Ding Xiang, Wang Xin-ming, Xie Zhou-qing, Xiang Cai-hong, Mai Bi-xian, Sun Li-guang, Zheng Mei, Sheng Guo-ying, Fu Jia-mo
State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China.
Environ Sci Technol. 2007 Aug 1;41(15):5204-9. doi: 10.1021/es070237w.
During the 2003 Chinese Arctic Research Expedition (CHINARE2003) from the Bohai Sea to the high Arctic (37 degrees N to 80 degrees N) aboard the icebreaker Xuelong (Snow Dragon), air samples were collected for the analysis of hexachlorocyclohexanes (HCHs) in the North Pacific Ocean and adjacent Arctic region. The sigma HCHs (alpha-HCH + gamma-HCH) ranged from 2.3 to 95.1 pg/m3 with the highest levels observed in Far East Asia (32.5 pg/m3), followed by the North Pacific Ocean (17.0 pg/m3) and the Arctic (7.3 pg/ m3). Compared to previous studies in the same areas in 1990s, our measurements were approximately 1 order of magnitude lower. Because of disproportionate chemical reduction and physical fractioning during long-range transport, the ratios of alpha-HCH to gamma-HCH (alpha/gamma-HCH) showed a significant increasing trend from low to high latitudes, suggesting thatthe alpha/gamma-HCH range of 4-7 could not be used to identify sources of technical HCHs especially in remote areas. The ratios of (+)-alpha-HCH to the sum of (+)-alpha-HCH and (-)-alpha-HCH were on average much more biased from 0.5 compared to previous observations in mid-1990s, indicating the exchange of atmospheric alpha-HCH with those in the oceans, where (+)-alpha-HCH was selectively depleted in biological degradation processes. Estimated fugacity ratios based on available data for both alpha-HCH and gamma-HCH further implied their net volatilization from seawater to air in the Arctic Ocean.
在2003年中国北极科学考察(CHINARE2003)期间,乘坐破冰船“雪龙号”从渤海前往高北极地区(北纬37度至80度),采集了空气样本,用于分析北太平洋及邻近北极地区的六氯环己烷(HCHs)。总六氯环己烷(α-六氯环己烷+γ-六氯环己烷)浓度范围为2.3至95.1皮克/立方米,其中在远东地区观测到的浓度最高(32.5皮克/立方米),其次是北太平洋(17.0皮克/立方米)和北极(7.3皮克/立方米)。与20世纪90年代同一地区的先前研究相比,我们的测量值大约低了1个数量级。由于在长距离传输过程中化学降解和物理分馏不均衡,α-六氯环己烷与γ-六氯环己烷的比例(α/γ-六氯环己烷)从低纬度到高纬度呈现出显著的上升趋势,这表明4至7的α/γ-六氯环己烷范围尤其在偏远地区不能用于识别工业用六氯环己烷的来源。与20世纪90年代中期的先前观测相比,(+)-α-六氯环己烷与(+)-α-六氯环己烷和(-)-α-六氯环己烷总和的比例平均更偏离0.5,这表明大气中的α-六氯环己烷与海洋中的α-六氯环己烷发生了交换,其中(+)-α-六氯环己烷在生物降解过程中被选择性消耗。基于α-六氯环己烷和γ-六氯环己烷现有数据估算的逸度比进一步表明它们在北冰洋中从海水向空气的净挥发。