Abstract:In the present study, the reduced adsorption of propanil on black carbon (BC) influenced by dissolved organic matter (DOM) was verified to be closely related to DOM molecule size and loading mode. Two congenetic carbons, a rice-residue-derived BC and the reduced product (RC), were characterized by similar specific surface area and different surface properties. Reduced product exhibits higher adsorption of propanil and DOM than BC. A series of model DOMs, including tannic acid (TA), pentagalloylglucose (PA), 3-… Show more
“…Moreover, the strong sorption domain (i.e. the micropore system) of the tiny BC fraction in the soils might be blocked or occupied by soil components such as DOC and mineral clays, thus attenuating the possible influence from BC (Kwon and Pignatello, 2005;Brändli et al, 2008;Xiao et al, 2012). Agarwal and Bucheli (2011) also observed the only governor of TOC in the distribution of PAHs in the organic carbon-rich agricultural soils.…”
Section: Effects Of Soil Properties On Extractability Of Pahs In Agedmentioning
Hard organic carbon Porosity Diffusion a b s t r a c t Sequestration and diffusion of three polycyclic aromatic hydrocarbons (PAHs) in seven Chinese soils were investigated for up to 200 days in sterile soil microcosms as functions of soil property and aging time. The aging of the PAHs, assessed using a mild extractant that removes primarily the labile fraction, showed a biphasic behavior. The rapid diffusion from labile to nonlabile domains was mainly dependent upon the distribution of meso-and micropore fraction and total organic carbon content. Meanwhile, the slow diffusion was found to decrease with the increase of the content of soil organic carbon, particularly of hard organic carbon (p < 0.01) and the meso-and micropore fraction, as well as with the increasing molecular size of PAHs. This work offers evidence that analyses of organic carbon fractionation and porosity are important to adequately assess the mechanistic basis of sequestration and diffusion of organic contaminants in soils.
“…Moreover, the strong sorption domain (i.e. the micropore system) of the tiny BC fraction in the soils might be blocked or occupied by soil components such as DOC and mineral clays, thus attenuating the possible influence from BC (Kwon and Pignatello, 2005;Brändli et al, 2008;Xiao et al, 2012). Agarwal and Bucheli (2011) also observed the only governor of TOC in the distribution of PAHs in the organic carbon-rich agricultural soils.…”
Section: Effects Of Soil Properties On Extractability Of Pahs In Agedmentioning
Hard organic carbon Porosity Diffusion a b s t r a c t Sequestration and diffusion of three polycyclic aromatic hydrocarbons (PAHs) in seven Chinese soils were investigated for up to 200 days in sterile soil microcosms as functions of soil property and aging time. The aging of the PAHs, assessed using a mild extractant that removes primarily the labile fraction, showed a biphasic behavior. The rapid diffusion from labile to nonlabile domains was mainly dependent upon the distribution of meso-and micropore fraction and total organic carbon content. Meanwhile, the slow diffusion was found to decrease with the increase of the content of soil organic carbon, particularly of hard organic carbon (p < 0.01) and the meso-and micropore fraction, as well as with the increasing molecular size of PAHs. This work offers evidence that analyses of organic carbon fractionation and porosity are important to adequately assess the mechanistic basis of sequestration and diffusion of organic contaminants in soils.
“…This relationship has been demonstrated in other carbon materials [24]. Our simulation results showed that the maximum numbers of water, EG, DMF, and NMP molecules that can be adsorbed per unit cell of GO are 490, 120, 97, and 70, respectively.…”
Section: Relationship Between the Interlayer Spacing Of Go And The Simentioning
confidence: 51%
“…The hydrodynamic diameter of a water molecule is ~ 2.7 Å [25]. The intercalation of a water monolayer causes the lattice of GO to expand by 2.2-2.5 Å [24]. The size of the DMF layer adsorbed by GO structure is ~ 4.4 Å [26].…”
Section: Relationship Between the Interlayer Spacing Of Go And The Simentioning
Graphene oxide (GO) contains numerous functional groups that facilitate the intercalation of polar solvents. The properties and applications of GO are closely related to its interlayer spacing. We report on the changes in the interlayer spacing of GO after the adsorption of water molecules and the polar organic solvents C 2 H 6 O 2 (EG), C 3 H 7 NO (DMF), C 5 H 9 NO (NMP). Experiments were conducted to investigate the variations in the functional groups and structure of GO after solvent adsorption, and they play a vital role in modeling and verifying the results of molecular dynamics simulation. The most stable GO structures are obtained through molecular dynamics simulation. The expansion of the interlayer spacing of GO after the adsorption of monolayer solvent molecules corresponds to the minimum three-dimensional size of the solvent molecules. The spatial arrangement of solvent molecules also contributes to the changes in interlayer spacing. Most adsorbed molecules are oriented parallel to the carbon plane of GO. However, as additional molecules are adsorbed into the interlaminations of GO, the adsorbed molecules are oriented perpendicular to the carbon plane of GO, and a large space forms between two GO interlayers. In addition, the role of large molecules in increasing interlayer spacing becomes more crucial than that of water molecules in the adsorption of binary solvent systems by GO.
“…After coexisting with 5 mg L −1 TA and GA, the maximum adsorbed capacity (q m ) of MCLR decreased to 92 and 6 %, respectively (Table 6S). This result indicated that TA acted as a strong competitor by occupying the effective adsorption sites for MCLR in the mesopore and macropore regions because of the larger molecule size of TA (1.93 nm×1.73 nm×1.32 nm) than MCLR (Xiao et al 2012). However, GA shows a slight influence on MCLR adsorption because the dominant adsorptive domain for GA is micropore, which is inaccessible to MCLR macromolecules.…”
Section: Effect Of Dommentioning
confidence: 90%
“…The three-dimensional size of MCLR was reported as 1.9 nm×1.5 nm×1.1 nm (Teng et al 2013). Therefore, the micropore regions (pore size <2 nm) may be unavailable for MCLR adsorption because the second widest dimension of MCLR (1.7× 1.5=2.55 nm) is 1.7 times larger than 2 nm (Xiao et al 2012). This notion is supported by evidence that the uptake of MCLR on micropore-based carbon is similar to that on nonporous carbon (Pendleton et al 2001).…”
The adsorption of microcystin-LR (MCLR) by biochar has never been well understood. For the first time, the unconventional adsorption of hydrophilic MCLR on wood-based biochars was comprehensively investigated as a function of biochar properties, environmental temperature, solution pH, coexisting dissolved organic matter (DOM), and polar organic competitors. High-temperature-prepared biochar from 700°C (BC-700) and low-temperature-prepared biochar from 300°C (BC-300) were characterized with significantly different surface areas but similar alkaline nature. Despite a very low surface area, BC-300 exhibited very high adsorption capacity, which implies the important contribution of surface groups to biochar. MCLR adsorption on biochars was pH dependent and was strongly reduced by macromolecular DOM. Polycarboxylic aliphatic acids and 2-(2-hydroxyethyl) guanidinium cation, which are similar to specific structural groups in MCLR, exhibited an evident competitive effect. The results indicated that both carboxylic and guanidino groups of MCLR serve significant functions in MCLR adsorption to biochar. The adsorption mechanisms may be primarily related to the columbic attractions and the hydrogen bonding interactions between MCLR and biochar surface. In particular, the irreversible adsorption enhancement of MCLR was observed on BC-700, which suggests that biochar amendment can aid in immobilizing MCLR from water to sediment, thereby prolonging MCLR environmental fate in biocharamended sediment.
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