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    Background Silver Concentrations in Illinois Precipitation and River Water

    Source: Journal of Applied Meteorology:;1975:;volume( 014 ):;issue: 002::page 217
    Author:
    Gatz, Donald F.
    DOI: 10.1175/1520-0450(1975)014<0217:BSCIIP>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: This work was undertaken to measure background silver in Illinois precipitation in the absence of any known seeding operations in on near Illinois. The rainfall-weighted mean concentration in samples from several stations was 73 ng l?1. This is somewhat higher than has been found in unseeded precipitation in other parts of North America, but not high enough to preclude wind-blown soil dust as a primary source.
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      Background Silver Concentrations in Illinois Precipitation and River Water

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4232266
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    contributor authorGatz, Donald F.
    date accessioned2017-06-09T17:38:04Z
    date available2017-06-09T17:38:04Z
    date copyright1975/03/01
    date issued1975
    identifier issn0021-8952
    identifier otherams-8848.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4232266
    description abstractThis work was undertaken to measure background silver in Illinois precipitation in the absence of any known seeding operations in on near Illinois. The rainfall-weighted mean concentration in samples from several stations was 73 ng l?1. This is somewhat higher than has been found in unseeded precipitation in other parts of North America, but not high enough to preclude wind-blown soil dust as a primary source.
    publisherAmerican Meteorological Society
    titleBackground Silver Concentrations in Illinois Precipitation and River Water
    typeJournal Paper
    journal volume14
    journal issue2
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1975)014<0217:BSCIIP>2.0.CO;2
    journal fristpage217
    journal lastpage221
    treeJournal of Applied Meteorology:;1975:;volume( 014 ):;issue: 002
    contenttypeFulltext
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