Gioia Rosalinda, Nizzetto Luca, Lohmann Rainer, Dachs Jordi, Temme Christian, Jones Kevin C
Centre for Chemicals Management and Department of Environmental Science, Lancaster Environment Centre, Lancaster University, Lancaster LA1 4YQ, UK.
Environ Sci Technol. 2008 Mar 1;42(5):1416-22. doi: 10.1021/es071432d.
Air and seawater samples were collected on board the RV Polarstern during a cruise from Bremerhaven, Germany to Cape Town, South Africa from October-November 2005. Broad latitudinal trends were observed with the lowest sigma27PCB air concentration (approximately 10 pg m(-3)) in the South Atlantic and the highest (approximately 1000 pg m(-3)) off the west coast of Africa. Sigma(ICES)PCBs ranged from 3.7 to 220 pg m(-3) in air samples and from 0.071 to 1.7 pg L(-1) in the dissolved phase seawater samples. Comparison with other data from cruises in the Atlantic Ocean since 1990 indicate little change in air concentrations over the remote open ocean. The relationship of gas-phase partial pressure with temperature was examined using the Clausius-Clapeyron equation; significant temperature dependencies were found for all PCBs over the South Atlantic, indicative of close air-water coupling. There was no temperature dependence for atmospheric PCBs overthe North Atlantic, where concentrations were controlled by advection of contaminated air masses. Due to large uncertainties in the Henry's Law Constant (HLC), fugacity fractions and air-water exchange fluxes were estimated using different HLCs reported in the literature. These suggest that conditions are close to air-water equilibrium for most of the ocean, but net deposition is dominating over volatilization in parts of the transect. Generally, the tri- and tetrachlorinated homologues dominated the total flux (> 70%). Total PCB fluxes (28, 52, 118, 138, and 153) ranged from -7 to 0.02 ng m(-2) day(-1).
2005年10月至11月,在从德国不来梅港到南非开普敦的航行过程中,“极地星”号研究船上采集了空气和海水样本。观察到明显的纬度趋势,南大西洋的σ27多氯联苯空气浓度最低(约10皮克/立方米),而非洲西海岸外的浓度最高(约1000皮克/立方米)。空气样本中的σ(ICES)多氯联苯含量在3.7至220皮克/立方米之间,溶解相海水样本中的含量在0.071至1.7皮克/升之间。与1990年以来大西洋其他航次的数据比较表明,偏远公海的空气浓度变化不大。使用克劳修斯-克拉佩龙方程研究了气相分压与温度的关系;在南大西洋,所有多氯联苯都存在明显的温度依赖性,表明空气-水耦合紧密。北大西洋大气中的多氯联苯不存在温度依赖性,其浓度受污染气团平流控制。由于亨利定律常数(HLC)存在很大不确定性,因此根据文献中报道的不同HLC估算了逸度分数和气-水交换通量。这些结果表明,大部分海洋的条件接近气-水平衡,但在部分断面,净沉降占主导地位,超过了挥发。一般来说,三氯和四氯同系物在总通量中占主导地位(>70%)。多氯联苯总通量(28、52、118、138和153)范围为-7至0.02纳克/平方米·天。