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使用预加载盘测定高度疏水有机污染物在脂质/蛋白质和聚二甲基硅氧烷之间的平衡分配系数。

Determining equilibrium partition coefficients between lipid/protein and polydimethylsiloxane for highly hydrophobic organic contaminants using preloaded disks.

机构信息

State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China; School of Environment, Guangzhou Key Laboratory of Environmental Exposure and Health, and Guangdong Key Laboratory of Environmental Pollution and Health, Jinan University, Guangzhou 510632, China; University of Chinese Academy of Sciences, Beijing 100049, China.

School of Environment, Guangzhou Key Laboratory of Environmental Exposure and Health, and Guangdong Key Laboratory of Environmental Pollution and Health, Jinan University, Guangzhou 510632, China.

出版信息

Sci Total Environ. 2017 Nov 15;598:385-392. doi: 10.1016/j.scitotenv.2017.04.123. Epub 2017 Apr 24.

Abstract

Bioaccumulation of hydrophobic organic contaminants is of great concern and understanding their partitioning to biological phases is crucial for estimating their bioaccumulation potential. The estimation, however, was of large uncertainty for highly hydrophobic organic contaminants (HHOCs) with log K>9 due to the challenge of quantifying their water concentrations. In the present study, partition coefficients between polydimethylsiloxane (PDMS) and storage lipid (K), membrane lipid (K) and protein (K) were measured for 21 polychlorinated biphenyls (PCBs), 14 polybrominated diphenyl ethers (PBDEs), dechlorane plus (DP) and decabromodiphenyl ethane (DBDPE), covering log K from 5.07 to 11.6, using a preloaded PDMS depletion method. The values of K, K and K were in the ranges of 5.36-52.5, 0.286-11.8 and 0.067-2.62g/g, respectively, being relatively constant although their K values extend more than six orders of magnitude. The relative sorption capacity of the biological phases showed storage lipid was the dominant sorption phase in biota, followed by membrane lipid and protein was the lowest. The K values of the compounds with log K<9 were similar (0.382-14.9g/g) regardless of the thickness of preloaded PDMS disks (58-209μm). For HHOCs, however, K values dropped when thinner PDMS disks were used, as a result of slow diffusion of HHOCs in PDMS. The K values of HHOCs measured by 58-μm PDMS disks ranged from 1.78 to 6.85g/g, which was consistent with compounds with log K<9. This validated that partition coefficients between PDMS and biological phases were independent of chemical hydrophobicity, showing the advantage of using PDMS-based methods to directly estimate bioaccumulation potential of HHOCs.

摘要

生物浓缩的疏水性有机污染物是非常关注的,了解它们分配到生物阶段对于估计其生物浓缩潜力至关重要。然而,由于难以量化其水浓度,对于疏水性极强的有机污染物(HHOCs),其log K 值大于 9,其估算存在很大的不确定性。在本研究中,使用预加载聚二甲基硅氧烷(PDMS)耗竭法,测量了 21 种多氯联苯(PCBs)、14 种多溴二苯醚(PBDEs)、氯丹加(DP)和十溴二苯乙烷(DBDPE)在储存脂质(K)、膜脂质(K)和蛋白质(K)之间的分配系数,log K 值范围为 5.07 至 11.6。K、K 和 K 的值分别在 5.36-52.5、0.286-11.8 和 0.067-2.62g/g 范围内,尽管它们的 K 值相差六个数量级以上,但相对恒定。生物相的相对吸附能力表明,储存脂质是生物体内的主要吸附相,其次是膜脂质,而蛋白质是最低的。log K 值小于 9 的化合物的 K 值相似(0.382-14.9g/g),与预加载 PDMS 圆盘的厚度(58-209μm)无关。然而,对于 HHOCs,当使用更薄的 PDMS 圆盘时,K 值会下降,这是由于 HHOCs 在 PDMS 中的扩散缓慢。使用 58-μm PDMS 圆盘测量的 HHOCs 的 K 值范围为 1.78 至 6.85g/g,与 log K 值小于 9 的化合物一致。这验证了 PDMS 与生物相之间的分配系数与化学疏水性无关,表明使用基于 PDMS 的方法直接估计 HHOCs 的生物浓缩潜力具有优势。

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