Quantitative Raman spectroscopic study of the H2CH4 gaseous system
文献类型:期刊论文
作者 | Fang, Jing1,2; Chou, I-Ming2![]() ![]() |
刊名 | JOURNAL OF RAMAN SPECTROSCOPY
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出版日期 | 2018-04-01 |
卷号 | 49期号:4页码:710-720 |
关键词 | H2ch4 Gas System Quantitative Analysis Raman Spectroscopy Silicate Melt Inclusion |
DOI | 10.1002/jrs.5337 |
产权排序 | 第1完成单位 ; 第2完成单位 |
文献子类 | Article |
英文摘要 | The Raman spectra of pure H-2 and CH4 gases and their 5 gaseous mixtures were collected at pressures from 1 to 40MPa at ambient temperature. They were systematically analyzed in order to establish methodology for quantitative determination of composition and pressure of H2CH4 bearing fluid inclusions. The peak positions of 4 vibrational bands of H-2 in pure H-2 gas decrease first and then increase after reaching their minima values at about 30MPa. The wavenumbers of ?(1) band of CH4 in pure CH4 gas decreases in wavenumber monotonically in the entire investigated pressure range. In H2CH4 gaseous mixtures, both the peak positions of H-2 and CH4 shift to lower wavenumbers with increasing pressure. The peak positions of ?(1) band of CH4 can be used to determine the pressure of pure CH4 and CH4-dominated fluids, where the peak position shifts are sufficiently large for precise pressure determination. The peak widths of H-2 and CH4 in pure H-2 and CH4 gases and H2CH4 gaseous mixtures broaden as pressure increases. The peak area ratios and the peak height ratios between CH4 and H-2 in H2CH4 binary mixtures are sensitive to composition (i.e., molar ratio between CH4 and H-2) but are almost independent of pressure. Thus, the peak area or peak height ratios can be used to determine the composition of H2CH4 fluids. On the other hand, the peak height ratios of Q(1)(1) to Q(1)(3) bands in pure H-2 gas or H-2-dominated gaseous mixtures are sensitive to pressure and insensitive to composition. Therefore, in H-2-dominated fluids, the relative peak heights of Q(1)(1) and Q(1)(3) of H-2 is a better alternative for pressure determination. Based on our established Raman quantitative analysis method, we determined the composition and internal pressure of a natural H2CH4-bearing melt inclusion in quartz from Jiajika granite. |
URL标识 | 查看原文 |
WOS关键词 | FLUID INCLUSIONS ; PRESSURE DETERMINATION ; GAS-MIXTURES ; HYDROGEN ; DENSITY ; METHANE ; CO2 ; CALIBRATION ; EQUATION ; SHIFTS |
语种 | 英语 |
WOS记录号 | WOS:000430468200010 |
源URL | [http://ir.idsse.ac.cn/handle/183446/5930] ![]() |
专题 | 深海科学研究部_深海极端环境模拟研究实验室 |
通讯作者 | Chou, I-Ming; Chou, I-Ming(Chinese Acad Sci, Inst Deep Sea Sci & Engn, CAS Key Lab Expt Study Deep Sea Extreme Condit, Sanya 572000, Hainan, Peoples R China) |
作者单位 | 1.Univ Chinese Acad Sci, Beijing 100871, Peoples R China 2.Chinese Acad Sci, Inst Deep Sea Sci & Engn, CAS Key Lab Expt Study Deep Sea Extreme Condit, Sanya 572000, Hainan, Peoples R China |
推荐引用方式 GB/T 7714 | Fang, Jing,Chou, I-Ming,Chen, Ying,et al. Quantitative Raman spectroscopic study of the H2CH4 gaseous system[J]. JOURNAL OF RAMAN SPECTROSCOPY,2018,49(4):710-720. |
APA | Fang, Jing,Chou, I-Ming,Chen, Ying,&Chou, I-Ming.(2018).Quantitative Raman spectroscopic study of the H2CH4 gaseous system.JOURNAL OF RAMAN SPECTROSCOPY,49(4),710-720. |
MLA | Fang, Jing,et al."Quantitative Raman spectroscopic study of the H2CH4 gaseous system".JOURNAL OF RAMAN SPECTROSCOPY 49.4(2018):710-720. |
入库方式: OAI收割
来源:深海科学与工程研究所
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