4.7 Article

Coating magnetite alters the mechanisms and site energy for sulfonamide antibiotic sorption on biochar

期刊

JOURNAL OF HAZARDOUS MATERIALS
卷 409, 期 -, 页码 -

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ELSEVIER
DOI: 10.1016/j.jhazmat.2020.125024

关键词

Biochar; Sorption; Sulfonamides; Mean of site energy

资金

  1. Open Project of State Key Laboratory of Urban Water Resource and Environment, Harbin Institute of Technology [ES201913]

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The presence of magnetite improved oxygen-containing groups and regulation of pi-systems within biochar, affecting the sorption capacities of sulfonamides. Positive correlations were found between site energy and oxygen content or pore volume of magnetite-coating biochars, indicating potential high energy sites for pi-pi interactions, H-bonding, and pore-filling during antibiotic sorption.
Magnetite-coating biochar (MBC) is a promising remediator for antibiotic contamination. Accurate models describing the sorption affinity are required to better understand the role of minerals. In this study, the presence of magnetite led to the improvements of oxygen-containing groups (i.e. (CO)-O-=) and regulation of pi-systems within BC. Based on Dubinin-Ashtakhov (DA) model, the differences of site energy (E-m) and sorption heterogeneity (sigma(e)*) led to the variances between sorption capacities of sulfonamides (SAs). The positive correlations between E-m and the oxygen content or pore volume of MBCs indicated that pi-pi interactions, H-bonding, and pore-filling may act as the high energy sites. Moreover, sigma(e)* was related to the distribution of magnetite on BC and their porosities. These results suggested that compared to BCs, the coating minerals improved the pi-interaction assisted H-bonding and proton configuration of antibiotic when sorbing on MBC. The negative correlations between the E(m)( )of different SAs with their molecular sizes and solubilities resulted from steric effects and competition with water, which further confirmed the proposed high energy sites on MBCs. This study provided the insightful information of site energy distribution and understanding of fate and transport of organic pollutants on BC when the iron minerals were embedded or coated.

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