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    Identification of Nuclei and Concentrations of Chemical Species in Snow Crystals Sampled at the South Pole

    Source: Journal of the Atmospheric Sciences:;1976:;Volume( 033 ):;issue: 005::page 833
    Author:
    Kumai, Motoi
    DOI: 10.1175/1520-0469(1976)033<0833:IONACO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A total of 380 electron micrographs and electron diffraction patterns of 93 snow crystal nuclei were analyzed in this observation. The nuclei were identified as mainly clay minerals and sodium chloride particles. The clay mineral nuclei were illite 20%, kaoline 8%, halloysite 4%, verniiculite 3%, and related minerals 24%. For the other nuclei, sodium chloride accounted for 20%, and unidentified nuclei accounted for 5%. Fifteen percent of the snow crystals did not appear to have nuclei. Therefore, all nuclei found in snow crystals were terrestrial substances from oceans and continents. The mass of nuclei was from 10?16 to 10?12 for both clay minerals and sodium chloride. The shapes of snow crystals were single bullets, combinations of bullets, and hexagonal hollow columns. The snow crystals formed at temperatures from ?30 to ?35°C. The snow crystal diameters were from 0.1 to 1.0 mm, and the crystal mass was from 10?8 to 10 ?5 g The mean mass concentration of sodium chloride in snow crystals was 40.6 ppb and that of clay minerals was 15.4 ppb. The sodium chloride nucleus concentration coincided within the experimental error with data taken from the chemical analysis of the South Pole snow cover made by several workers. It was concluded that most of the sodium chloride contained in the South Pole snow cover was due to the sodium chloride nuclei of snow crystals.
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      Identification of Nuclei and Concentrations of Chemical Species in Snow Crystals Sampled at the South Pole

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4152916
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    contributor authorKumai, Motoi
    date accessioned2017-06-09T14:18:50Z
    date available2017-06-09T14:18:50Z
    date copyright1976/05/01
    date issued1976
    identifier issn0022-4928
    identifier otherams-17063.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152916
    description abstractA total of 380 electron micrographs and electron diffraction patterns of 93 snow crystal nuclei were analyzed in this observation. The nuclei were identified as mainly clay minerals and sodium chloride particles. The clay mineral nuclei were illite 20%, kaoline 8%, halloysite 4%, verniiculite 3%, and related minerals 24%. For the other nuclei, sodium chloride accounted for 20%, and unidentified nuclei accounted for 5%. Fifteen percent of the snow crystals did not appear to have nuclei. Therefore, all nuclei found in snow crystals were terrestrial substances from oceans and continents. The mass of nuclei was from 10?16 to 10?12 for both clay minerals and sodium chloride. The shapes of snow crystals were single bullets, combinations of bullets, and hexagonal hollow columns. The snow crystals formed at temperatures from ?30 to ?35°C. The snow crystal diameters were from 0.1 to 1.0 mm, and the crystal mass was from 10?8 to 10 ?5 g The mean mass concentration of sodium chloride in snow crystals was 40.6 ppb and that of clay minerals was 15.4 ppb. The sodium chloride nucleus concentration coincided within the experimental error with data taken from the chemical analysis of the South Pole snow cover made by several workers. It was concluded that most of the sodium chloride contained in the South Pole snow cover was due to the sodium chloride nuclei of snow crystals.
    publisherAmerican Meteorological Society
    titleIdentification of Nuclei and Concentrations of Chemical Species in Snow Crystals Sampled at the South Pole
    typeJournal Paper
    journal volume33
    journal issue5
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1976)033<0833:IONACO>2.0.CO;2
    journal fristpage833
    journal lastpage841
    treeJournal of the Atmospheric Sciences:;1976:;Volume( 033 ):;issue: 005
    contenttypeFulltext
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