Graduate School of Oceanography, University of Rhode Island, Narragansett, Rhode Island 02882-1197, USA.
Environ Sci Technol. 2010 May 15;44(10):3832-8. doi: 10.1021/es9039852.
Surface ocean and lower atmosphere samples were collected on the R/V Revelle during a scientific cruise from San Diego, CA to New Zealand via Samoa and the South Pacific Gyre (SPG) from 12/2006 to 1/2007. Samples were analyzed for polychlorinated biphenyls (PCBs) and hexachlorobenzene (HCB). summation operator(ICES)PCBs gaseous concentrations (ICES: International Council for the Exploration of the Sea) ranged from 28-103 pg m(-3) in the northern hemisphere (NH) and 1.5-36 pg m(-3) in the southern hemisphere (SH), whereas dissolved seawater concentrations were between 0.2-15 pg L(-1) in the NH and 0.3-7.8 pg L(-1) in the SH. Both gas (PCBs) and dissolved phase concentrations (PCBs) displayed highest concentrations near North America and lowest in the SPG. In the NH, HCB ranged from 42-89 pg m(-3), higher than the average in the SH (31 pg m(-3)), while HCB were comparable in both hemispheres (NH: 0.4-1.6 pg L(-1), SH: 0.4-0.8 pg L(-1)). Fugacity ratio calculations suggest PCBs were volatilizing from surface waters to the overlying atmosphere, and air-water exchange fluxes were approximately 0.5 to approximately 30.4 ng m(-2) d(-1). This is the first study reporting the degassing of PCBs from the open ocean into the air. Previous studies deduced net deposition of PCBs into the Atlantic and Arctic Oceans. As has been observed for other oceans, HCB was at/near air-water equilibrium. A mass balance model was used to interpret the short-term variations in PCBs in the SPG, which was not observed for HCB. It is suggested that hydroxyl radical depletion reaction and air-water gas exchange together controlled the variation in PCBs.
在 2006 年 12 月至 2007 年 1 月期间,“Revelle”号科学考察船从加利福尼亚州圣地亚哥出发,经萨摩亚和南太平洋环流(SPG)前往新西兰,采集了表层海洋和低层大气样本。这些样本用于分析多氯联苯(PCBs)和六氯苯(HCB)。北半球(NH)的大气总 PCBs(ICES:国际海洋勘探理事会)浓度范围为 28-103 pg m(-3),南半球(SH)浓度范围为 1.5-36 pg m(-3),而溶解在海水中的 PCBs 浓度范围为 0.2-15 pg L(-1)在 NH 和 0.3-7.8 pg L(-1)在 SH。无论是在气相(PCBs)还是在溶解相中(PCBs),PCBs 的浓度均在靠近北美洲的地区最高,在 SPG 中的浓度最低。在 NH,HCB的浓度范围为 42-89 pg m(-3),高于 SH 的平均值(31 pg m(-3)),而在两个半球(NH:0.4-1.6 pg L(-1),SH:0.4-0.8 pg L(-1))中,HCB的浓度相当。逸度比计算表明 PCBs 正在从地表水挥发到上层大气中,空气-水交换通量约为 0.5 至 30.4 ng m(-2) d(-1)。这是第一项报道 PCBs 从开阔海域排放到大气中的研究。先前的研究推断出 PCBs 正以净沉积的形式进入大西洋和北冰洋。与其他海洋一样,HCB 处于或接近气-水平衡状态。一个质量平衡模型被用于解释 SPG 中PCBs的短期变化,但 HCB 没有出现这种情况。据推测,羟基自由基消耗反应和空气-水气体交换共同控制了PCBs的变化。