Department of Environmental Chemistry (IDAEA-CSIC), Barcelona, Catalunya, Spain.
Department of Environmental Chemistry (IDAEA-CSIC), Barcelona, Catalunya, Spain; Aix Marseille Univ, University de Toulon, CNRS, IRD, MIO UM 110, Marseille, France.
Sci Total Environ. 2018 Sep 15;636:1109-1116. doi: 10.1016/j.scitotenv.2018.04.330. Epub 2018 May 3.
Soils are a major reservoir of semivolatile organic pollutants such as polychlorinated biphenyls (PCBs) and polycyclic aromatic hydrocarbons (PAHs), and exert a control on their atmospheric occurrence. We present here an assessment of the atmospheric occurrence and seasonality of soil/snow-air partitioning and exchange of PCBs, PAHs, hexachlorobenzene (HCB), and hexachlorocyclohexanes (HCHs) in the arctic city Tromsø, northern Norway. The fugacities of the organic pollutants in soils and snow were determined using a soil fugacity sampler by equilibrating the air concentrations with those in the surface soil/snow. The concentrations in soils did not show a significant seasonality. Conversely, the ambient air concentrations and the soil (or snow) fugacity showed a clear seasonality for PCBs, HCH, HCB and some PAHs, related to temperature. Fugacities in soil/snow were correlated with those in the ambient gas phase, suggesting a close seasonal air-soil/snow coupling. Generally, there was a net deposition or close to equilibrium conditions during the winter, which contrasts with the net volatilization observed during the warmer periods. The chemicals with lower octanol-air partition coefficients showed a larger tendency for being volatilized and thus remobilized from this coastal arctic environment. Conversely, the more hydrophobic compounds were close to air-soil/snow equilibrium or showed a net deposition.
土壤是半挥发性有机污染物(如多氯联苯(PCBs)和多环芳烃(PAHs))的主要储存库,并对其大气存在起到控制作用。我们在这里评估了北极城市特罗姆瑟(挪威北部)土壤/雪-气分配和 PCBs、PAHs、六氯苯(HCB)和六氯环己烷(HCHs)交换的大气出现和季节性。使用土壤逸度采样器通过使空气浓度与地表土壤/雪中的浓度平衡来确定土壤和雪中有机污染物的逸度。土壤中的浓度没有表现出明显的季节性。相反,环境空气浓度和土壤(或雪)逸度表现出明显的季节性,与温度有关,PCBs、HCH、HCB 和一些 PAHs 也是如此。土壤/雪中的逸度与环境气相中的逸度相关,表明季节性空气-土壤/雪耦合密切。通常,在冬季存在净沉积或接近平衡的条件,这与在温暖时期观察到的净挥发作用形成对比。具有较低辛醇-空气分配系数的化学物质表现出更大的挥发性,因此更容易从这个沿海北极环境中重新迁移。相反,疏水性更强的化合物更接近空气-土壤/雪平衡或表现出净沉积。