Study on smectite-to-illite transformation mechanism
Study on smectite-to-illite transformation mechanism
批准号:
16540437
负责人:
INOUE Atsuyuki
金额:
$2.37万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for Scientific Research (C)
财政年份:
2004
资助国家:
日本
项目状态:
已结题
起止时间:
2004 至 2006
中文摘要
成功完成了利用Kakkonda地热田IT-2岩心样品对蒙脱石-伊利石转化机理的研究,并在国内外期刊上发表了5篇论文。今年,我们在Guadeloupe的Bouillante地热田进行了莫脱石到贝德尔石的转化,作为我们目前的蒙脱石到伊利石转化机制模型的应用。详细的XRD, FTIR和化学分析清楚地表明,随着深度和温度的增加,蒙脱土通过两层间的层结从蒙脱土转变为贝德尔石。然而,基于碳和氧同位素数据分析,这种转变不是由热控制的贝德尔化解释的,而是由与粘土降水相关的溶液组成控制的。从我们目前的蒙脱石-伊利石转化机制模型来看,这一结论是合理的。这一结果已提交给美国矿物学家与法国同事合著的一篇文章。下一步,了解粘土矿物在水岩相互作用中的降水动力学是很重要的。通过实验工作来了解硅酸盐离子在溶液中的行为是不容易的。因此,我们开始研究氢氧化铁矿物的结晶过程,特别是阴离子在FeOOH矿物形成中的作用,而不是硅酸盐的结晶。我们在这个课题上有了有趣的结果,并发表了两篇论文。
英文摘要
Study on smectite-to-illite transformation mechanism, using the core samples IT-2 from the Kakkonda geothermal field, has been successfully completed and the results have been published in five papers of international and national journals. In this year, we worked on motmorillonite-to-beidellite transformation at Bouillante geothermal field, Guadeloupe as an application of our current model of smectite-to-illite transformation mechanism. Detailed XRD, FTIR and chemical analyses clearly demonstrated a transition from montmorillonite to beidellite with increasing depth and temperature via interstratification of the two layers. However this transition was not explained by a thermally controlled beidellitization but control of solution composition related to the precipitation of clays, based on the carbon and oxygen isotopes data analysis. This conclusion is reasonably accepted from the viewpoint of our current model of smectite-to-illite transformation mechanism. This result has been submitted to an article of American Mineralogist co-authored with French colleagues.In the next step, it is important to understand the precipitation dynamics of clay minerals in water-rock interaction. It is not easy that experimental works undertakes to understand the behavior of silicate ions in solution. Instead of crystallization of silicates, thus, we started working on crystallization process of iron oxyhydroxide minerals, especially focusing on understanding of the role of anions in the formation of FeOOH minerals. We have interested results on this subject and published two papers.
期刊论文(36)
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Formation of illite-smectite mixed-layer minerals in hydrothermally altered volcanic rocks : Integration of geological, fluid chemical, isotopic, XRD, and TEM evidence at Kakkonda geothermal system
热液蚀变火山岩中伊利石-蒙脱石混合层矿物的形成:Kakkonda 地热系统地质、流体化学、同位素、XRD 和 TEM 证据的整合
DOI:
--
发表时间:
2005
期刊:
Clay Science 12(Supplement)
影响因子:
--
作者:
[T.Murakami, A.Inoue, B.Lanson, A.Meunier, D.Beaufort, A.Inoue]
通讯作者:
A.Inoue
K-ray absorption fine structure spectroscopy study of arsenate adsorption on schwertmannite
施威特曼石吸附砷酸盐的K射线吸收精细结构光谱研究
DOI:
--
发表时间:
2007
期刊:
CP882, X-ray Absorption Fine structure - XAFS13
影响因子:
--
作者:
[M.Sakamaki, H.Takahashi, T.Konishi, A.Inoue, T.Fujikawa]
通讯作者:
T.Fujikawa
高塩濃度,高アルカリ環境における粘土鉱物の生成と変化-放射性廃棄物地層処分環境におけるベントナイト緩衝材の変質に関連して-
高盐、高碱性环境下粘土矿物的形成与变化——与放射性废物地质处置环境中膨润土缓冲材料的蚀变有关——
DOI:
--
发表时间:
2004
期刊:
粘土科学 43巻
影响因子:
--
作者:
[Nakano, N., 井上厚行]
通讯作者:
井上厚行
Stacking defects and long-period polytypes in kaolin minerals from a hydrothermal deposit
热液矿床高岭土矿物的堆积缺陷和长周期多型
DOI:
--
发表时间:
2005
期刊:
European Journal of Mineralogy 17
影响因子:
--
作者:
[T.Kogure, A.Inoue]
通讯作者:
A.Inoue
Determination of defect structures in kaolin minerals by high-resolution transmission electron microscopy(HRTEM)
高岭土矿物缺陷结构的高分辨率透射电子显微镜(HRTEM)测定
DOI:
--
发表时间:
2005
期刊:
American Mineralogist 90巻
影响因子:
--
作者:
[Kogure, T., Inoue, A.]
通讯作者:
A.
共 13 条
Development of geothermometer suitable for estimating the formation temperature of trioctahedral chlorite and its application
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批准号:21540492
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项目类别:Grant-in-Aid for Scientific Research (C)
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资助金额:$2.91万
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财政年份:2009
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负责人:INOUE Atsuyuki
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依托单位:
Crystal growth of illitic minerals in open systems
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批准号:06453003
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项目类别:Grant-in-Aid for Scientific Research (B)
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资助金额:$4.74万
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财政年份:1994
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负责人:INOUE Atsuyuki
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依托单位:
海外基金