首页> 外文期刊>Environmental toxicology and chemistry >MODELING BIPHASIC SORPTION AND DESORPTION OF HYDROPHOBIC ORGANIC CONTAMINANTS IN SEDIMENTS
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MODELING BIPHASIC SORPTION AND DESORPTION OF HYDROPHOBIC ORGANIC CONTAMINANTS IN SEDIMENTS

机译:沉积物中疏水性有机污染物的双吸附和脱附模型

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A model was developed to predict biphasic sorption and desorption of hydrophobic organic compounds in contaminated sediments. The model was based on relatively rapid porous diffusion in amorphous organic carbon and slow solid-phase diffusion in condensed-phase organic carbon. The model was used to simulate measured solid—fluid phase desorption (rates and pore-water concentrations) for four polycyclic aromatic hydrocarbons exhibiting a range of hydrophobicities (phenanthrene, anthracene, pyrene, and benzo[a]pyrene) in two field-contaminated sediments from Utica Harbor (Utica, NY, USA) and Rouge River (Detroit, MI, USA). Pore-water concentrations have been related to bioavailability, indicating the potential usefulness of the model to predict bioavailability. Key model parameters included the fraction of condensed-phase carbon (estimated by combustion at 375℃), partition coefficient to the condensed-phase carbon (estimated by desorption measurements on coal-like particles physically separated from Utica Harbor sediments), and diffusivity and ratio of volume to surface area of the condensed-phase organic matter (fitted to measured desorption data on both sediments and for the measured polycyclic aromatic hydrocarbons). Best fit for the diffusion coefficient in the condensed-phase organic matter was 8.5 x 10~(-20) m~2/s, and ratio of volume to surface area was 2 μm. These parameters estimated measured pore-water concentrations of all polycyclic aromatic hydrocarbons in both sediments with an average error of 46% and a correlation coefficient of 0.76 and the fast-desorbing fractions (as measured by the fraction removed with a nonpolar polymeric sorbent XAD-2) with an average error of approximately 30% and a correlation coefficient of 0.54 (14% and 0.76, respectively, for all but benzo[a]pyrene). Modeling results were relatively insensitive to the two fitted parameters, with changes of an order of magnitude or more being required to affect the correlation between the model and observations significantly.
机译:建立了一个模型来预测受污染沉积物中疏水性有机化合物的两相吸附和解吸。该模型基于非晶态有机碳中相对较快的多孔扩散和冷凝相有机碳中较慢的固相扩散。该模型用于模拟在两种被现场污染的沉积物中表现出一定范围的疏水性(菲,蒽,pyr和苯并[a] py)的四种多环芳烃的固-液相解吸(速率和孔隙水浓度)。从美国的尤蒂卡港口(Utica,NY,USA)和Rouge River(美国的密歇根州底特律)出发。孔隙水浓度与生物利用度有关,表明该模型预测生物利用度的潜在用途。关键的模型参数包括:冷凝相碳的比例(通过在375℃下燃烧估算),分配给冷凝相碳的分配系数(通过对与乌提卡港口沉积物物理分离的煤样颗粒的解吸测量估算),扩散系数和比例体积相对于冷凝相有机物的表面积(适合于沉积物和测得的多环芳烃的解吸数据)。冷凝相有机质中扩散系数的最佳拟合为8.5 x 10〜(-20)m〜2 / s,体积与表面积之比为2μm。这些参数估计了两种沉积物中所有多环芳烃的孔隙水浓度,平均误差为46%,相关系数为0.76,并且具有快速脱附分数(通过用非极性聚合物吸附剂XAD-2去除的分数进行测量) )的平均误差约为30%,相关系数为0.54(除苯并[a] py以外的所有相关系数分别为14%和0.76)。建模结果对两个拟合参数相对不敏感,需要大量或更大数量级的变化才能显着影响模型与观测值之间的相关性。

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