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    Measurements of 7Be and 210Pb in Rain, Snow, and Hail

    Source: Journal of Applied Meteorology:;1994:;volume( 033 ):;issue: 007::page 869
    Author:
    Gaffney, Jeffrey S.
    ,
    Orlandini, Kent A.
    ,
    Marley, Nancy A.
    ,
    Popp, Carl J.
    DOI: 10.1175/1520-0450(1994)033<0869:MOAIRS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Measurements of the levels of 7Be and 210Pb are reported for rain, snow, and hail samples taken at Argonne, Illinois, and Socorro, New Mexico. These natural radioisotopes are indicators of the sources of the aerosols contributing materials to the precipitation samples. The data presented indicate that the more soluble 7Be is enriched in the precipitation samples with respect to 210Pb, as compared to the ratios of these radioisotopes found in aerosol samples. Use of the 210Po/210Pb activity ratios as an internal clock indicated that the aerosols contributing to the precipitation ranged in age from 10 to 47 days. Levels of 7Be ranged from 11 to 55 pCi L?1 for the samples, with the highest levels in a stratus precipitation event and in a thunderstorm with the lowest wet deposition rate. These results are discussed with regard to the potential for use of these radioisotopes in the determination of stratospheric-tropospheric mixing and in their geochemical usage as indicators of sedimentation rates.
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      Measurements of 7Be and 210Pb in Rain, Snow, and Hail

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4147361
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    contributor authorGaffney, Jeffrey S.
    contributor authorOrlandini, Kent A.
    contributor authorMarley, Nancy A.
    contributor authorPopp, Carl J.
    date accessioned2017-06-09T14:04:56Z
    date available2017-06-09T14:04:56Z
    date copyright1994/07/01
    date issued1994
    identifier issn0894-8763
    identifier otherams-12063.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4147361
    description abstractMeasurements of the levels of 7Be and 210Pb are reported for rain, snow, and hail samples taken at Argonne, Illinois, and Socorro, New Mexico. These natural radioisotopes are indicators of the sources of the aerosols contributing materials to the precipitation samples. The data presented indicate that the more soluble 7Be is enriched in the precipitation samples with respect to 210Pb, as compared to the ratios of these radioisotopes found in aerosol samples. Use of the 210Po/210Pb activity ratios as an internal clock indicated that the aerosols contributing to the precipitation ranged in age from 10 to 47 days. Levels of 7Be ranged from 11 to 55 pCi L?1 for the samples, with the highest levels in a stratus precipitation event and in a thunderstorm with the lowest wet deposition rate. These results are discussed with regard to the potential for use of these radioisotopes in the determination of stratospheric-tropospheric mixing and in their geochemical usage as indicators of sedimentation rates.
    publisherAmerican Meteorological Society
    titleMeasurements of 7Be and 210Pb in Rain, Snow, and Hail
    typeJournal Paper
    journal volume33
    journal issue7
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1994)033<0869:MOAIRS>2.0.CO;2
    journal fristpage869
    journal lastpage873
    treeJournal of Applied Meteorology:;1994:;volume( 033 ):;issue: 007
    contenttypeFulltext
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