Sorption Of Phenanthrene Research Articles

Comparative Sorption of Phenanthrene and Benzo[α]pyrene to Soil Humic Acids

Sorption of phenanthrene (Phen) and benzo[α]pyrene (BaP) by humic acids (HAs) extracted from four typical soils in China, including cinnamon soil, fluvo-aquic soil, red soil, and mountain meadow soil were investigated. All sorption data were fitted well by the Freundlich model, but BaP exhibited stronger and more nonlinear sorption than Phen by a given HA. For Phen isotherms, there was a positive relation between K oc values and aliphaticity of HAs, whereas a negative correlation was observed between n values and aliphaticity. This indicated the importance of aliphatic groups in Phen sorption capacity and nonlinearity. Compared to Phen, a similar trend was obtained between n values of BaP and aliphaticity or aromatic carbon. However, no correlation existed between K oc values for BaP and aliphaticity or aromatic carbon.

Sorption of polycyclic aromatic hydrocarbons on particulate organic matters

Particulate organic matter (POM) is a key organic matter fraction which can influence soil fertility. Its interactions with hydrophobic organic pollutants (HOCs) have not been characterized and the mechanisms of retention of HOCs by POM remain unclear. In the present study, sorption behaviors of polycyclic aromatic hydrocarbons (PAHs) naphthalene (NAP), phenanthrene (PHE), and pyrene (PYR) by POMs separated from different soils were examined and the POMs were characterized by elemental analysis, solid state (13)C NMR, and Fourier transform infrared spectroscopy (FT-IR). The results indicated that POMs were mainly composed of aliphatic components with high polarity. The different original POMs showed similar chemical composition and configuration. Sorption behaviors of PAHs indicated that there was no significant difference in sorption capacity among the POMs. Sorption of NAP and PHE by POMs displayed a nonlinear isotherm, while sorption of PYR yielded a linear isotherm. No significant hysteresis and ionic strength effect were observed for PAH desorption from the POMs.

Impact of low-molecular-weight organic acids on the availability of phenanthrene and pyrene in soil

The impact of low-molecular-weight organic acids (LMWOAs) on the availability of phenanthrene and pyrene was investigated using laboratory batch assays. Experiments were conducted with two types of soil with different organic contents. The LMWOAs used were citric and oxalic acid. A mild solvent extraction procedure and a sorption–desorption experiment were used to predict the availability of phenanthrene and pyrene. Results showed that the extractable amounts of phenanthrene and pyrene in both soil types increased with increased citric or oxalic acid concentration. Citric acid addition promoted phenanthrene and pyrene extraction to a greater degree than oxalic acid. Compared with freshly spiked soils, the extractable amounts of phenanthrene and pyrene with the addition of LMWOAs decreased significantly after 60 days of cultivation. Soils with higher values of soil organic carbon content ( f oc) showed decreased phenanthrene and pyrene availability after the addition of LMWOAs. The sorption and desorption results also demonstrated the enhanced availability of PAHs with LMWOA addition. Phenanthrene sorption could be described using a linear model, regardless of the addition of LMWOAs. The simulated distribution constants ( K d) for phenanthrene sorption decreased significantly with the addition of LMWOAs. In contrast, phenanthrene desorption clearly increased with the addition of LMWOAs. These results suggest that the availabilities of phenanthrene and pyrene can be increased with the addition of suitable LMWOAs.

Impact of Kerogen Heterogeneity on Sorption of Organic Pollutants. 2. Sorption Equilibria

Phenanthrene and naphthalene sorption isotherms were measured for three different series of kerogen materials using completely mixed batch reactors. Sorption isotherms were nonlinear for each sorbate-sorbent system, and the Freundlich isotherm equation fit the sorption data well. The Freundlich isotherm linearity parameter n ranged from 0.192 to 0.729 for phenanthrene and from 0.389 to 0.731 for naphthalene. The n values correlated linearly with rigidity and aromaticity of the kerogen matrix, but the single-point, organic carbon-normalized distribution coefficients varied dramatically among the tested sorbents. A dual-mode sorption equation consisting of a linear partitioning domain and a Langmuir adsorption domain adequately quantified the overall sorption equilibrium for each sorbent-sorbate system. Both models fit the data well, with r2 values of 0.965 to 0.996 for the Freundlich model and 0.963 to 0.997 for the dual-mode model for the phenanthrene sorption isotherms. The dual-mode model fitting results showed that as the rigidity and aromaticity of the kerogen matrix increased, the contribution of the linear partitioning domain to the overall sorption equilibrium decreased, whereas the contribution of the Langmuir adsorption domain increased. The present study suggested that kerogen materials found in soils and sediments should not be treated as a single, unified, carbonaceous sorbent phase.

Phenanthrene sorption to humic acids, humin, and black carbon in sediments from typical water systems in China

Humic acid (HA) and humin (HM) were extracted with 0.1 M NaOH and black carbon (BC) was isolated using a combustion method at 375 degrees C from six sediments in different areas in China and their sorption isotherms for phenanthrene (Phen) were determined. All sorption isotherms were nonlinear and fitted well with the Freundlich model. Among the SOM, HM and BC with more aromatic carbon controlled the sorption nonlinearity and capacity. Compared to HM, higher K (oc) values were observed for BC due to the combustion of organic matter and native sorbates in HM. For HAs isotherms, a positive relation was observed between the K (oc) values and aliphaticity or H/C ratios, but a negative relation was shown between the n values and polarity of HAs. HA, HM, and BC were responsible for 0.4-9.3%, 46-97%, and 65-96% of the total sorption, respectively, indicating the dominance of HM and BC fractions in overall sorption of Phen by the sediments.

Sorption of phenanthrene by nanosized alumina coated with sequentially extracted humic acids

Sorption of hydrophobic organic compounds (HOCs) to natural organic matter (NOM) is an important process that affects the transport, transformation, bioavailability, and fate of HOCs in the environment. Manufactured nanoparticles (NPs) such as nano-oxides will inevitably enter the environment in the processes of their production, transfer, and use and could be coated by the ubiquitous NOM. Thus, sorption of HOCs to NOM in the environment could be affected by the NP interactions with NOM. Furthermore, the toxicity of nano-oxides could be increased due to the adsorbed HOCs. Therefore, sorption of phenanthrene by nano-Al(2)O(3) coated with humic acid (HA) was examined in this study to explore the possible effect of nanoparticles (NPs) on the environmental behavior of HOCs and the potential environmental and health risks of NPs. Four HAs were sequentially extracted with 0.1 mol/L NaOH from a peat soil. HAs, nano-Al(2)O(3), and HA-coated nano-Al(2)O(3) were characterized by techniques such as elemental analysis, solid-state (13)C NMR, N(2) surface area analysis, and zeta potential measurement. Adsorption isotherms of HAs by nano-Al(2)O(3) and phenanthrene by HAs and HA-coated nano-Al(2)O(3) were obtained using a batch equilibration technique at 25 +/- 1 degrees C. HA concentrations were measured by total organic carbon analysis. Phenanthrene concentrations were measured by liquid scintillation counting. The adsorption maxima of HAs by nano-Al(2)O(3) was one order of magnitude higher than that by soil inorganic minerals. Phenanthrene isotherms of HA-coated nano-Al(2)O(3) were more nonlinear than that of their respective bulk HAs. Concentration-dependent organic carbon-normalized sorption coefficients (K' (oc)) of phenanthrene by HA-coated nano-Al(2)O(3) were lower than those for their respective bulk HAs, especially at relatively high concentrations. Isotherm nonlinearity of phenanthrene could be interpreted by a combination of partitioning accompanied by linear isotherm with adsorption accompanied by nonlinear isotherm. HA conformation changes during their adsorption on nano-Al(2)O(3) could play an important role in phenanthrene sorption and were responsible for higher nonlinearity of phenanthrene isotherms and lower phenanthrene K' (oc) on the adsorbed HAs than their respective bulk HAs. Adsorption of HA on nano-Al(2)O(3) would form a more condensed HA state with higher pi-polarity/polarizability and lower partitioning affinity than the respective bulk HA, leading to an increase of relative contribution of adsorption to the total sorption and more nonlinear phenanthrene isotherms in the adsorbed HA due to the increase in phenanthrene adsorption affinity and decrease in phenanthrene partitioning affinity. Adsorption of HA on nano-Al(2)O(3) was much higher than that on soil oxide minerals and could form a more condensed HA state with higher pi-polarity/polarizability and lower partitioning affinity than the bulk HA, causing the significant difference in phenanthrene sorption between the adsorbed HA and the respective bulk HA. Therefore, once released in the environment, NPs such as nano-Al(2)O(3) will strongly alter the environmental transport, fate, and bioavailability of HOCs and could be potentially more toxic due to the adsorbed toxic chemicals. Due to the high adsorption of HA on nano-Al(2)O(3) and its significant effect on phenanthrene sorption, interactions of NOM with nano-oxides and their mechanistic relations with NOM conformation changes and HOC sorption merit further research. In addition, due to the higher sorption of phenanthrene on the HA-coated nano-Al(2)O(3) than the pure counterpart, the effect of NOM and HOCs on the ecotoxicity of NPs should be addressed in the future.

Predicted models for phenanthrene sorption nonlinearity and capacity based on different HA/BC ratios in sediments

Phenanthrene (Phen) sorption isotherms for synthetic sediment organic matter samples with nine different humic acid/black carbon (HA/BC) ratios were determined to provide predicted models for Phen sorption nonlinearity and affinity by sediments. The sorption data were fitted well by the Freundlich model. The nonlinear sorption of Phen was dominated by BC particles. According to BC/TOC content, Phen sorption nonlinearity can be predicted using the exponential model: n = 0.410 + 0.454 ∗ exp(−0.028 BC/TOC). As sorption is a combination of absorption into soft carbon and adsorption onto hard carbon, based on published K HA, K FBC, and n bc values and measured f BC and f oc values, Phen sorption affinity-related parameter K oc values can be predicted from the simplified dual sorption model: f oc K oc = ( f oc - f BC ) K HA + f BC K FBC C e n bc - 1 . For sediments from the Song–Liao watershed (China), the exponential model and dual sorption model gave good predictions for n and K oc values, which support the availability of the two predicted models.

The effect of solvent-conditioning on soil organic matter sorption affinity for diuron and phenanthrene

The effect of solvent-conditioning on the sorption of diuron and phenanthrene was investigated. The organic carbon-normalized sorption coefficients ( K OC) for diuron and phenanthrene (determined from single initial concentrations of 0.8 mg L −1 and 1.5 mg L −1, respectively) were consistently higher following solvent-conditioning of a whole soil with five organic solvents (acetonitrile, acetone, methanol, chloroform and dichloromethane). The relative increase in K OC was inversely related to the polarity of the conditioning solvent (i.e. greater increases in K OC were observed for the least polar solvents: chloroform and dichloromethane). The effect of solvent-conditioning on the sorption properties of the same soil that had been lipid-extracted using accelerated solvent extraction (ASE) was also investigated. Since lipid extraction involves treatment with a non-polar solvent (95:5 dichloromethane:methanol) one may have expected no further increase in K OC on solvent-conditioning. On the contrary, the lipid-extracted soil exhibited very similar increases in K OC as the whole soil. This demonstrated that lipid removal and solvent-conditioning, which both increased K OC for this soil, are quite separate phenomena.

Role of Suberin, Suberan, and Hemicellulose in Phenanthrene Sorption by Root Tissue Fractions of Switchgrass (Panicum virgatum) Seedlings

Sorption of organic pollutants by root tissue fractions, and the role of root turnover in mobilizing organic pollutants in soils, may help elucidate mechanisms of pollutant uptake by plants. The sorption of phenanthrene by bulk root tissue of switchgrass (Panicum virgatum) seedlings exhibits uptake much higher than predicted based on the extractable lipids in root tissues and the octanol-water partition coefficient for phenanthrene. Surprisingly, the removal of waxes, extracted by organic solvents, results in only a slight reduction in sorption, however, the subsequent removal of suberin (polymeric lipids) by saponification greatly reduces the affinity of the residual materials (by 7-fold), suggesting that suberin serves as the major sorption medium for organic pollutants. The sorption capability of suberan (i.e., lignin and cellulose) components is completely masked by coexisting hemicellulose materials. The removal of the hemicellulose by acid hydrolysis markedly enhanced the affinity of plant root tissue fractions for phenanthrene (5-40 times), which was attributed to sorption by the aromatic condensed domains as derived from solid-state 13C NMR data. Reversible sorption-desorption of bulk root tissue and the extractable lipids was observed, but the hydrolyzing fractions and the dewaxed-saponifiable residues demonstrated irreversible sorption.

Phenanthrene partitioning in sediment–surfactant–fresh/saline water systems

The objective of this study was to investigate the influence of salinity on the effectiveness of surfactants in the remediation of sediments contaminated with phenanthrene (PHE). This is an example of a more general application of surfactants in removing hydrophobic organic compounds (HOCs) from contaminated soil/sediment in saline environments via in-situ enhanced sorption or ex-situ soil washing. Salinity effects on surfactant micelle formation and PHE partitioning into solution surfactant micelles and sorbed surfactant were investigated. The critical micelle concentration of surfactants decreased, and PHE partition between surfactant micelles and water increased with increasing salinity. Carbon-normalized partition coefficients ( K ss) of PHE onto the sorbed cationic surfactant increased significantly with increasing salinity, which illustrates a more pronounced immobilization of PHE by cationic surfactant in a saline system. Reduction of PHE sorption by anionic surfactant was more pronounced in the saline system, indicating that the anionic surfactant has a higher soil washing effectiveness in saline systems.

Static and dynamic sorption of phenanthrene in mangrove sediment slurry

The static and dynamic sorption of phenanthrene (Phe) in three types of mangrove sediment slurries (sandy, silty and muddy) were described by three models, namely linear model, Freundlich adsorption isotherm model and Langmuir adsorption isotherm model. The Freundlich adsorption isotherm was the best model to describe the static sorption behavior of Phe in mangrove sediment slurry with the regression coefficients ranging from 0.96 to 0.99. In static sorption, the sorption capacity and sorption intensity were reduced with the inoculation of Sphingomonas, a PAH-degrading bacterial isolate, suggesting that the inoculum even though inactive and/or dead would enhance bioavailability of Phe. On the other hand, the static sorption of Phe was significantly enhanced at high salinity (20 ppt) while no difference was found at low salinities ranging from 5 to 15 ppt. During the dynamic sorption process, i.e. with biodegradation by indigenous microorganisms and the inoculation of Sphingomonas, linear regression was the most suitable model to describe Phe sorption behavior. The partition coefficient α was the highest in silty sediment, followed by sandy sediment and the muddy sediment had the lowest value. These results indicated that the sorption behavior of Phe changed from non-linear to linear when biodegradation took place and the silty mangrove sediment slurry had the highest sorption affinity.

Effects of humic acid and lipid on the sorption of phenanthrene on char

The impact of two types of natural organic matters (NOM), humic acid (HA) and lipid, on char properties and sorption affinities for phenanthrene was studied. Char was coated with HA and lipid at a concentration of 0.060, 0.250 and 0.500 g/g char. HA, lipid, char and coated char were characterized and their sorption behaviors for phenanthrene were compared. Coating with NOM increased the polarity and aliphaticity, and reduced the specific surface area (SSA) of char, depending on the coated amount and the type of NOM. At the lower HA and lipid loading there was a strong attenuation of N 2-assessible SSA. The SSA attenuation was less pronounced at larger HA and lipid loadings, which was most likely due to the preferential sorption at reactive sites and formation of clusters. The sorption isotherms of phenanthrene on char and coated char fitted Freundlich equation well, suggesting that all sorption isotherms were nonlinear, with N values in the range of 0.495–0.873. Coated char with HA and lipid decreased the organic carbon-normalized sorption coefficients K FOC and increased the N values. Lipid was more effective than HA in decreasing SSA, phenanthrene sorption capacity and sorption isotherm nonlinearity. The N values were correlated positively with the aliphaticity and negatively with pore volume of sorbents. The results of this investigation demonstrated that different NOM plays a different role in attenuating the SSA and sorption affinity of char for phenanthrene.

Effects of chemical oxidation on sorption and desorption of PAHs in typical Chinese soils

In situ chemical oxidation is a commonly applied soil and groundwater remediation technology, but can have significant effects on soil properties, which in turn might affect fate and transport of organic contaminants. In this study, it was found that oxidation treatment resulted mainly in breakdown of soil organic matter (SOM) components. Sorption of naphthalene and phenanthrene to the original soils and the KMnO 4-treated soils was linear, indicating that hydrophobic partitioning to SOM was the predominant mechanism for sorption. Desorption from the original and treated soils was highly resistant, and was well modeled with a biphasic desorption model. Desorption of residual naphthalene after treating naphthalene-contaminated soils with different doses of KMnO 4 also followed the biphasic desorption model very well. It appears that neither changes of soil properties caused by chemical oxidation nor direct chemical oxidation of contaminated soils had a noticeable effect on the nature of PAH–SOM interactions.

Sorption of Phenanthrene by Humic Acid-Coated Nanosized TiO2 and ZnO

Phenanthrene sorption by nano-TiO2 and nano-ZnO particles was enhanced significantly by coated humic acids (HAs), implying that additional toxicity can be potentially given to these nanooxides by adsorbed HOCs once released to the environment. Phenanthrene isotherms of adsorbed HA on nano-TiO2 and nano-ZnO were more nonlinear than that of their respective bulk HA. Both HA conformation changes and fractionation were observed upon HA adsorption on nano-TiO2 and nano-ZnO, which further affected phenanthrene sorption. Nano-TiO2 and nano-ZnO interacted with differentfunctional groups of HA (i.e., phenolic OH with nano-TiO2, while COOH with nano-ZnO), leading to different conformations of adsorbed HA. Interaction of HA phenolic OH with nano-TiO2 increased the pi-polarity/polarizability of adsorbed HA and, consequently, its phenanthrene adsorption affinity and isotherm nonlinearity. Interactions of COOH groups on HA aromatic rings with nano-ZnO would also increase the pi-polarity/polarizability of adsorbed HA and its phenanthrene adsorption affinity, whereas interactions of COOH groups on HA aliphatic chains with nano-ZnO would make the adsorbed HA be in a more condensed state with lower partitioning affinity. Increase in adsorption and decrease in partitioning were responsible for the more nonlinear phenanthrene isotherms of adsorbed HA than bulk HA.

Characteristics of Soil Organic Matter and Sorption of Phenanthrene, Naphthalene 1,3,5-TCB and o-Xylene

Nonlinear isotherm behavior has been reported for the sorption of hydrophobic organic compounds (HOCs) in soil/water systems, but the mechanisms are unclear. The model of “soft” and “hard” carbon domains has been extensively cited in the sorption literature to account for nonlinear sorption behaviors, but the structural compositions of soil organic matter (SOM) are not well understood. The objective of this study was to examine the characteristics of SOM and the effect of SOM heterogeneity on sorption isotherm by elemental analysis, organic petrographic examination, scanning electron microscopy, 13C nuclear magnetic resonance and studying the sorption behaviors of phenanthrene, naphthalene, 1,3,5-trichlorobenzene and o-xylene in soil and its isolated fractions, humic acid (HA) and humin (denser particulates and lighter particulates). DP mainly contained low maturation and high paraffinic carbon huminite. LP was composed of inertinite, huminite, vitrinite and exinite, with smaller particle size and higher maturation than DP. Humic acid approached the lignite coal rank. All isotherms were nonlinear, and nonlinearity increased in the following order: HA > DP > soil > BE > LP. The sorption of HOCs in soil was primarily regulated by SOM. Humic acid seemed to be the soft carbon domain and insoluble condensed organic matter (humin) the hard carbon domain. Isotherm nonlinearity was negatively correlated with hydrophobicity and molecular size, while sorption capacity increased with increase of these parameters. Aliphatic structures of SOM, as observed for LP, could also contribute to both isotherm nonlinearity and large sorption capacity.

Phenanthrene uptake by Medicago sativa L. under the influence of an arbuscular mycorrhizal fungus

Phenanthrene uptake by Medicago sativa L. was investigated under the influence of an arbuscular mycorrhizal fungus. Inoculation of lucerne with the arbuscular mycorrhizal fungus Glomus etunicatum L. resulted in higher phenanthrene accumulation in the roots and lower accumulation in the shoots compared to non-mycorrhizal controls. Studies on sorption and desorption of phenanthrene by roots and characterization of heterogeneity of mycorrhizal and non-mycorrhizal roots using solid-state 13C nuclear magnetic resonance spectroscopy ( 13C NMR) demonstrated that increased aromatic components due to mycorrhizal inoculation resulted in enhanced phenanthrene uptake by the roots but lower translocation to the shoots. Direct visualization using two-photon excitation microscopy (TPEM) revealed higher phenanthrene accumulation in epidermal cells of roots and lower transport into the root interior and stem in mycorrhizal plants than in non-mycorrhizal controls. These results provide some insight into the mechanisms by which arbuscular mycorrhizal inoculation may influence the uptake of organic contaminants by plants.

Effect of biosurfactant on the sorption of phenanthrene onto original and H2O2-treated soils

The objective of this study was to examine the effect of biosurfactant on the sorption of phenanthrene (PHE) onto the original or H2O2-treated black loamy soil (typic isohumisols) and red sandy soil (typic ferralisols). The sorption isotherms were performed with the original and "soft" carbon-removed soils in the presence and absence of biosurfactant (200 mg/L). The sorption and degradation of biosurfactant were investigated. The result showed that organic matter played an important role in PHE sorption onto the black loamy and red sandy soils, and the PHE sorption isotherms on the "soft" carbon-removed soils exhibited more nonlinearity than those on the original soils. The values of partition coefficient (Kd) on the original black loamy soil with or without 200 mg/L biosurfactant were 181.6 and 494.5 mL/g, respectively. Correspondingly, in the red sandy soil, Kd was 246.4 and 212.8 mL/g in the presence or absence of biosurfactant, respectively. The changes of Kd suggested that biosurfactant inhibited PHE sorption onto the black loamy soil, but facilitated PHE sorption onto the red sandy soil. The nonlinearity of PHE sorption isotherm was decreased in the presence of biosurfactant. Site specific sorption might occur during PHE sorption onto both the original and the "soft" carbon-removed soils in the presence of biosurfactant. It was noted that biosurfactant could also be sorbed onto soils. The maximal sorption capacity of the red sandy soil for biosurfactant was (76.9 +/- 0.007) microg/g, which was 1.31 times that of black loamy soil. Biosurfactant was degraded quickly in the two selected soils, and 92% of biosurfactant were mineralized throughout the incubation experiment for 7 d. It implied that biosurfactant should be added frequently when the remediation of polycyclic aromatic hydrocarbon (PAH)-contaminated soils was conducted through PAH desorption approach facilitated by biosurfactant.

Effects of temperature and surfactants on naphthalene and phenanthrene sorption by soil

Adsorption experiments were carried out to investigate the sorption behaviors of naphthalene and phenanthrene in six different soils and to determine the effects of temperature, linear alkylbenzene sulfonate (LAS) and cetylrimethyl ammonium bromide (CTAB) on sorption. The results show that for a given sorbent phenanthrene exhibited greater nonlinear and stronger sorption than naphthalene. There was a strong negative correlation for the K oc values with organic carbon content ( f oc). The increase of temperature was not favorable to sorption. Sorption decreased along with the increasing aqueous LAS concentration from 0 to 1000 mg/L. At low CTAB concentration (< 100 mg/L), the adsorption increased as CTAB hemimicelles formed on the soil surface. At high concentration, CTAB decreased the adsorption by occupying active hydrophobic adsorption sites and solubilization of naphthalene and phenanthrene.

Transport of Colloids and Associated Hydrophobic Organic Chemicals through a Natural Media Filter

In this project, the ability of natural media filtration (NMF) to remove colloidal particles and associated hydrophobic organic compounds from the aqueous phase was evaluated by performing sorption and transport experiments with leaf compost media. Phenanthrene sorption isotherm experiments for compost and model colloidal (latex) particles found that phenanthrene has a greater affinity for the colloidal particles than for the compost materials. In column experiments, the transport of phenanthrene through the NMF in the presence and absence of two colloidal particles with different hydrophobicities [sulfate (more hydrophobic) and carboxylate (less hydrophobic)] showed that the effluent phenanthrene concentration in the presence of colloids, particularly sulfate latex particles, is much higher than that in the absence of colloids. The results from a mathematical model used to evaluate data from the column experiments suggest that enhancement of contaminant transport can be significant under the following conditions: high colloidal concentrations, high partition coefficient between contaminant and colloids, or a slow desorption rate of contaminant from colloids.

Phenanthrene Sorption by Fruit Cuticles and Potato Periderm with Different Compositional Characteristics

Phenanthrene sorption by fruit cuticles (tomato, apple, and grape), potato tuber periderm, and their fractions were investigated to elucidate effects of compositional characteristics on affinity of plant cuticle (above-ground) and periderm (below-ground) with hydrophobic organic contaminants (HOCs). The distinct roles of the extractable lipids (waxes), the depolymerizable lipids (cutin/suberin), the nonsaponifiable lipids (cutan/suberan) and polysaccharide are discussed. The cutin/suberin rather than waxes dominates the sorption properties of bulk cuticle/periderm, but the sorption coefficient (K(d)) is linearly correlated with the total lipid contents. Polysaccharide plays a negative role in HOC sorption due to its obviously poor affinity with HOCs and restriction effect on the other powerful sorptive regions in cuticle/periderm. The significantly lower sorption of periderm than cuticle is attributed to the former having higher polysaccharide and lower depolymerizable lipids. The linear correlation of K(d) of bulk cuticle/periderm with polysaccharide content is observed for a potential prediction of plant uptake.