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Experimental study of sulfur dioxide interaction with silicates and aluminosilicates at temperatures of 650 and 850°C
Investigation of sulfur dioxiderock interaction is a fundamental geochemical problem because SO2 is one of the major components of the gas phase emitted during volcanic activity, both eruptive and fumarolic. In recent years, the problem of the volcanic emission of SO2 and its interaction with rocks...
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| Published in: | Geochemistry international 2010-10, Vol.48 (10), p.1039-1046 |
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| Main Authors: | , , , , |
| Format: | Article |
| Language: | English |
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| cites | cdi_FETCH-LOGICAL-c2305-4f4eefa6c2104b3e67a590bc6f74a4a37217d3ffd1e2ec9b84ba5cf86727d8ec3 |
| container_end_page | 1046 |
| container_issue | 10 |
| container_start_page | 1039 |
| container_title | Geochemistry international |
| container_volume | 48 |
| creator | Li, E. Yu Chareev, D. A. Shilobreeva, S. N. Grichuk, D. V. Tyutyunnik, O. A. |
| description | Investigation of sulfur dioxiderock interaction is a fundamental geochemical problem because SO2 is one of the major components of the gas phase emitted during volcanic activity, both eruptive and fumarolic. In recent years, the problem of the volcanic emission of SO2 and its interaction with rocks has attracted much attention of planetologists owing to the discovery of considerable con tents of sulfur compounds in the atmospheres of Venus and the Jovian satellite Io. Sodium sulfate is probably one of the main minerals on the surface of Io [1]. On the basis of laboratory modeling, Johnson and Burnett [2] showed that sodium sulfate can be produced by the interaction of SO2with silicate rocks. |
| doi_str_mv | 10.1134/S0016702910100095 |
| format | article |
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Yu ; Chareev, D. A. ; Shilobreeva, S. N. ; Grichuk, D. V. ; Tyutyunnik, O. A.</creator><creatorcontrib>Li, E. Yu ; Chareev, D. A. ; Shilobreeva, S. N. ; Grichuk, D. V. ; Tyutyunnik, O. A.</creatorcontrib><description>Investigation of sulfur dioxiderock interaction is a fundamental geochemical problem because SO2 is one of the major components of the gas phase emitted during volcanic activity, both eruptive and fumarolic. In recent years, the problem of the volcanic emission of SO2 and its interaction with rocks has attracted much attention of planetologists owing to the discovery of considerable con tents of sulfur compounds in the atmospheres of Venus and the Jovian satellite Io. Sodium sulfate is probably one of the main minerals on the surface of Io [1]. On the basis of laboratory modeling, Johnson and Burnett [2] showed that sodium sulfate can be produced by the interaction of SO2with silicate rocks.</description><identifier>ISSN: 0016-7029</identifier><identifier>EISSN: 1556-1968</identifier><identifier>DOI: 10.1134/S0016702910100095</identifier><language>eng</language><publisher>Dordrecht: SP MAIK Nauka/Interperiodica</publisher><subject>Aluminum silicates ; Earth and Environmental Science ; Earth Sciences ; Geochemistry ; Rocks ; Short Communications ; Silica ; Silicates ; Sodium sulfate ; Sulfates ; Sulfur ; Sulfur content ; Sulfur dioxide ; Temperature effects</subject><ispartof>Geochemistry international, 2010-10, Vol.48 (10), p.1039-1046</ispartof><rights>Pleiades Publishing, Ltd. 2010</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c2305-4f4eefa6c2104b3e67a590bc6f74a4a37217d3ffd1e2ec9b84ba5cf86727d8ec3</citedby><cites>FETCH-LOGICAL-c2305-4f4eefa6c2104b3e67a590bc6f74a4a37217d3ffd1e2ec9b84ba5cf86727d8ec3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Li, E. 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On the basis of laboratory modeling, Johnson and Burnett [2] showed that sodium sulfate can be produced by the interaction of SO2with silicate rocks.</description><subject>Aluminum silicates</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geochemistry</subject><subject>Rocks</subject><subject>Short Communications</subject><subject>Silica</subject><subject>Silicates</subject><subject>Sodium sulfate</subject><subject>Sulfates</subject><subject>Sulfur</subject><subject>Sulfur content</subject><subject>Sulfur dioxide</subject><subject>Temperature effects</subject><issn>0016-7029</issn><issn>1556-1968</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2010</creationdate><recordtype>article</recordtype><recordid>eNp1kE1OwzAQhS0EEqVwAHYW-8A4_kuWqCo_UiUWwDpynTG4SpNiO9DeijNwMlKKBBJiNZp5730jPUJOGZwzxsXFPQBTGvKSAQOAUu6REZNSZaxUxT4ZbeVsqx-SoxgXAELwUo_I63S9wuCX2CbT0Jj6ekM7R2PfuD7Q2ndrXyP1bcJgbPJdS998eqbRN96ahJGatqam6Ze-7X4dE024HMAm9WHYB6KS8OUtJHy8T47JgTNNxJPvOSaPV9OHyU02u7u-nVzOMptzkJlwAtEZZXMGYs5RaSNLmFvltDDCcJ0zXXPnaoY52nJeiLmR1hVK57ou0PIxOdtxV6F76TGmatH1oR1eVgVIobiUbDCxncmGLsaArloNjZiwqRhU23arP-0OmXyXiYO3fcLwA_4_9Ak13X3h</recordid><startdate>201010</startdate><enddate>201010</enddate><creator>Li, E. 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| fulltext | fulltext |
| identifier | ISSN: 0016-7029 |
| ispartof | Geochemistry international, 2010-10, Vol.48 (10), p.1039-1046 |
| issn | 0016-7029 1556-1968 |
| language | eng |
| recordid | cdi_proquest_journals_805463551 |
| source | Springer Nature |
| subjects | Aluminum silicates Earth and Environmental Science Earth Sciences Geochemistry Rocks Short Communications Silica Silicates Sodium sulfate Sulfates Sulfur Sulfur content Sulfur dioxide Temperature effects |
| title | Experimental study of sulfur dioxide interaction with silicates and aluminosilicates at temperatures of 650 and 850°C |
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