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Raman Micro-Spectroscopic Study of Sulfate Ion in the System Na2SO4 – H2O
引用本文:ZHU Dongliang,ZHU Ziang,PAN Junyi,DING Junying,NI Pei. Raman Micro-Spectroscopic Study of Sulfate Ion in the System Na2SO4 – H2O[J]. 《地质学报》英文版, 2015, 89(3): 887-893. DOI: 10.1111/1755-6724.12486
作者姓名:ZHU Dongliang  ZHU Ziang  PAN Junyi  DING Junying  NI Pei
作者单位:State Key Laboratory for Mineral Deposits Research, School of Earth Science and Engineering, Nanjing University, Nanjing 210093, China
摘    要:This work aims to quantify sulfate ion concentrations in the system Na2SO4-H2O using Raman micro-spectroscopy.Raman spectra of sodium sulfate solutions with known concentrations were collected at ambient temperature(293 K) and in the 500 cm1-4000 cm-1 spectral region.The results indicate that the intensity of the SO42- band increases with increasing concentrations of sulfate ion.A linear correlation was found between the concentration of SO42-(c) and parameter I1,which represents the ratio of the area of the SO42- band to that of the O-H stretching band of water(As/Aw):I1=-0.00102+0.01538 c.Furthermore,we deconvoluted the O-H stretching band of water(2800 cm-1-3800 cm-1) at 3232 and 3430 cm-1 into two sub-Gaussian bands,and then defined Raman intensity of the two sub-bands as ABi(3232 cm-1) and AB2(3430 cm-1),defined the full width of half maximum(FWHM) of the two sub-bands as WB1(3232 cm-1) and WB2(3430 cm-1).A linear correlation between the concentration of SO42-(c) and parameter I2,which represents the ratio of Raman intensity of SO42-(As)(in 981 cm-1) to(AB1+AB2),was also established:I2=-0.0111+0.3653 c.However,no correlations were found between concentration of SO42-(c) and FWHM ratios,which includes the ratio of FWHM of SO42-(Ws) to WB1 WB2 and WB1+B2(the sum of WB1 and WB2),suggesting that FWHM is not suitable for quantitative studies of sulfate solutions with Raman spectroscopy.A comparison of Raman spectroscopic studies of mixed Na2SO4 and NaCI solutions with a constant SO42- concentration and variable CI- concentrations suggest that the I parameter is affected by CI-,whereas the I2 parameter was not.Therefore,even if the solution is not purely Na2SO4-H2O,SO42- concentrations can still be calculated from the Raman spectra if the H2O band is deconvoluted into two sub-bands,making this method potentially applicable to analysis of natural fluid inclusions.

关 键 词:bands  stretching  FWHM  ambient  potentially  spectroscopic  purely  quantify  applicable  envelope
收稿时间:2014-10-16
修稿时间:2015-03-16

Raman Micro-Spectroscopic Study of Sulfate Ion in the System Na2SO4-H2O
ZHU Dongliang,ZHU Ziang,PAN Junyi,DING Junying and NI Pei. Raman Micro-Spectroscopic Study of Sulfate Ion in the System Na2SO4-H2O[J]. Acta Geologica Sinica (English Edition), 2015, 89(3): 887-893. DOI: 10.1111/1755-6724.12486
Authors:ZHU Dongliang  ZHU Ziang  PAN Junyi  DING Junying  NI Pei
Affiliation:State Key Laboratory for Mineral Deposits Research, School of Earth Science and Engineering, Nanjing University, Nanjing 210093, China
Abstract:This work aims to quantify sulfate ion concentrations in the system Na_2SO_4-H_2O using Raman micro-spectroscopy.Raman spectra of sodium sulfate solutions with known concentrations were collected at ambient temperature(293 K) and in the 500 cm~(_1)-4000 cm~(-1) spectral region.The results indicate that the intensity of the SO_4~(2-) band increases with increasing concentrations of sulfate ion.A linear correlation was found between the concentration of SO_4~(2-)(c) and parameter I_1,which represents the ratio of the area of the SO_4~(2-) band to that of the O-H stretching band of water(A_s/A_w):I_1=-0.00102+0.01538 c.Furthermore,we deconvoluted the O-H stretching band of water(2800 cm~(-1)-3800 cm~(-1)) at 3232 and 3430 cm~(-1) into two sub-Gaussian bands,and then defined Raman intensity of the two sub-bands as A_(Bi)(3232 cm~(-1)) and A_(B2)(3430 cm~(-1)),defined the full width of half maximum(FWHM) of the two sub-bands as W_(B1)(3232 cm~(-1)) and W_(B2)(3430 cm~(-1)).A linear correlation between the concentration of SO_4~(2-)(c) and parameter I_2,which represents the ratio of Raman intensity of SO_4~(2-)(A_s)(in 981 cm~(-1)) to(A_(B1)+A_(B2)),was also established:I_2=-0.0111+0.3653 c.However,no correlations were found between concentration of SO_4~(2-)(c) and FWHM ratios,which includes the ratio of FWHM of SO_4~(2-)(W_s) to W_(B1) W_(B2) and W_(B1+B2)(the sum of W_(B1) and W_(B2)),suggesting that FWHM is not suitable for quantitative studies of sulfate solutions with Raman spectroscopy.A comparison of Raman spectroscopic studies of mixed Na_2SO_4 and NaCI solutions with a constant SO_4~(2-) concentration and variable CI~- concentrations suggest that the I parameter is affected by CI~-,whereas the I_2 parameter was not.Therefore,even if the solution is not purely Na_2SO_4-H_2O,SO_4~(2-) concentrations can still be calculated from the Raman spectra if the H_2O band is deconvoluted into two sub-bands,making this method potentially applicable to analysis of natural fluid inclusions.
Keywords:Na2SO4-H2O system  Raman spectroscopy  quantitative analysis  fluid inclusion
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