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Hydroxyl radical in/on illuminated polar snow: formation rates, lifetimes, and steady-state concentrations

机译:照明的极地雪中/之上的羟基自由基:形成速率,寿命和稳态浓度

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pstrongAbstract./strong While the hydroxyl radical (supmoa?¢/mo/supOH) in the snowpack is likely a dominant oxidant for organic species and bromide, little is known about the kinetics or steady-state concentrations of supmoa?¢/mo/supOH on/in snow and ice. Here we measure the formation rate, lifetime, and concentration of supmoa?¢/mo/supOH for illuminated polar snow samples studied in the laboratory and in the field. Laboratory studies show that supmoa?¢/mo/supOH kinetics and steady-state concentrations are essentially the same for a given sample studied as ice and liquid; this is in contrast to other photooxidants, which show a concentration enhancement in ice relative to solution as a result of kinetic differences in the two phases. The average production rate of supmoa?¢/mo/supOH in samples studied at Summit, Greenland, is 5??times lower than the average measured in the laboratory, while the average supmoa?¢/mo/supOH lifetime determined in the field is 5 times higher than in the laboratory. These differences indicate that the polar snows we studied in the laboratory are affected by contamination, despite significant efforts to prevent this; our results suggest similar contamination may be a widespread problem in laboratory studies of ice chemistry. Steady-state concentrations of supmoa?¢/mo/supOH in clean snow studied in the field at Summit, Greenland, range from (0.8 to 3)a????a??10supa??15/supspan class="thinspace"/spanM, comparable to values reported for midlatitude cloud and fog drops, rain, and deliquesced marine particles, even though impurity concentrations in the snow samples are much lower. Partitioning of firn air supmoa?¢/mo/supOH to the snow grains will approximately double the steady-state concentration of snow-grain hydroxyl radical, leading to an average [supmoa?¢/mo/supOH] in near-surface, summer Summit snow of approximately 4a????a??10supa??15/supspan class="thinspace"/spanM. At this concentration, the supmoa?¢/mo/supOH-mediated lifetimes of organics and bromide in Summit snow grains are approximately 3??days and 7span class="thinspace"/spanh, respectively, suggesting that hydroxyl radical is a major oxidant for both species./p.
机译:> >摘要。虽然积雪堆中的羟基自由基( a?¢ OH)可能是有机物和溴化物的主要氧化剂,在雪和冰上/中 a?¢ OH的动力学或稳态浓度知之甚少。在这里,我们测量了在实验室和现场研究的照明极地雪样的形成速率,寿命和 a?¢ OH的浓度。实验室研究表明,对于所研究的给定样品(如冰和液体), a?¢ OH动力学和稳态浓度基本相同。这与其他光氧化剂相反,其他光氧化剂由于两相的动力学差异,使冰中的浓度相对于溶液增加。在格陵兰萨米特研究的样品中, a?¢ OH的平均生产率比实验室测量的平均值低5倍,而平均在现场确定的> a?¢ OH寿命是实验室的5倍。这些差异表明,尽管我们为防止这种情况付出了巨大的努力,但我们在实验室研究的极地雪却受到污染的影响。我们的结果表明,类似的污染可能是冰化学实验室研究中普遍存在的问题。在格陵兰萨米特地区的实地研究中,洁净雪中 a?mo OH的稳态浓度范围为(0.8至3)a? 10 a ?? 15 class =“ thinspace”> M,与中纬度云和雾滴,雨水和潮解性海洋颗粒的报告值相当,即使其中的杂质浓度较高雪样要低得多。燃烧的空气 a?¢ OH在雪粒中的分配将使雪粒羟基自由基的稳态浓度大约增加一倍,从而导致平均值[ < mo> a?¢ OH]在大约4a的夏季夏季顶峰雪中???? a ?? 10 a ?? 15 class =“ thinspace“> M。在此浓度下,Summit雪粒中的 a?¢ OH介导的有机物和溴化物的寿命大约为3-7天和7 class =“ thinspace”>

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