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Estimating the Degree of Equilibrium between Passive Samplers and Pore Water for PCBs: Case Study and Comparison of Methods

机译:估计PCBS与孔隙水之间的均衡程度:案例研究与方法的比较

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Background. Passive samplers present many advantages over conventional alternatives for measuring hydrophobic organic compound (HOC) concentrations in sediment pore water and surface water based on both cost and data usability. Equilibrium based passive samplers, such as polydiemthylsiloxane (PDMS) coated glass rods (i.e., solid phase micro-extraction (SPME) samplers) enable collection of representative, depth discrete data without needing to collect large volume aqueous samples. The mathematical relationship to calculate pore water or surface water concentrations from sorbed mass in the samplers assumes equilibrium of HOCs such as polychlorinated biphenyls (PCBs) or polyaromatic hydrocarbons (PAH) between the sampler and the surrounding water, where equilibrium means no further changes in the concentrations in the sampler over time. Concentrations in the sampler will approach equilibrium with sufficiently long deployment times but the degree of equilibrium can be measured and corrected for in the pore water concentration calculations. Measuring the degree of equilibrium achieved and then adjusting calculated pore water concentrations provides a higher level of accuracy in the concentration data.
机译:背景。无源取样器在基于成本和数据可用性的基础上,具有测量沉积物孔隙水和地表水中的疏水性有机化合物(HOC)浓度的常规替代方案的许多优点。基于平衡的无源取样器,例如聚二羟基硅氧烷(PDMS)涂覆的玻璃棒(即,固相微萃取(SPME)采样器)能够收集代表性的深度离散数据,而不需要收集大容量水性样品。从采样器中的吸附质量计算孔隙水或表面水浓度的数学关系假定了种子器和周围水之间的多氯化双烯基(PCB)或多芳芳烃(PAH)的平衡,其中平衡意味着没有进一步变化随着时间的推移,采样器中的浓度。采样器中的浓度将以足够长的部署时间接近平衡,但可以在孔隙水浓度计算中测量和校正平衡程度。测量所达到的平衡程度,然后调节计算的孔隙水浓度在浓度数据中提供更高水平的精度。

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