Hong Sungmin, Barbante Carlo, Boutron Claude, Gabrielli Paolo, Gaspari Vania, Cescon Paolo, Thompson Lonnie, Ferrari Christophe, Francou Bernard, Maurice-Bourgoin Laurence
Korea Polar Research Institute, Korea Ocean Research and Development Institute, Ansan, Seoul, Korea.
J Environ Monit. 2004 Apr;6(4):322-6. doi: 10.1039/b314251e. Epub 2004 Feb 9.
V, Co, Cu, Zn, As, Rb, Sr, Ag, Cd, Ba, Pb, Bi and U have been analysed by inductively coupled plasma sector field mass spectrometry in various sections of a dated snow/ice core drilled at an altitude of 6542 m on the Sajama ice cap in Bolivia. The analysed sections were dated from the Last Glacial Stage ( approximately 22,000 years ago), the Mid-Holocene and the last centuries. The observed variations of crustal enrichment factors (EFc) for the various metals show contrasting situations. For V, Co, Rb, Sr and U, EFc values close to unity are observed for all sections, then showing that these elements are mainly derived from rock and soil dust. For the other metals, clear time trends are observed, with a pronounced increase of EFc values during the 19th and 20th centuries. This increase shows evidence of metal pollution associated with human activity in South America. For Pb an important contribution was from gasoline additives. For metals such as Cu, Zn, Ag and Cd an important contribution was from metal production activities, with a continuous increase of production during the 20th century in countries such as Peru, Chile and Bolivia.
通过电感耦合等离子体质谱仪对在玻利维亚萨哈马冰帽海拔6542米处钻取的一根有年代测定的雪/冰芯的不同部分中的钒(V)、钴(Co)、铜(Cu)、锌(Zn)、砷(As)、铷(Rb)、锶(Sr)、银(Ag)、镉(Cd)、钡(Ba)、铅(Pb)、铋(Bi)和铀(U)进行了分析。所分析的部分可追溯到末次冰期(约22000年前)、全新世中期和过去几个世纪。各种金属的地壳富集因子(EFc)的观测变化呈现出不同的情况。对于钒、钴、铷、锶和铀,所有部分的EFc值都接近1,这表明这些元素主要源自岩石和土壤尘埃。对于其他金属,则观察到明显的时间趋势,在19世纪和20世纪期间EFc值显著增加。这种增加表明了与南美洲人类活动相关的金属污染。对于铅,一个重要来源是汽油添加剂。对于铜、锌、银和镉等金属,一个重要来源是金属生产活动,在20世纪,秘鲁、智利和玻利维亚等国的金属产量持续增加。