Developments of non-destructive quantification for trace elements in high-pressure run-products by proton beam
Developments of non-destructive quantification for trace elements in high-pressure run-products by proton beam
批准号:
09554027
负责人:
KATO Takumi
金额:
$5.5万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for Scientific Research (B).
财政年份:
1997
资助国家:
日本
项目状态:
已结题
起止时间:
1997 至 2000
中文摘要
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英文摘要
This project aims to study and develop non-destructive quantitative analytical method of trace elements in high-pressure run-products by PIXE (proton-induced X-ray emission) method. We have developed : 1) a micro-proton beam line for high-pressure product analyses and sample chamber for microanalyses equipped with microscope, micro-driving stage, and two solid state detectors for light and heavy element analyses ; 2) analytical procedures for high-pressure run-products ; 3) quantification of trace elements in single fluid inclusions buried in mineral matrix. A 4 MeV proton micro-beam of 2 nA, 50 μm in size was obtained in the developed beam line by a new quadropole magnet. By using PIXE at the new beam line, high-pressure run-product, graphite-diamond mixtures and basaltic glasses maintained at 2000 C and 7.7 GPa, was analyzed. The graphite contained almost the elements derived from basaltic glass as interlayer impurities, indicating concentration of many elements in graphite under the high-pressure condition. Natural diamonds include usually graphite, so that analyses of the graphite can provide a chemical information of diamond-growth. In addition, trace elements ranged from 10 to 1000 μg/g in single fluid inclusions were determined with ±15 % relative precision by using the developed quantification. At the present measurements, a few μg/g elements were detected in the fluid inclusion with 200 μm in diameter, corresponding to several-picograms (〜10^<-12> g) detection of elements in inclusions.
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M.Kurosawa et al.: "Quantitative trace element analyses of silicate reterence materials and a stainless steel using the proton microprobe"Chemical Geology. 160. 241-250 (1999)
M.Kurosawa 等人:“使用质子微探针对硅酸盐保留材料和不锈钢进行定量痕量元素分析”化学地质学。
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T.KATO and N.NAKATA: "MELTING RELATION OF Mg_2SiO_4-Mg_3Al_2Si_3O_R" Phys.Earth Planet.Inter.(1998)
T.KATO 和 N.NAKATA:“Mg_2SiO_4-Mg_3Al_2Si_3O_R 的熔化关系”Phys.Earth Planet.Inter.(1998)
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T.Kato, N.Nakata, E.Ohtani, and K.Onuma: "Melting experiments on the forsterite-pyrope system at 8 and 13.5 GPa"Physics of the Earth and Planetary Interiors. 107. 97-102 (1998)
T.Kato、N.Nakata、E.Ohtani 和 K.Onuma:“镁橄榄石-镁铝榴石系统在 8 和 13.5 GPa 下的熔化实验”地球和行星内部物理学。
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T.Kubo, E.Ohtani, T.Kato, T.Shinmei, and K.Fujino: "Effect of water on the α-β transformation kinetics in San Carlos Olivine"Science. 281. 85-87 (1998)
T.Kubo、E.Ohtani、T.Kato、T.Shinmei 和 K.Fujino:“水对圣卡洛斯橄榄石中 α-β 转化动力学的影响”《科学》281. 85-87 (1998)。
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M.Kurosawa,J.L.Campbell,W.J.Teesdale,H.Ohyi,Y.Deguchi,and S.Murao: "Quantitative trace element analyses of silicate reference materials and a stainless steel using the proton microprobe"Chemical Geology. 160. 241-250 (1999)
M.Kurosawa、J.L.Campbell、W.J.Teesdale、H.Ohyi、Y.Deguchi 和 S.Murao:“使用质子微探针对硅酸盐标准材料和不锈钢进行定量痕量元素分析”化学地质学。
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共 37 条
Changes of deep Earth materials and high pressure materials under high pressures
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批准号:10045023
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项目类别:Grant-in-Aid for Scientific Research (B).
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资助金额:$2.82万
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财政年份:1998
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负责人:KATO Takumi
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依托单位:
Element partitioning and diffusion in silicate high pressure phases
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批准号:08454151
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项目类别:Grant-in-Aid for Scientific Research (B)
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资助金额:$4.8万
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财政年份:1996
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负责人:KATO Takumi
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依托单位:
海外基金