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Determination of volatiles in magma by micro-gas-analysis of melt inclutions in phenocrysts

Determination of volatiles in magma by micro-gas-analysis of melt inclutions in phenocrysts
斑晶中熔体包裹体的微量气体分析测定岩浆中的挥发物
批准号:
63470031
负责人:
KUSAKABE Minoru
金额:
$3.26万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for General Scientific Research (B)
财政年份:
1988
资助国家:
日本
项目状态:
已结题
起止时间:
1988 至 1989

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中文摘要
翻译
斑晶中的玻璃包裹体可被视为“淬火岩浆”的一部分,通过微量气体分析可获得玛玛的挥发分。组装了激光加热气体提取和QMS分析系统,用于在100 μ m尺度上测定玻璃中的H_2O和CO_2含量。用光束直径为10 μ m、能量为7 W的ND-YAG激光器在真空中熔化玻璃。放出的气体收集在液体空气冷阱中。用捕集器分离CO_2和H_2O。为了避免H_2O吸附在引出管壁上,H_2O与加热的铀金属反应被还原成H_2。H_2和CO_2用静态操作的QMS测定。H_2O和CO_2的线性范围分别为0.04-99 ng和0.01-18 ng。根据坑径和坑深估算了释放H_2O和CO_2的坑体积。熔融的玻璃的质量由凹坑体积和玻璃的密度计算。利用马里亚纳海槽玄武岩的玻璃质边缘(H_2O= 1.37wt%,CO_2=326 ppm)进行了实验研究。直径为90 ~ 300 μ m、深度为15 ~ 110 μ m的蚀坑中,H_2O的释放量为30-120 ng,CO_2的释放量为0.08-1.2 ng。微量元素分析结果为1.4 <plus-minus>± 0.2(S.E.)wt%的H_2O和390 <plus-minus>40(S.E.)ppm的CO_2浓度。采用本技术,可以获得直径约为100 mm的熔融包裹体。假设夹杂物具有上述气体组成,则可以分析150 μ m的气体。
英文摘要
The volatile compositions in maama can be obtained by micro-gas-analysis of glass inclusions in phenocrysts which can be regarded as a part of a "quenched magma". The system for gas extraction by laser heating followed by QMS analysis was assembled to determine H_2O and CO_2 contents in glasses on a 100 mum scale. A ND-YAG laser with a beam diameter of 10 mum And the energy of 7W was used to melt glasses in vacuum. The evolved gases were collected in a liquid air cold trap. CO_2 was separated from H_2O by trap work. In order to avoid the absorption of H_2O onto walls of the extraction line, H_2O was reduced to H_2 by reaction with a heated uranium metal. The resulting H_2 and CO_2 were determined by a statically operated QMS. The linear calibration curves were obtained in the range between 0.04-99 ng for H_2O and 0.01-18 ng for CO_2. The pit volume which released H_2O and CO_2 was estimated from the diameter and depth of the pit. The mass of the glass melted was calculated from the pit volume and the density of the glass. The gas concentrations were obtained by dividing the amount of H_2 and CO_2 determined by the mass of the glass melted.Glassy margin of the Mariana Trough basalt (H_2O=1.37 wt% and CO_2=326 ppm) was used to test this technique. The amount of the evolved gases from each pit with a size ranging from 90 to 300 mum in diameter and from 15 to 110 mum in depth was between 30-120 ng for H_2O and between 0.08-1.2 ng for CO_2. The microanalysis showed 1.4<plus-minus>0.2 (S.E.) wt% for H_2O and 390<plus-minus>40 (S.E.) ppm for CO_2 based on 6 independent analyses. With the present technique, a melt inclusion with a diameter of ca. 150 mum can be analyzed, assuming the inclusion has the above gas composition.
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斎藤元治: 火山(第2集). 34. (1989)
齐藤元晴:火山(第 2 卷)。(1989 年)。
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斎藤元治,日下部実: "火山噴火におけるマグマ中の揮発性物質の挙動-斑晶中のガラス包有物の分析に基づくアプロ-チ-" 火山(第2集). 34. 275-293 (1989)
Motoharu Saito、Minoru Kusakabe:“火山喷发期间岩浆中挥发性物质的行为 - 基于斑晶中玻璃包裹体分析的方法”《火山》(第 2 卷)。275-293 (1989)。
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Genji Saitoh and Minoru Kusakabe: "Behavior of magmatic volatiles in volcanic eruptions based on glass inclusion analysis" Bull. Volcanol. Soc. Japan. 34(4). 275-293 (1989)
Genji Saitoh 和 Minoru Kusakabe:“基于玻璃包裹体分析的火山喷发中岩浆挥发物的行为”公牛。
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斎藤元治,日下部実: "火山噴火におけるマグマ中の揮発性物質の挙動ー斑晶中のガラス包有物の分析に基づくアプロ-チー" 火山(第2集). 34. 275-293 (1989)
Motoharu Saito、Minoru Kusakabe:“火山喷发期间岩浆中挥发性物质的行为 - 基于斑晶玻璃包裹体分析的方法”《火山》(第 2 卷)。275-293 (1989)。
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Lake Nyos in dual agony-An assessment of the limnic eruption and dam collapse-
  • 批准号:
    16403012
  • 项目类别:
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  • 资助金额:
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  • 财政年份:
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    14340172
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    Grant-in-Aid for Scientific Research (B)
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    2002
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Continuous monitoring of water chemistry of Lake Nyos using an automated CDT and satellite data
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    13573013
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  • 资助金额:
    $8.9万
  • 财政年份:
    2001
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  • 依托单位:
ARE MAGMAS BENEATH THE CAMEROON VOLCANIC LINE ENRICHED IN CARBON DIOXIDE? -RELATIONSHIP WITH THE LAKE NYOS-TYPE GAS DISASTERS-
  • 批准号:
    10041121
  • 项目类别:
    Grant-in-Aid for Scientific Research (B).
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海外基金