University of Rhode Island Graduate School of Oceanography, South Ferry Road, Narragansett, Rhode Island 02882, United States.
Environ Sci Technol. 2011 Mar 15;45(6):2270-7. doi: 10.1021/es1040865. Epub 2011 Feb 22.
To be able to use polyethylene passive samplers (PE) in the field, the partitioning constants between PE and water (K(PEw)) of the compounds examined must be known. The K(PEw)s of triclosan (TCS), methyl-triclosan (MTCS), n-nonylphenol (n-NP), nonylphenol-technical mix (NP-tech), n-octylphenol (n-OP), and t-octylphenol (t-OP) were measured as a function of pH, temperature, and salinity, and a salt effect was calculated for TCS, n-OP, and t-OP. Log K(PEw)s used for calculating dissolved concentrations were taken from 20 °C studies taking salt into account: 3.42 (TCS), 4.53 (MTCS), 4.20 (n-NP), 3.69 (n-OP), and 2.87 (t-OP). The K(PEw) of hydroxyl-group containing compounds were strongly affected by pH, whereas MTCS with its methoxy-group was not. Measured K(PEw)s could not be estimated from octanol-water partitioning constants due to the semipolar makeup of the compounds investigated. Instead, a good correlation (K(PEw) = 0.679 × K(hdw) + 1.033, r(2) = 0.984, p = 0.001) was obtained with hexadecane-water partitioning constants (K(hdw)) predicted from COSMOtherm. During deployments in Narragansett Bay (RI) in the fall of 2009, concentrations of MTCS and t-OP in surface and bottom waters ranged from 40-225 pg L(-1) and 3.5-11 ng L(-1), respectively. These concentrations are far below EC(50) values for rainbow trout. Surface/bottom and bottom/porewater activity ratios were calculated. These indicated surface waters as the main source of MTCS, while surface water as well as sediments were sources of t-OP.
为了能够在野外使用聚乙烯被动采样器(PE),必须知道所研究化合物在 PE 与水之间的分配常数(K(PEw))。测定了三氯生(TCS)、甲基三氯生(MTCS)、壬基酚(n-NP)、壬基酚-工业混合物(NP-tech)、辛基酚(n-OP)和叔辛基酚(t-OP)的 K(PEw)随 pH 值、温度和盐度的变化,并计算了 TCS、n-OP 和 t-OP 的盐效应。用于计算溶解浓度的 log K(PEw)取自考虑盐分的 20°C 研究:3.42(TCS)、4.53(MTCS)、4.20(n-NP)、3.69(n-OP)和 2.87(t-OP)。含羟基化合物的 K(PEw)受 pH 值影响较大,而含甲氧基的 MTCS 则不受影响。由于所研究化合物的半极性组成,无法根据辛醇-水分配常数来估算实测的 K(PEw)。相反,从 COSMOtherm 预测的十六烷-水分配常数(K(hdw))与 K(PEw)之间存在良好的相关性(K(PEw) = 0.679 × K(hdw) + 1.033,r(2) = 0.984,p = 0.001)。2009 年秋季在罗得岛州纳拉甘塞特湾(Narragansett Bay)进行部署时,表层和底层水中 MTCS 和 t-OP 的浓度范围分别为 40-225 pg L(-1)和 3.5-11 ng L(-1)。这些浓度远低于虹鳟鱼的 EC(50)值。计算了表层/底层和底层/孔隙水的活度比。这些表明表层水是 MTCS 的主要来源,而表层水和沉积物都是 t-OP 的来源。