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西北太平洋到北冰洋的有机磷酸酯(OPEs)的发生、分布、气-海交换和大气沉降。

Occurrence, distribution, air-seawater exchange and atmospheric deposition of organophosphate esters (OPEs) from the Northwestern Pacific to the Arctic Ocean.

机构信息

College of Marine Environment and Ecology, Shanghai Ocean University, Shanghai 201306, China; National Marine Environmental Monitoring Center, Dalian 116023, China; Hainan Tropical Ocean University, Sanya 572022, China.

College of Marine Environment and Ecology, Shanghai Ocean University, Shanghai 201306, China; National Marine Environmental Monitoring Center, Dalian 116023, China.

出版信息

Mar Pollut Bull. 2020 Aug;157:111243. doi: 10.1016/j.marpolbul.2020.111243. Epub 2020 May 29.

Abstract

Eleven organophosphate esters (OPEs) in air and seawater were investigated from the Northwestern Pacific to the Arctic Ocean. The concentration of ΣOPEs in air and seawater ranged from 231.56 to 1884.25 pg/m and from 8.47 to 143.45 ng/L, respectively. Halogenated OPEs dominated in both two media. The slight decreasing trend was observed for OPEs in gaseous air, no obvious trend for particle-bound OPEs and in seawater. The net air-seawater exchange flux ranged from -792.68 to 590.29 pg/m/day. The dry deposition flux ranged from 16.4 to 185 ng/m/day with high value observed at the Bering Strait (64.70 ng/m/day). The relationship between temperature and OPEs particle-bound fractions suggests that temperature might be a driving factor of OPEs long-range atmospheric transport (LRAT). This research highlighted that OPEs are subject to LRAT from the Asian continent to the northwestern Pacific and Arctic Oceans and demonstrated the "sink" in polar regions of OPEs atmospheric transportation.

摘要

从西北太平洋到北极海洋,研究了空气中和海水中的 11 种有机磷酸酯 (OPEs)。空气中和海水中的ΣOPEs 浓度范围分别为 231.56 到 1884.25 pg/m 和 8.47 到 143.45 ng/L。两种介质中均以卤代 OPEs 为主。气态空气中的 OPEs 呈轻微下降趋势,颗粒结合态 OPEs 和海水中的 OPEs 则无明显趋势。空气-海水交换通量的范围为-792.68 到 590.29 pg/m/天。干沉降通量范围为 16.4 到 185 ng/m/天,在白令海峡观测到的通量最高(64.70 ng/m/天)。温度与 OPEs 颗粒结合分数之间的关系表明,温度可能是 OPEs 长程大气传输(LRAT)的驱动因素。这项研究强调了 OPEs 从亚洲大陆到西北太平洋和北极海洋的 LRAT,并展示了 OPEs 大气传输在极地的“汇”作用。

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