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首页> 外文期刊>Geophysical Research Letters >Particulate and water-soluble carbon measured in recent snow at Summit, Greenland
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Particulate and water-soluble carbon measured in recent snow at Summit, Greenland

机译:格陵兰萨米特峰最近积雪中测得的颗粒状碳和水溶性碳

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[1] Water-soluble organic carbon (WSOC), waterinsoluble particulate organic carbon (WIOC), and particulate elemental carbon (EC) were measured simultaneously for the first time on the Greenland Ice Sheet in surface snow and in a 3-meter snow pit. Snow pit concentrations reveal that, on average, WSOC makes up the majority (89%) of carbonaceous species, followed by WIOC (10%) and EC (1%). The enhancement of OC relative to EC (ratio 99: 1) in Greenland snow suggests that, along with atmospheric particulate matter, gaseous organics contribute to snow-phase OC. Comparison of summer surface snow concentrations in 2006 with past summer snow pit layers (2002 - 2005) found a significant depletion in WSOC (20 - 82%) and WIOC (46 - 65%) relative to EC for 3 of the 4 years. The apparent substantial loss of WSOC and WIOC in aged snow suggests that post-depositional processes, such as photochemical reactions, need to be considered in linking ice core records of organics to atmospheric concentrations.
机译:[1]首次在格陵兰冰原上在表雪和3米雪坑中同时测量了水溶性有机碳(WSOC),水不溶性颗粒有机碳(WIOC)和颗粒元素碳(EC)。 。雪坑浓度显示,平均而言,WSOC占碳质物种的大部分(89%),其次是WIOC(10%)和EC(1%)。格陵兰雪中OC相对于EC的增强(比率99:1)表明,气态有机物与大气颗粒物一起构成了雪相OC。将2006年夏季地面雪浓度与过去夏季雪坑层(2002年至2005年)进行比较,发现在4年中的3年中,WSOC(20-82%)和WIOC(46-65%)显着减少。在老雪中WSOC和WIOC的明显损失表明,在将有机物的冰芯记录与大气浓度联系起来时,需要考虑沉积后过程,例如光化学反应。

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