Professional Committee of Rock and Mineral Testing Technology of the Geological Society of China, National Geological Experiment and Testing CenterHost
2018 Vol. 37, No. 2
Article Contents

Ran ZHANG, Hong XU, Mei-mei LI. Vibrational Spectroscopy Characteristics of Rare Mineral Chambersite in Jixian of Tianjin, China[J]. Rock and Mineral Analysis, 2018, 37(2): 139-145. doi: 10.15898/j.cnki.11-2131/td.201703160034
Citation: Ran ZHANG, Hong XU, Mei-mei LI. Vibrational Spectroscopy Characteristics of Rare Mineral Chambersite in Jixian of Tianjin, China[J]. Rock and Mineral Analysis, 2018, 37(2): 139-145. doi: 10.15898/j.cnki.11-2131/td.201703160034

Vibrational Spectroscopy Characteristics of Rare Mineral Chambersite in Jixian of Tianjin, China

More Information
  • Chambersite (Mn3B7O13Cl) is a type of rare mineral. The Chambersite deposit in Jixian, Tianjin is the only commercially valuable deposit in the world. The Chambersite particle in Jixian is very fine (50-300 nm), which is different from that of American Chambersite. Until now, little study was carried out has been conducted on Chinese Chambersite. In order to explore the mineralogical and material characteristics of Chambersite in Jixian, a Vibration Spectrum and high-temperature Raman Spectrum were recorded. Normal-temperature Vibration Spectrum shows that the main spectrum band assignment of Chinese Chambersite is the same as that of American Chambersite. However, as a whole, the peak position is shifted toward the high-frequency direction and the spectral width and intensity are small. High-temperature Raman Spectroscopy shows that with the increase of temperature, bands generally shift to the low frequency, the displacement distance increases first and then decreases, and the displacement distance turns at 680-687 K. The small particle size is the main reason for spectrum peak changes. High-temperature Raman Spectroscopy technique was used to test and analyze Chambersite with very fine particle size, and the relationship between the peak change and phase transition was studied, thus demonstrating that high temperature Raman Spectroscopy can be used as an effective method to study mineral phase transition.
  • 加载中
  • [1] 肖成东, 张静, 张宝华, 等.天津蓟县锰方硼石矿床[J].地质调查与研究, 2007, 30(3):186-191.

    Google Scholar

    Xiao C D, Zhang J, Zhang B H, et al.Chambersite deposit in Jixian, Tianjin[J].Geological Survey and Research, 2007, 30(3):186-191.

    Google Scholar

    [2] 肖荣阁, 大井隆夫, 侯万荣, 等.天津蓟县硼矿床锰方硼石矿物的硼同位素研究[J].现代地质, 2002, 16(3):270-275.

    Google Scholar

    Xiao R G, Tako O, Hou W R, et al.Boron isotopic composition of Dongshuichang Chambersite deposit, Jixian, Tianjin, China[J].Geoscience, 2002, 16(3):270-275.

    Google Scholar

    [3] 王秋舒, 许虹, 高燊, 等.稀有矿物锰方硼石的合成及其矿床地质意义[J].地学前缘, 2013, 20(3):123-130.

    Google Scholar

    Wang Q S, Xu H, Gao S, et al.Synthesis of the rare mineral Chambersite and its ore deposit geological significance[J].Earth Science Frontiers, 2013, 20(3):123-130.

    Google Scholar

    [4] Grice J D, Gault R A, Velthuizen J V.Borate minerals of the Penobsquis and Millstream Deposit, Southern New Brunswick[J].Canadian Mineralogist, 2005, 43:1469-1488. doi: 10.2113/gscanmin.43.5.1469

    CrossRef Google Scholar

    [5] 王秋舒. 天津蓟县锰方硼石矿物学特征及其成矿机理初探[D]. 北京: 中国地质大学(北京), 2013.

    Google Scholar

    Wang Q S. Mineralogical Characteristcis of the Chambersite and Its Ore Genesis of Jixian, Tianjin[D]. Beijing: China University of Geosciences (Beijing), 2013.

    Google Scholar

    [6] 王富良, 付勇, 徐志刚, 等.天津蓟县东水厂锰方硼石矿床成因新认识[J].地质学报, 2016, 90(2):398-408.

    Google Scholar

    Wang F L, Fu Y, Xu Z G, et al.The new understanding of the cause of Dongshuichang Chambersite deposit in Jixian, Tianjin[J].Acta Geologica Sinica, 2016, 90(2):398-408.

    Google Scholar

    [7] Fan D L, Yang P J, Wang R, et al.Characteristics and origin of the Middle Proterozoic Dongshuichang Chambersite deposit, Jixian, Tianjin, China[J].Ore Geology Reviews, 1999, 15(1-3):15-29. doi: 10.1016/S0169-1368(99)00012-8

    CrossRef Google Scholar

    [8] 曾贻善.锰方硼石的合成及其地球化学意义[J].地质学报, 1983(4):401-409.

    Google Scholar

    Zeng Y S.Synthesis of Chambersite and its geochemical implication[J].Acta Geologica Sinica, 1983(4):401-409.

    Google Scholar

    [9] Frost R L, Lópze A, Scholz R, et al.Vibrational spectro-scopy of the borate mineral Chambersite Mn3B7O13Cl-Implications of the molecular structure[J].Spectrochimica Acta Part A:Molecular and Biomolecular Spectroscopy, 2014, 120:270-273. doi: 10.1016/j.saa.2013.10.026

    CrossRef Google Scholar

    [10] 查福标, 谢先德, 彭文世.硼酸盐矿物的振动光谱研究:Ⅲ.理论分析[J].矿物学报, 1993, 13(4):303-308.

    Google Scholar

    Zha F B, Xie X D, Peng W S.A vibrational spectral study of Borates-Ⅲ.Theoretical analyses[J].Acta Mineralogic Sinica, 1993, 13(4):303-308.

    Google Scholar

    [11] 查福标, 谢先德, 彭文世.硼酸盐矿物的振动光谱研究:Ⅱ.红外光谱特征[J].矿物学报, 1993, 13(3):230-236.

    Google Scholar

    Zha F B, Xie X D, Peng W S.A vibrational spectral study of Borates-Ⅱ.Infraed spectroscopy[J].Acta Mineralogic Sinica, 1993, 13(3):230-236.

    Google Scholar

    [12] Wachowiak J, Pieczak A.Congolite and Trembathite from the Klodawa salt mine, central Poland:Records of the thermal history of the parental salt dome[J].The Canadian Mineralogist, 2012, 50:1387-1399. doi: 10.3749/canmin.50.5.1387

    CrossRef Google Scholar

    [13] 谢先德, 查福标.硼酸盐矿物的振动光谱研究:Ⅰ.拉曼光谱特征[J].矿物学报, 1993, 13(2):130-136.

    Google Scholar

    Xie X D, Zha F B.vibrational spectral study of Borates-Ⅰ.Raman spectroscopy[J].Acta Mineralogic Sinica, 1993, 13(2):130-136.

    Google Scholar

    [14] 陈辉, 蒋国昌, 尤静林, 等.高温拉曼光谱技术的实现及应用[J].光谱学与光谱分析, 2007, 27(12):2464-2467.

    Google Scholar

    Chen H, Jiang G C, You J L, et al.High temperature Raman spectroscopy techniques and its applications[J].Spectroscopy and Spectral Analysis, 2007, 27(12):2464-2467.

    Google Scholar

    [15] 陈辉, 蒋国昌, 尤静林, 等.高温拉曼光谱提高信噪比的途径分析[J].光谱学与光谱分析, 2007, 27(6):1148-1151.

    Google Scholar

    Chen H, Jiang G C, You J L, et al.Analysis of different methods for denoising of high temperature Raman spectra[J].Spectroscopy and Spectral Analysis, 2007, 27(6):1148-1151.

    Google Scholar

  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Figures(4)

Tables(1)

Article Metrics

Article views(3785) PDF downloads(83) Cited by(0)

Access History

Other Articles By Authors

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint