National Institute of Advanced Industrial Science and Technology (AIST), 16-1 Onogawa, Tsukuba, Ibaraki 305-8569, Japan.
Environ Int. 2013 May;55:25-32. doi: 10.1016/j.envint.2013.02.005. Epub 2013 Mar 19.
Perfluorinated alkyl substances (PFASs) have been found widely in the environment including remote marine locations. The mode of transport of PFASs to remote marine locations is a subject of considerable scientific interest. Assessment of distribution of PFASs in wet precipitation samples (i.e., rainfall and snow) collected over an area covering continental, coastal, and open ocean will enable an understanding of not only the global transport but also the regional transport of PFASs. Nevertheless, it is imperative to examine the representativeness and suitability of wet precipitation matrixes to allow for drawing conclusions on the transport PFASs. In this study, we collected wet precipitation samples including rainfall, surface snow, and snow core from several locations in Japan to elucidate the suitability of these matrixes for describing local and regional transport of PFASs. Rain water collected at various time intervals within a single rainfall event showed high fluxes of PFASs in the first 1-mm deposition. The scavenging rate of PFASs by wet deposition varied depending on the fluorocarbon chain length of PFAS. The depositional fluxes of PFASs measured for continental (Tsukuba, Japan) and open ocean (Pacific Ocean, 1000km off Japanese coast) locations were similar, on the order of a few nanograms per square meter. The PFAS profiles in "freshly" deposited and "aged" (deposited on the ground for a few days) snow samples taken from the same location varied considerably. The freshly deposited snow represents current atmospheric profiles of PFASs, whereas the aged snow sample reflects sequestration of local sources of PFASs from the atmosphere. Post-depositional modifications in PFAS profiles were evident, suggesting reactions of PFASs on snow/ice surface. Transformation of precursor chemicals such as fluorotelomer alcohols into perfluoroalkylcarboxylates is evident on snow surface. Snow cores have been used to evaluate time trends of PFAS contamination in remote environments. Snow collected at various depths from a core of up to 7.7m deep, at Mt. Tateyama (2450m), Japan, showed the highest concentrations of PFASs in the surface layer and the concentrations decreased with increasing depth for most PFASs, except for perfluorobutanesulfonate (PFBS). Downward movement of highly water soluble PFASs such as PFBS, following melting and freezing cycles of snow, was evident from the analysis of snow core.
全氟烷基物质(PFASs)在环境中广泛存在,包括偏远的海洋地区。PFASs 向偏远海洋地区的迁移方式是一个备受关注的科学问题。评估涵盖大陆、沿海和开阔海域的区域内湿沉降样品(即降雨和降雪)中 PFASs 的分布,不仅可以了解 PFASs 的全球迁移情况,还可以了解其区域迁移情况。然而,为了能够对 PFASs 的迁移做出结论,检查湿沉降矩阵的代表性和适宜性是至关重要的。在这项研究中,我们从日本的几个地点收集了包括降雨、地表雪和雪芯在内的湿沉降样品,以阐明这些矩阵在描述 PFASs 局部和区域迁移方面的适宜性。在一次降雨事件的不同时间间隔内收集的雨水在最初的 1 毫米沉积中表现出高 PFASs 通量。PFASs 通过湿沉降的清除率取决于氟碳链长的不同。在大陆(日本筑波)和开阔海洋(日本海岸外 1000 公里的太平洋)位置测量的 PFASs 沉积通量相似,约为每平方米几纳克。从同一地点采集的“新鲜”沉积和“老化”(在地面沉积几天)雪样中的 PFAS 剖面差异很大。新鲜沉积的雪代表了当前大气中 PFASs 的分布情况,而老化的雪样则反映了大气中本地 PFASs 源的封存。PFASs 剖面在沉积后的变化表明,PFASs 在雪/冰表面发生了反应。氟调聚物醇等前体化学品转化为全氟烷基羧酸酯的现象在雪表面明显。雪芯已被用于评估偏远环境中 PFAS 污染的时间趋势。在日本立山(2450 米)的一个长达 7.7 米深的雪芯中,从不同深度采集的雪样显示,PFASs 的浓度在表层最高,除全氟丁烷磺酸(PFBS)外,大多数 PFASs 的浓度随深度的增加而降低。PFBS 等高度水溶性 PFASs 在雪的融化和冻结循环后向下迁移,这一点从雪芯分析中可以明显看出。