2014
DOI: 10.2116/bunsekikagaku.63.351
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Concentrations of Chemical Constituents in Glaze at the Summit of Mt. Kajigamori in Kochi Prefecture, Shikoku Region, Japan

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Cited by 2 publications
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“…Shi et al 15 reported that the levels of carbonaceous materials and mineral particles were comparable in aerosols from urban areas, suburban areas and the clean air district in Beijing, but that coal fly ash was higher in the clean air district. Recently, Imai et al [16][17][18][19] classified the ISPs included in insoluble rime, hard rime, and snow into five categories, with their chemical components corresponding to their area of generation: AREA-A, Huabei-type; AREA-B, Dongbei-type; AREA-B2, Korean peninsula-type; AREA-C, Heilongjiang-Russia-type, and AREA-D, Japan-type. When the winter monsoon is predominant, the S(-II) compounds were transported from northeast China together with various components of coal combustion exhaust from similar areas of ISP generation.…”
Section: Introductionmentioning
confidence: 99%
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“…Shi et al 15 reported that the levels of carbonaceous materials and mineral particles were comparable in aerosols from urban areas, suburban areas and the clean air district in Beijing, but that coal fly ash was higher in the clean air district. Recently, Imai et al [16][17][18][19] classified the ISPs included in insoluble rime, hard rime, and snow into five categories, with their chemical components corresponding to their area of generation: AREA-A, Huabei-type; AREA-B, Dongbei-type; AREA-B2, Korean peninsula-type; AREA-C, Heilongjiang-Russia-type, and AREA-D, Japan-type. When the winter monsoon is predominant, the S(-II) compounds were transported from northeast China together with various components of coal combustion exhaust from similar areas of ISP generation.…”
Section: Introductionmentioning
confidence: 99%
“…The aim of this work is to use WDXRF to provide a methodology for the sulfur speciation of airborne particles, including the origin and/or fractions of S(VI) and S(-II), determined from the combination of (i) the ratio of the elemental components of the filtrates and (ii) the chemical shift of the S-Kα line. [17][18][19][20] The application of this methodology is interesting in terms of its applicability to other elements.…”
Section: Introductionmentioning
confidence: 99%