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首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Nonmethane hydrocarbons in surface waters, their sea-air fluxes and impact on OH in the marine boundary layer during the First Aerosol Characterization Experiment (ACE 1)
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Nonmethane hydrocarbons in surface waters, their sea-air fluxes and impact on OH in the marine boundary layer during the First Aerosol Characterization Experiment (ACE 1)

机译:在第一个气溶胶表征实验(ACE 1)期间,地表水中的非甲烷碳氢化合物,它们的海气通量以及对海洋边界层中的OH的影响

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摘要

Concentrations of six abundant alkanes (propane, 2-methylpropane, butane, 2-methyl-butane, pentane, cyclopentane) and three abundant alkenes (2-methylpropene, cis-2-butene, 1,3-butadiene) were determined in air equilibrated with surface seawater in real time during the International Global Atmospheric Chemistry First Aerosol Characterization Experiment (ACE 1) campaign to the Southern Ocean in November-December 1995. Concentrations in ocean surface water inferred from these measurements generally lay within the ranges observed by other investigators at other times in other regions of the global ocean. Concentrations tended to decrease with increasing latitude. Comparison with a limited number of dissolved organic carbon (DOC) data obtained during transit from Hawaii to Hobart, Tasmania, suggested that higher hydrocarbon concentrations were associated with higher DOC levels. During the ACE 1 intensive study period west and south of Tasmania the differences in NMHC concentrations among the three major water masses sampled, while frequently significant, were not related in a simple direct or inverse way to surface water temperature, concentrations of nitrate, chlorophyll a, or dimethylsulfide, or to calculated sea-to-air transfer velocity or solar radiation intensity. The only correlations that showed some consistency within water masses were with temperature (negative) and nitrate (positive), an essential nutrient for phytoplankton growth. Deduced sea-to-air fluxes indicated modes open-ocean emissions of C_3-C_5 NMHC in this part of the global ocean. Assuming that the deduced fluxes were balanced by reaction with hydroxyl radical, OH, we estimated that the nine measured NMHC together accounted for negligible removal of OH compared to that due to the dominant OH + CO reaction and about 5 times less than that due to the DMS + OH reaction in the region of the marine boundary layer studied during ACE 1.
机译:在平衡的空气中测定了六种丰富的烷烃(丙烷,2-甲基丙烷,丁烷,2-甲基丁烷,戊烷,环戊烷)和三种丰富的烯烃(2-甲基丙烯,顺-2-丁烯,1,3-丁二烯)的浓度在1995年11月至12月向南大洋进行的全球全球大气化学首次气溶胶表征实验(ACE 1)活动中,实时获取了地表海水。根据这些测量结果推断出的海表水浓度通常在其他研究人员观察到的范围内其他时间在全球海洋的其他地区。随着纬度的增加,浓度趋于降低。与从夏威夷到塔斯马尼亚州霍巴特的运输过程中获得的有限数量的溶解有机碳(DOC)数据进行的比较表明,较高的烃浓度与较高的DOC水平有关。在塔斯马尼亚州西部和南部的ACE 1强化研究期间,虽然采样的三个主要水团中的NMHC浓度差异通常很显着,但它们与地表水温,硝酸盐,叶绿素a的浓度没有简单的直接或相反的关系。或二甲硫,或计算出的海对空传输速度或太阳辐射强度。在水团中显示出一定一致性的唯一相关性是温度(负)和硝酸盐(正),这是浮游植物生长所必需的营养素。推算出的海对空通量表明全球海洋这部分地区C_3-C_5 NMHC的海洋公开排放模式。假设推导的通量是通过与羟基自由基OH的反应平衡的,我们估计,与主要的OH + CO反应相比,测得的9种NMHC在一起对OH的去除率可忽略不计,并且比由OH + CO反应引起的去除率低约5倍。在ACE 1期间研究了海洋边界层区域的DMS + OH反应。

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