The influence of ionic strength on carbonate-based spectroscopic barometry for aqueous fluids: an in-situ Raman study on Na2CO3-NaCl solutions

被引:7
作者
Wu, Jia [1 ]
Wang, Shixia [2 ]
Zheng, Haifei [3 ]
机构
[1] China Univ Petr, Coll Geosci, State Key Lab Petr Resources & Prospecting, Beijing 102249, Peoples R China
[2] Univ Shanghai Sci & Technol, Coll Sci, Shanghai 200093, Peoples R China
[3] Peking Univ, Dept Geol, Key Lab Orogen Belts & Crustal Evolut, Beijing 100871, Peoples R China
来源
SCIENTIFIC REPORTS | 2016年 / 6卷
基金
中国国家自然科学基金;
关键词
HIGH-PRESSURE; MAGNESIUM-SULFATE; QUARTZ SOLUBILITY; TEMPERATURE; WATER; BICARBONATE; INCLUSIONS; SCATTERING; GAUGE; RUBY;
D O I
10.1038/srep39088
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The Raman wavenumber of the symmetric stretching vibration of carbonate ion (nu(1)-CO32-) was measured in three aqueous solutions containing 2.0 mol.L-1 Na2CO3 and 0.20, 0.42, or 0.92 mol.L-1 NaCl, respectively, from 122 to 1538 MPa at 22 degrees C using a moissanite anvil cell. The nu(1) Raman signal linearly shifted to higher wavenumbers with increasing pressure. Most importantly, the slope of nu(1)-CO32- Raman frequency shift (partial derivative nu(1)/partial derivative P) I was independent of NaCl concentration. Moreover, elevated ionic strength was found to shift the apparent outline of the carbonate peak toward low wavenumbers, possibly by increasing the proportion of the contact ion pair NaCO3-. Further investigations revealed no cross-interaction between the pressure effect and the ionic strength effect on the Raman spectra, possibly because the distribution of different ion-pair species in the carbonate equilibrium was largely pressure-independent. These results suggested that the ionic strength should be incorporated as an additional constraint for measuring the internal pressure of various solution-based systems. Combining the nu(1)-CO32- Raman frequency slope with the pressure herein with the values for the temperature or the ionic strength dependencies determined from previous studies, we developed an empirical equation that can be used to estimate the pressure of carbonate-bearing aqueous solutions.
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页数:9
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