{"title":"白石的水热处理;白石的水热处理;Hydrothermal treatment of pectolite","authors":"Ryohei Otsuka, Takabumi Sakamoto, Shigeru Suzuki, Shinji Shinoda, Hitoshi Koshimizu","doi":"10.2465/GKK1952.14.SPECIAL1_170","DOIUrl":null,"url":null,"abstract":"In order to investigate the genesis of stevensite and “hydrated talc” experimentally, naturally occurring pectolite was treated hydrothermally with 1, 2 and 4 normal magnesium chloride solution and with basic magnesium carbonate for various Mg (in basic magnesium carbonate)/Si (in pectolite) molecular ratios ranging from 0.1 to 1.5. The products were examined by means of X-ray diffraction, thermal analysis, transmission and scanning electron microscopy and chemical analysis. As a result, it was found that pectolite alters to stevensite (Mg/Si=0.1-0.3), stevensite and serpentine (Mg/Si=0.5-1.0) and serpentine (Mg/Si=1.5) by hydrothermal treatment with basic magnesium carbonate treatment. On the other hand, it altered to “hydrated talc” and small amount of serpentine by magnesium chloride solution treatment, as reported previously (Sakamoto et al, 1975a). Some considerations were made on the mechanism of the conversion process of pectolite to these layer silicate minerals.","PeriodicalId":242743,"journal":{"name":"Journal of the Mineralogical Society of Japan","volume":"160 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"ペクトライトの水熱処理;ペクトライトの水熱処理;Hydrothermal treatment of pectolite\",\"authors\":\"Ryohei Otsuka, Takabumi Sakamoto, Shigeru Suzuki, Shinji Shinoda, Hitoshi Koshimizu\",\"doi\":\"10.2465/GKK1952.14.SPECIAL1_170\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"In order to investigate the genesis of stevensite and “hydrated talc” experimentally, naturally occurring pectolite was treated hydrothermally with 1, 2 and 4 normal magnesium chloride solution and with basic magnesium carbonate for various Mg (in basic magnesium carbonate)/Si (in pectolite) molecular ratios ranging from 0.1 to 1.5. The products were examined by means of X-ray diffraction, thermal analysis, transmission and scanning electron microscopy and chemical analysis. As a result, it was found that pectolite alters to stevensite (Mg/Si=0.1-0.3), stevensite and serpentine (Mg/Si=0.5-1.0) and serpentine (Mg/Si=1.5) by hydrothermal treatment with basic magnesium carbonate treatment. On the other hand, it altered to “hydrated talc” and small amount of serpentine by magnesium chloride solution treatment, as reported previously (Sakamoto et al, 1975a). Some considerations were made on the mechanism of the conversion process of pectolite to these layer silicate minerals.\",\"PeriodicalId\":242743,\"journal\":{\"name\":\"Journal of the Mineralogical Society of Japan\",\"volume\":\"160 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1900-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of the Mineralogical Society of Japan\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.2465/GKK1952.14.SPECIAL1_170\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of the Mineralogical Society of Japan","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.2465/GKK1952.14.SPECIAL1_170","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
摘要
为了实验研究橄榄石和“水合滑石”的成因,用1、2和4普通氯化镁溶液和碱式碳酸镁对天然pectolite进行了水热处理,使Mg(在碱式碳酸镁中)/Si(在pectolite中)的分子比在0.1 ~ 1.5之间。采用x射线衍射、热分析、透射电镜、扫描电镜和化学分析等方法对产物进行了表征。结果表明,经碱式碳酸镁水热处理后,榴辉岩可转变为闪辉石(Mg/Si=0.1 ~ 0.3)、闪辉石和蛇纹石(Mg/Si=0.5 ~ 1.0)和蛇纹石(Mg/Si=1.5)。另一方面,如先前报道,经氯化镁溶液处理后,它变成了“水合滑石粉”和少量蛇纹石(Sakamoto et al, 1975a)。并对其转化为这些层状硅酸盐矿物的机理进行了探讨。
ペクトライトの水熱処理;ペクトライトの水熱処理;Hydrothermal treatment of pectolite
In order to investigate the genesis of stevensite and “hydrated talc” experimentally, naturally occurring pectolite was treated hydrothermally with 1, 2 and 4 normal magnesium chloride solution and with basic magnesium carbonate for various Mg (in basic magnesium carbonate)/Si (in pectolite) molecular ratios ranging from 0.1 to 1.5. The products were examined by means of X-ray diffraction, thermal analysis, transmission and scanning electron microscopy and chemical analysis. As a result, it was found that pectolite alters to stevensite (Mg/Si=0.1-0.3), stevensite and serpentine (Mg/Si=0.5-1.0) and serpentine (Mg/Si=1.5) by hydrothermal treatment with basic magnesium carbonate treatment. On the other hand, it altered to “hydrated talc” and small amount of serpentine by magnesium chloride solution treatment, as reported previously (Sakamoto et al, 1975a). Some considerations were made on the mechanism of the conversion process of pectolite to these layer silicate minerals.