Department of Applied Environmental Science (ITM) and ‡Bolin Centre for Climate Research, Stockholm University , 10691, Stockholm Sweden.
Environ Sci Technol. 2014 Jun 17;48(12):6719-25. doi: 10.1021/es500736q. Epub 2014 Jun 4.
There is a wealth of studies of polychlorinated biphenyls (PCB) in surface water and biota of the Arctic Ocean. Still, there are no observation-based assessments of PCB distribution and inventories in and between the major Arctic Ocean compartments. Here, the first water column distribution of PCBs in the central Arctic Ocean basins (Nansen, Amundsen, and Makarov) is presented, demonstrating nutrient-like vertical profiles with 5-10 times higher concentrations in the intermediate and deep water masses than in surface waters. The consistent vertical profiles in all three Arctic Ocean basins likely reflect buildup of PCBs transported from the shelf seas and from dissolution and/or mineralization of settling particles. Combined with measurement data on PCBs in other Arctic Ocean compartments collected over the past decade, the total Arctic Ocean inventory of ∑7PCB was estimated to 182 ± 40 t (±1 standard error of the mean), with sediments (144 ± 40 t), intermediate (5 ± 1 t) and deep water masses (30 ± 2 t) storing 98% of the PCBs in the Arctic Ocean. Further, we used hydrographic and carbon cycle parametrizations to assess the main pathways of PCBs into and out of the Arctic Ocean during the 20th century. River discharge appeared to be the major pathway for PCBs into the Arctic Ocean with 115 ± 11 t, followed by ocean currents (52 ± 17 t) and net atmospheric deposition (30 ± 28 t). Ocean currents provided the only important pathway out of the Arctic Ocean, with an estimated cumulative flux of 22 ± 10 t. The observation-based inventory of ∑7PCB of 182 ± 40 t is consistent with the contemporary inventory based on cumulative fluxes for ∑7PCB of 173 ± 36 t. Information on the concentration and distribution of PCBs in the deeper compartments of the Arctic Ocean improves our understanding of the large-scale fate of POPs in the Arctic and may also provide a means to test and improve models used to assess the fate of organic pollutants in the Arctic.
北极海洋表层水和生物群中多氯联苯(PCB)的研究已有很多。然而,对于主要北极海洋隔室之间和内部的 PCB 分布和库存,仍没有基于观测的评估。在这里,首次呈现了北极中央海洋盆地(南森、阿蒙森和马卡罗夫)中 PCB 的水柱分布情况,这些分布呈现出类似于营养物的垂直分布模式,在中层和深层水体中的浓度比表层水高出 5-10 倍。这三个北极海洋盆地中一致的垂直分布模式可能反映了从陆架海运输以及沉降颗粒的溶解和/或矿化而积累的 PCB。结合过去十年中在其他北极海洋隔室中测量的 PCB 数据,估计整个北极海洋的∑7PCB 总库存为 182 ± 40 t(平均值±1 个标准误差),其中沉积物(144 ± 40 t)、中层(5 ± 1 t)和深层水体(30 ± 2 t)储存了北极海洋中 98%的 PCB。此外,我们使用水文学和碳循环参数化来评估 20 世纪 PCB 进入和离开北极海洋的主要途径。河流排放似乎是 PCB 进入北极海洋的主要途径,为 115 ± 11 t,其次是海流(52 ± 17 t)和净大气沉积(30 ± 28 t)。海流是离开北极海洋的唯一重要途径,估计累积通量为 22 ± 10 t。基于观测的∑7PCB 库存为 182 ± 40 t,与基于累积通量的当代∑7PCB 库存(173 ± 36 t)一致。有关北极海洋深层隔室中 PCB 的浓度和分布的信息提高了我们对北极 POPs 大规模命运的理解,也可能提供一种手段来测试和改进用于评估北极有机污染物命运的模型。