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Frontiers of Environmental Science & Engineering

ISSN 2095-2201

ISSN 2095-221X(Online)

CN 10-1013/X

Postal Subscription Code 80-973

2018 Impact Factor: 3.883

Front Envir Sci Eng    2012, Vol. 6 Issue (1) : 59-65    https://doi.org/10.1007/s11783-010-0259-1
RESEARCH ARTICLE
Effects of different sediment fractions on sorption of galaxolide
Lixia JIN, Mengchang HE(), Jinghuan ZHANG
State Key Laboratory of Water Environment Simulation, School of Environment, Beijing Normal University, Beijing 100875, China
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Abstract

Sorption isotherms of galaxolide (HHCB) of different fractions from two sediments with different mineral and organic carbon contents were determined to compare HHCB sorption behavior and contribution to the total sorption. The HHCB sorption isotherms that used the batch equilibration method were studied on different sediments of different fractions. The sorption isotherms of 600°C heating fractions were detailed using the linear model, while the other fractions were nonlinear and fitted well with the Freundlich model. The dissolved organic carbon (DOC) removed, NaOH extracted, and 375°C heating fractions showed more nonlinear sorption than the original sediments, which suggested more heterogeneous sorption sites in these fractions. Compared to the original sediments, the 375°C heating fractions had higher carbon-normalized distribution coefficient (Koc) values, indicating a higher sorption affinity for HHCB. Among the different sediment fractions, the contribution of the 600°C heating fractions to the overall sorption were the lowest (<20%), while the 375°C heating fractions were the highest (up to 85%).

Keywords galaxolide (HHCB)      sorption      organic carbon      sediment      carbon-normalized distribution coefficient (Koc)     
Corresponding Author(s): HE Mengchang,Email:hemc@bnu.edu.cn   
Issue Date: 01 February 2012
 Cite this article:   
Lixia JIN,Mengchang HE,Jinghuan ZHANG. Effects of different sediment fractions on sorption of galaxolide[J]. Front Envir Sci Eng, 2012, 6(1): 59-65.
 URL:  
https://academic.hep.com.cn/fese/EN/10.1007/s11783-010-0259-1
https://academic.hep.com.cn/fese/EN/Y2012/V6/I1/59
samplesTOC/%fa/%ash/%SSA/(m2·g-1)clay/%silt/%sand/%Davb/μmTg/°C
Daliao River (SA)
original sediment2.84-12.265.350.1968.4531.3633.0553.13
DOC removed3.58114.311.949.040.1875.3624.4621.3848.52
NaOH extracted2.5979.17.7115.450.2459.0840.6845.6143.52
heated at 375°C1.2523.14.6611.420.2069.3230.4832.36-
heated at 600°C-88.41.8113.230.3768.6930.9331.66-
Yellow River (SB)
Original sediment0.12-5.963.76043.5956.4062.3553.24
DOC removed0.14111.25.603.68042.6557.3563.1854.44
NaOH extracted0.0858.65.153.45047.8952.1057.7040.41
Heated at 375°C0.0941.45.758.33043.8556.1661.98-
Heated at 600°C-94.23.754.31043.1256.8862.69-
Tab.1  Characteristics of different fractions from two river sediments
Fig.1  FTIR spectra of different sediment fractions
Note: a and f- original sediment, b and g- DOC removed, c and h- NaOH extracted, d and i- heated at 375°C, and e and j- heated at 600°C
Fig.1  FTIR spectra of different sediment fractions
Note: a and f- original sediment, b and g- DOC removed, c and h- NaOH extracted, d and i- heated at 375°C, and e and j- heated at 600°C
Fig.2  Sorption isotherms of HHCB on different sediment fractions
Fig.2  Sorption isotherms of HHCB on different sediment fractions
linear modelFreundlich model
sorbentsKdR2nR2KFOCaNcKOCb/(mL·g-1)
Ce = 0.01 mg·L-1Ce = 0.1 mg·L-1Ce = 0.5 mg·L-1
Daliao River (SA)
original sediment2.91×1030.9610.93±0.110.9639.17×104161.27×1051.08×1059.62×104
DOC removed3.19×1030.9801.33±0.080.9971.26×105162.74×1045.87×1041.00×105
NaOH extracted2.82×1030.9821.30±0.070.9921.74×105184.23×1048.58×1041.41×105
heated at 375°C1.97×1030.9400.84±0.080.9532.34×105204.81×1053.35×1052.60×105
heated at 600°C2.08×1030.9741.18±0.090.889-18---
Yellow River (SB)
original sediment1.50×1030.9740.90±0.120.9731.14×106161.77×1051.42×1061.21×106
DOC removed2.28×1030.9741.34±0.130.9762.40×106165.05×1051.10×1061.90×106
NaOH extracted3.46×1030.9831.31±0.030.9974.38×106181.05×1062.15×1063.54×106
heated at 375°C3.60×1030.9741.27±0.090.9918.24×106202.39×1064.44×1066.84×106
heated at 600°C3.44×1030.9581.28±0.140.913-18---
Tab.2  Fitting parameters by linear and Freundlich models for HHCB sorption on different fractions from two river sediments
Fig.3  Contribution of each fraction to total HHCB sorption by the original sediments
Fig.3  Contribution of each fraction to total HHCB sorption by the original sediments
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