Synthesis and alteration of 3-octahedral clay minerals.
Synthesis and alteration of 3-octahedral clay minerals.
批准号:
62540612
负责人:
HAYASHI Hisato
金额:
$1.22万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for General Scientific Research (C)
财政年份:
1987
资助国家:
日本
项目状态:
已结题
起止时间:
1987 至 1989
中文摘要
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英文摘要
Kaolinite and 3-octahedral smectites were synthesized under several hydrothermal conditions from diatomaceous earth, which occurs at Takanosu, Akita Prefecture, and from rice husk ash.1. Synthesis of kaolinite from diatomaceous earth. Kaolinite has been prepared from dispersions of diatomaceous earth in aqueous solution of AlCl_3 at 170-230゚C. Kaolinite began to produce at 170゚C for 3 hours. Its yield in synthetic products was estimated by DTA and X-ray methods. For 180 hours, kaolinite was produced about 10 % at 170゚C, about 30 % at 200゚C, and 60 % at 230゚C.2. Synthesis of smectite from diatomaceous earth. (1) Mg-smectite. Mg-smectite has been prepared from the HCl treated diatomaceous earth in aqueous solutions of MgCl_2 at 200゚C in various Si : Mg molar ratios ranging from 8 : 8-3. Smectites were produces from the starting materials with Si : Mg (molar ratio) = 8 : 6. Smectites and talcs were produced from the starting materials with Si : Mg (molar ratio) = 8 : 8. Smectites and serpentine minerals were produced from the starting materials with Si : Mg (molar ratio) = 8 : 4.5. The starting materials with Si : Mg (molar ratio) = 8 : 3 altered spectites having very broad basal reflection. (2) Ni-seectite. Diatomaceous earth was ground at 10 hours (10-h) and 30 hours (30-h). Ni-smectite has been prepared from dispersions [Si : Mg Li (solar ratio) = 8 : 5.33 : 0.66] of the ground diatomaceous earth in aqueous solutions of NiCl_2 (pH 13.50) at 200゚C. Smectite began to produce from 3 hours treatment. Smectites were produced easier the starting material ground 30 hours (30-h) than that of 10 hours ground (10-h).3. Synthesis of 3-octahedral smectite from rice husk ash. Rice husk ash can be used as a superior siliceous material for production of smectite. The best condition is as follows ; Temperature of calcination : 450゚C, Si : Mg : Li (solar ratio) = 8 : 5.34 : 0.66, pH of the dispersion before reaction : 13.2-13.5, Reaction time : 4 days.
期刊论文(4)
专著(0)
科研奖励(0)
会议论文
H. HAYASHI: "On clay minerals in soil from Yurihara, Akita." Report Res. Inst. Natural Resources, Mining College, Akita University. No. 53, 33-40 (1988).
H. HAYASHI:“关于秋田县尤里原土壤中的粘土矿物。”
DOI:
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影响因子:
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作者:
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通讯作者:
林久人: "珪藻土を用いた粘土鉱物の合成" 秋田大学鉱山学部研究報告. No.10. 101-107 (1989)
Hisato Hayashi:“利用硅藻土合成粘土矿物”秋田大学矿业学院研究报告第10. 101-107号(1989年)。
DOI:
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作者:
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通讯作者:
林久人: "秋田県由利原の土壌粘土鉱物について" 秋田大学鉱山学部附属資源地学研究施設報告. NO.53. 33-40 (1988)
Hisato Hayashi:“关于秋田县由利原市的土壤粘土矿物”,秋田大学矿业学院资源地质研究所的报告,第 53-40 号(1988 年)。
DOI:
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发表时间:
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影响因子:
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作者:
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通讯作者:
Hydrothermal alteration and formation of clay minerals.
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批准号:63303006
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项目类别:Grant-in-Aid for Co-operative Research (A)
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资助金额:$5.06万
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财政年份:1988
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负责人:HAYASHI Hisato
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依托单位:
国内基金
海外基金
新型滤波器综合技术-直接综合技术(Direct synthesis Technique)的研究及应用
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批准号:61671111
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项目类别:面上项目
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资助金额:58.0万元
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批准年份:2016
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负责人:肖飞
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依托单位: