Lamont-Doherty Earth Observatory of Columbia University , Palisades, New York 10964, United States.
Environ Sci Technol. 2014;48(3):1451-7. doi: 10.1021/es4035655. Epub 2014 Jan 13.
A unique ∼ 10 year record of the lead isotopic composition of airborne insoluble particulate matter deposited in central Greenland was extracted from recent snow layers at NorthGRIP (75.1°N, 042.3°W; elevation 2,959 m), spanning the years 1989-2001. Comparison with lead isotopic signatures of both natural and anthropogenic northern hemisphere (NH) aerosol sources shows that human activities must have accounted for most of the insoluble lead deposited on Greenland during the late 1990 s, exceeding by far the natural contribution from large Asian mineral dust inputs. Lead isotopes imply predominance with time of European/Canadian sources over U.S.-derived lead, with an admixed signature typical of Chinese anthropogenic lead sources. The relative contribution of the latter shows a marked seasonal increase during spring. Our record also suggests that China's weight in the overall supply of insoluble pollutants deposited on Greenland was growing over the past decade of the 20th century.
从格陵兰中部 NorthGRIP (75.1°N,042.3°W;海拔 2959 米)的近期雪层中提取了一段独特的约 10 年的记录,记录了沉积在格陵兰的空气中不可溶解的颗粒物质的铅同位素组成,时间跨度为 1989 年至 2001 年。与来自自然和人为的北半球(NH)气溶胶源的铅同位素特征进行比较表明,在 20 世纪 90 年代末,人类活动必定是在格陵兰沉积的大部分不可溶解铅的主要来源,远远超过了来自亚洲大型粉尘输入的自然贡献。铅同位素表明,欧洲/加拿大来源的铅随着时间的推移超过了美国来源的铅,而且存在典型的中国人为铅源的混合特征。后者的相对贡献在春季呈现出明显的季节性增加。我们的记录还表明,在 20 世纪的过去十年中,中国在沉积在格陵兰的不可溶解污染物的总供应中的份额不断增加。