue coating. The origin of this IR band is controversial as yet. In this paper, the infrared spectra of several natural and synthetic rock crystal samples which were heated to 673 K and 1073 K were measured after these samples returned to room temperature. Comparing the infrared spectra of samples before and after heating, we found the absorption band at 3585 cm<sup<−1</sup< was induced by the thermal process, which indicates that this band cannot be used as diagnostic evidence for synthetic rock crystal alone. In addition, the LiOH bands decreased while AlOH bands increased upon thermal processing. And the negative correlation between the LiOH bands and the 3585 cm<sup<−1</sup< band was also distinct. The above results reveal that the thermal process destroyed the LiOH defects, leading to the formation of a new AlLi defect. And the isolated OH<sup<−</sup< defect inside dislocations generated upon thermal processing is considered to be the exact cause of the 3585 cm<sup<−1</sup< band. rock crystal thermal process origin of the 3585 cm<sup<−1</sup< infrared band Crystallography Yuyu Zheng verfasserin aut Xuesong Liu verfasserin aut Guihua Li verfasserin aut Xiaoyan Yu verfasserin aut Yue Wang verfasserin aut Hejun Li verfasserin aut Haibin Liu verfasserin aut Guangqi Shan verfasserin aut Ting Li verfasserin aut Xiuyun Ding verfasserin aut Xiaoxue Zhao verfasserin aut Zhun Huang verfasserin aut Ran Du verfasserin aut Minmin Tian verfasserin aut Fei Yan verfasserin aut Bing Sun verfasserin aut In Crystals MDPI AG, 2011 11(2021), 9, p 1083 (DE-627)718303067 (DE-600)2661516-2 20734352 nnns volume:11 year:2021 number:9, p 1083 https://doi.org/10.3390/cryst11091083 kostenfrei https://doaj.org/article/daf2b38a4deb4388adce32b027ca7676 kostenfrei https://www.mdpi.com/2073-4352/11/9/1083 kostenfrei https://doaj.org/toc/2073-4352 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 11 2021 9, p 1083 |
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Jianjun Li @@aut@@ Yuyu Zheng @@aut@@ Xuesong Liu @@aut@@ Guihua Li @@aut@@ Xiaoyan Yu @@aut@@ Yue Wang @@aut@@ Hejun Li @@aut@@ Haibin Liu @@aut@@ Guangqi Shan @@aut@@ Ting Li @@aut@@ Xiuyun Ding @@aut@@ Xiaoxue Zhao @@aut@@ Zhun Huang @@aut@@ Ran Du @@aut@@ Minmin Tian @@aut@@ Fei Yan @@aut@@ Bing Sun @@aut@@ |
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Thermal Process of Rock Crystal: Cause of Infrared Absorption Band at 3585 cm<sup<−1</sup< |
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Synthetic rock crystals often show a typical infrared (IR) absorption band at 3585 cm<sup<−1</sup<. However, the authors recently found this band in a natural rock crystal with blue coating. The origin of this IR band is controversial as yet. In this paper, the infrared spectra of several natural and synthetic rock crystal samples which were heated to 673 K and 1073 K were measured after these samples returned to room temperature. Comparing the infrared spectra of samples before and after heating, we found the absorption band at 3585 cm<sup<−1</sup< was induced by the thermal process, which indicates that this band cannot be used as diagnostic evidence for synthetic rock crystal alone. In addition, the LiOH bands decreased while AlOH bands increased upon thermal processing. And the negative correlation between the LiOH bands and the 3585 cm<sup<−1</sup< band was also distinct. The above results reveal that the thermal process destroyed the LiOH defects, leading to the formation of a new AlLi defect. And the isolated OH<sup<−</sup< defect inside dislocations generated upon thermal processing is considered to be the exact cause of the 3585 cm<sup<−1</sup< band. |
abstractGer |
Synthetic rock crystals often show a typical infrared (IR) absorption band at 3585 cm<sup<−1</sup<. However, the authors recently found this band in a natural rock crystal with blue coating. The origin of this IR band is controversial as yet. In this paper, the infrared spectra of several natural and synthetic rock crystal samples which were heated to 673 K and 1073 K were measured after these samples returned to room temperature. Comparing the infrared spectra of samples before and after heating, we found the absorption band at 3585 cm<sup<−1</sup< was induced by the thermal process, which indicates that this band cannot be used as diagnostic evidence for synthetic rock crystal alone. In addition, the LiOH bands decreased while AlOH bands increased upon thermal processing. And the negative correlation between the LiOH bands and the 3585 cm<sup<−1</sup< band was also distinct. The above results reveal that the thermal process destroyed the LiOH defects, leading to the formation of a new AlLi defect. And the isolated OH<sup<−</sup< defect inside dislocations generated upon thermal processing is considered to be the exact cause of the 3585 cm<sup<−1</sup< band. |
abstract_unstemmed |
Synthetic rock crystals often show a typical infrared (IR) absorption band at 3585 cm<sup<−1</sup<. However, the authors recently found this band in a natural rock crystal with blue coating. The origin of this IR band is controversial as yet. In this paper, the infrared spectra of several natural and synthetic rock crystal samples which were heated to 673 K and 1073 K were measured after these samples returned to room temperature. Comparing the infrared spectra of samples before and after heating, we found the absorption band at 3585 cm<sup<−1</sup< was induced by the thermal process, which indicates that this band cannot be used as diagnostic evidence for synthetic rock crystal alone. In addition, the LiOH bands decreased while AlOH bands increased upon thermal processing. And the negative correlation between the LiOH bands and the 3585 cm<sup<−1</sup< band was also distinct. The above results reveal that the thermal process destroyed the LiOH defects, leading to the formation of a new AlLi defect. And the isolated OH<sup<−</sup< defect inside dislocations generated upon thermal processing is considered to be the exact cause of the 3585 cm<sup<−1</sup< band. |
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Thermal Process of Rock Crystal: Cause of Infrared Absorption Band at 3585 cm<sup<−1</sup< |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">DOAJ086629204</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20240412160817.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">230311s2021 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.3390/cryst11091083</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)DOAJ086629204</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)DOAJdaf2b38a4deb4388adce32b027ca7676</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">QD901-999</subfield></datafield><datafield tag="100" ind1="0" ind2=" "><subfield code="a">Jianjun Li</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Thermal Process of Rock Crystal: Cause of Infrared Absorption Band at 3585 cm<sup<−1</sup<</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2021</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Synthetic rock crystals often show a typical infrared (IR) absorption band at 3585 cm<sup<−1</sup<. 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