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Year-round record of dissolved and particulate metals in surface snow at Dome Concordia (East Antarctica)

机译:圆顶康科迪亚(南极东部)地表雪中溶解金属和颗粒金属的全年记录

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摘要

From January to December 2010, surface snow samples were collected with monthly resolution at the Concordia station (75 degrees 06'S, 123 degrees 20'E), on the Antarctic plateau, and analysed for major and trace elements in both dissolved and particulate (i.e. insoluble particles, >0.45 pm) phase. Additional surface snow samples were collected with daily resolution, for the determination of sea-salt sodium and not-sea-salt calcium, in order to support the discussion on the seasonal variations of trace elements. Concentrations of alkaline and alkaline-earth elements were higher in winter (April-October) than in summer (November-March) by a factor of 1.2-3.3, in agreement with the higher concentration of sea-salt atmospheric particles reaching the Antarctic plateau during the winter. Similarly, trace elements were generally higher in winter by a factor of 1.2-1.5, whereas Al and Fe did not show any significant seasonal trend.
机译:2010年1月至2010年12月,在南极高原的Concordia站(南纬75度06',东经123度20')以每月分辨率采集地表雪样品,并分析了溶解和颗粒(即不溶)中的主要和微量元素颗粒,> 0.45 pm)相。为了每日分析微量元素的季节性变化,我们以每日的分辨率收集了额外的地表雪样品,用于测定海盐钠和非海盐钙。冬季(4月至10月)的碱和碱土元素浓度比夏季(11月至3月)的浓度高1.2-3.3倍,这与南极高原在2002年到达南极高原的海盐大气颗粒的浓度较高相符。冬天。同样,冬季的微量元素含量通常高出1.2-1.5,而铝和铁没有显示出明显的季节性趋势。

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