{"title":"热液中氧化硫物种的拉曼光谱","authors":"Christian Schmidt , Sandro Jahn","doi":"10.1016/j.jvolgeores.2024.108146","DOIUrl":null,"url":null,"abstract":"<div><p>Raman spectroscopic determination of sulfur species molalities in hydrothermal fluids requires correct assignment and knowledge of the scattering efficiencies of Raman bands. Therefore, we studied the Raman spectra of NaHSO<sub>4</sub> and H<sub>2</sub>SO<sub>4</sub> solutions experimentally to 700 °C, and of Na<sub>2</sub>SO<sub>4</sub>, NaHSO<sub>4</sub>, H<sub>2</sub>SO<sub>4</sub>, and H<sub>2</sub>SO<sub>3</sub> solutions by ab initio molecular dynamics simulation at 727 °C. The results indicate that the scattering efficiencies of the <em>ν</em><sub>s</sub>(SO<sub>3</sub>), ν<sub>as</sub>(SO<sub>3</sub>), and ν(S–OH) Raman bands of HSO<sub>4</sub><sup>−</sup>(aq) depend on the H<sup>+</sup> activity. The asymmetric shape of the ν<sub>s</sub>(SO<sub>3</sub>) Raman band of HSO<sub>4</sub><sup>−</sup>(aq) becomes more symmetric with increasing temperature, which correlates with decreasing hydrogen bonding in the molecular environment. Proton activity and ion pairing do not have a large effect on the change in the band asymmetry with temperature, and a resonance effect on the band shape is not observed. Therefore, we attribute the asymmetric shape of the ν<sub>s</sub>(SO<sub>3</sub>) Raman band of HSO<sub>4</sub><sup>−</sup>(aq) mostly to hydrogen bonding of the proton in the H–OSO<sub>3</sub><sup>−</sup> molecule with water in its environment. The AIMD simulations clarify assignments of Raman bands of H<sub>2</sub>SO<sub>4</sub><sup>0</sup>, specifically to ν<sub>s</sub>(SO<sub>2</sub>) and ν<sub>as</sub>(SO<sub>2</sub>) at ∼1140 cm<sup>−1</sup> and ∼1370 cm<sup>−1</sup>, to ν<sub>s</sub>(SO<sub>4</sub>) and ν<sub>as</sub>(SO<sub>4</sub>) at ∼970 cm<sup>−1</sup> and ∼1220 cm<sup>−1</sup>, and to ν<sub>s</sub>(S–(OH)<sub>2</sub>) and ν<sub>as</sub>(S–(OH)<sub>2</sub>) at ∼750 cm<sup>−1</sup> and ∼840 cm<sup>−1</sup>. In addition, the experiments showed that diamond is not inert to H<sub>2</sub>SO<sub>4</sub> at high temperatures as reduction of S(VI) to S(IV) produces SO<sub>2</sub><sup>0</sup> and oxidation of diamond generates CO<sub>2</sub><sup>0</sup>.</p></div>","PeriodicalId":54753,"journal":{"name":"Journal of Volcanology and Geothermal Research","volume":"454 ","pages":"Article 108146"},"PeriodicalIF":2.4000,"publicationDate":"2024-08-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S0377027324001380/pdfft?md5=440e4ed03a45bd5364ba185af336b023&pid=1-s2.0-S0377027324001380-main.pdf","citationCount":"0","resultStr":"{\"title\":\"Raman spectra of oxidized sulfur species in hydrothermal fluids\",\"authors\":\"Christian Schmidt , Sandro Jahn\",\"doi\":\"10.1016/j.jvolgeores.2024.108146\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Raman spectroscopic determination of sulfur species molalities in hydrothermal fluids requires correct assignment and knowledge of the scattering efficiencies of Raman bands. Therefore, we studied the Raman spectra of NaHSO<sub>4</sub> and H<sub>2</sub>SO<sub>4</sub> solutions experimentally to 700 °C, and of Na<sub>2</sub>SO<sub>4</sub>, NaHSO<sub>4</sub>, H<sub>2</sub>SO<sub>4</sub>, and H<sub>2</sub>SO<sub>3</sub> solutions by ab initio molecular dynamics simulation at 727 °C. The results indicate that the scattering efficiencies of the <em>ν</em><sub>s</sub>(SO<sub>3</sub>), ν<sub>as</sub>(SO<sub>3</sub>), and ν(S–OH) Raman bands of HSO<sub>4</sub><sup>−</sup>(aq) depend on the H<sup>+</sup> activity. The asymmetric shape of the ν<sub>s</sub>(SO<sub>3</sub>) Raman band of HSO<sub>4</sub><sup>−</sup>(aq) becomes more symmetric with increasing temperature, which correlates with decreasing hydrogen bonding in the molecular environment. Proton activity and ion pairing do not have a large effect on the change in the band asymmetry with temperature, and a resonance effect on the band shape is not observed. Therefore, we attribute the asymmetric shape of the ν<sub>s</sub>(SO<sub>3</sub>) Raman band of HSO<sub>4</sub><sup>−</sup>(aq) mostly to hydrogen bonding of the proton in the H–OSO<sub>3</sub><sup>−</sup> molecule with water in its environment. The AIMD simulations clarify assignments of Raman bands of H<sub>2</sub>SO<sub>4</sub><sup>0</sup>, specifically to ν<sub>s</sub>(SO<sub>2</sub>) and ν<sub>as</sub>(SO<sub>2</sub>) at ∼1140 cm<sup>−1</sup> and ∼1370 cm<sup>−1</sup>, to ν<sub>s</sub>(SO<sub>4</sub>) and ν<sub>as</sub>(SO<sub>4</sub>) at ∼970 cm<sup>−1</sup> and ∼1220 cm<sup>−1</sup>, and to ν<sub>s</sub>(S–(OH)<sub>2</sub>) and ν<sub>as</sub>(S–(OH)<sub>2</sub>) at ∼750 cm<sup>−1</sup> and ∼840 cm<sup>−1</sup>. In addition, the experiments showed that diamond is not inert to H<sub>2</sub>SO<sub>4</sub> at high temperatures as reduction of S(VI) to S(IV) produces SO<sub>2</sub><sup>0</sup> and oxidation of diamond generates CO<sub>2</sub><sup>0</sup>.</p></div>\",\"PeriodicalId\":54753,\"journal\":{\"name\":\"Journal of Volcanology and Geothermal Research\",\"volume\":\"454 \",\"pages\":\"Article 108146\"},\"PeriodicalIF\":2.4000,\"publicationDate\":\"2024-08-05\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://www.sciencedirect.com/science/article/pii/S0377027324001380/pdfft?md5=440e4ed03a45bd5364ba185af336b023&pid=1-s2.0-S0377027324001380-main.pdf\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Volcanology and Geothermal Research\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0377027324001380\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Volcanology and Geothermal Research","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0377027324001380","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
Raman spectra of oxidized sulfur species in hydrothermal fluids
Raman spectroscopic determination of sulfur species molalities in hydrothermal fluids requires correct assignment and knowledge of the scattering efficiencies of Raman bands. Therefore, we studied the Raman spectra of NaHSO4 and H2SO4 solutions experimentally to 700 °C, and of Na2SO4, NaHSO4, H2SO4, and H2SO3 solutions by ab initio molecular dynamics simulation at 727 °C. The results indicate that the scattering efficiencies of the νs(SO3), νas(SO3), and ν(S–OH) Raman bands of HSO4−(aq) depend on the H+ activity. The asymmetric shape of the νs(SO3) Raman band of HSO4−(aq) becomes more symmetric with increasing temperature, which correlates with decreasing hydrogen bonding in the molecular environment. Proton activity and ion pairing do not have a large effect on the change in the band asymmetry with temperature, and a resonance effect on the band shape is not observed. Therefore, we attribute the asymmetric shape of the νs(SO3) Raman band of HSO4−(aq) mostly to hydrogen bonding of the proton in the H–OSO3− molecule with water in its environment. The AIMD simulations clarify assignments of Raman bands of H2SO40, specifically to νs(SO2) and νas(SO2) at ∼1140 cm−1 and ∼1370 cm−1, to νs(SO4) and νas(SO4) at ∼970 cm−1 and ∼1220 cm−1, and to νs(S–(OH)2) and νas(S–(OH)2) at ∼750 cm−1 and ∼840 cm−1. In addition, the experiments showed that diamond is not inert to H2SO4 at high temperatures as reduction of S(VI) to S(IV) produces SO20 and oxidation of diamond generates CO20.
期刊介绍:
An international research journal with focus on volcanic and geothermal processes and their impact on the environment and society.
Submission of papers covering the following aspects of volcanology and geothermal research are encouraged:
(1) Geological aspects of volcanic systems: volcano stratigraphy, structure and tectonic influence; eruptive history; evolution of volcanic landforms; eruption style and progress; dispersal patterns of lava and ash; analysis of real-time eruption observations.
(2) Geochemical and petrological aspects of volcanic rocks: magma genesis and evolution; crystallization; volatile compositions, solubility, and degassing; volcanic petrography and textural analysis.
(3) Hydrology, geochemistry and measurement of volcanic and hydrothermal fluids: volcanic gas emissions; fumaroles and springs; crater lakes; hydrothermal mineralization.
(4) Geophysical aspects of volcanic systems: physical properties of volcanic rocks and magmas; heat flow studies; volcano seismology, geodesy and remote sensing.
(5) Computational modeling and experimental simulation of magmatic and hydrothermal processes: eruption dynamics; magma transport and storage; plume dynamics and ash dispersal; lava flow dynamics; hydrothermal fluid flow; thermodynamics of aqueous fluids and melts.
(6) Volcano hazard and risk research: hazard zonation methodology, development of forecasting tools; assessment techniques for vulnerability and impact.