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中国黄河口水中和沉积物中全氟辛烷磺酸(PFOS)的分布及影响因素。

Perfluorooctane sulfonate (PFOS) distribution and effect factors in the water and sediment of the Yellow River Estuary, China.

机构信息

School of Geography and Tourism, Qufu Normal University, Rizhao, 276826, China.

出版信息

Environ Monit Assess. 2013 Oct;185(10):8517-24. doi: 10.1007/s10661-013-3192-5. Epub 2013 Apr 17.

Abstract

The distribution of perfluorooctane sulfonate (PFOS) was investigated in a total of 15 water and sediment samples from the Yellow River Estuary, China in April 2011. The results indicated that the concentrations of PFOS in the water and sediment samples averaged 157.5 ng/L and 198.8 ng/g and ranged from 82.30 to 261.8 ng/L and 75.48 to 457.0 ng/g, respectively. The concentrations of PFOS in the sediment column increased from 45.32 to 379.98 ng/g with the decrease of the sampling depth, which showed that the increased PFOS pollution in the sediment appeared in this region in over recent years. The distribution coefficient (K d) of PFOS between water and sediment linearly increased from 0.37 to 4.80 L/g as the salinity (S‰) increased from 0.18 to 4.47. Correlation analysis revealed that K d was significantly and positively correlated to the contents of total organic carbon and clay of the sediment, and salinity. Therefore, salinity was an important parameter in controlling the sediment-water interactions and the fate or transport of PFOS in the aquatic environment. The results of this study showed that the estuary was an important sink for PFOS and suggested that PFOS might be carried with the river water and transported for long distances before it reached to the sea and largely scavenged to the sediment in the estuaries due to the change in salinity.

摘要

2011 年 4 月,在中国黄河口共采集了 15 个水和沉积物样本,研究了全氟辛烷磺酸(PFOS)的分布情况。结果表明,水样和沉积物样品中 PFOS 的浓度平均值分别为 157.5ng/L 和 198.8ng/g,范围分别为 82.30-261.8ng/L 和 75.48-457.0ng/g。沉积物柱中 PFOS 的浓度从 45.32ng/g 增加到 379.98ng/g,随着采样深度的降低而增加,这表明近年来该地区的沉积物中 PFOS 污染有所增加。PFOS 在水和沉积物之间的分配系数(Kd)随着盐度(S‰)从 0.18 增加到 4.47 而从 0.37 线性增加到 4.80L/g。相关分析表明,Kd 与沉积物中总有机碳和粘土的含量以及盐度显著正相关。因此,盐度是控制水-沉积物相互作用和 PFOS 在水生态系统中归宿或迁移的重要参数。本研究结果表明,河口是 PFOS 的重要汇,由于盐度的变化,PFOS 可能随河水携带并长距离运输,到达海洋后大部分被河口的沉积物大量吸收。

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