Sorption of Sulfonamide Pharmaceutical Antibiotics on Whole Soils and Particle‐Size Fractions
- 1 July 2004
- journal article
- Published by Wiley in Journal of Environmental Quality
- Vol. 33 (4) , 1331-1342
- https://doi.org/10.2134/jeq2004.1331
Abstract
Residues of pharmaceutical antibiotics are found in the environment, whose fate and effects are governed by sorption. Thus, the extent and mechanisms of the soil sorption of p‐aminobenzoic acid and five sulfonamide antibiotics (sulfanilamide, sulfadimidine, sulfadiazine, sulfadimethoxine, and sulfapyridine) were investigated using topsoils of fertilized and unfertilized Chernozem and their organic–mineral particle‐size fractions. Freundlich adsorption coefficients (Kf) ranged from 0.5 to 6.5. Adsorption increased with aromaticity and electronegativity of functional groups attached to the sulfonyl–phenylamine core. Adsorption to soil and particle‐size fractions increased in the sequence: coarse silt < whole soil < medium silt < sand < clay < fine silt and was influenced by pH. Sorption nonlinearity (1/n ≤ 0.76) indicated specific interactions with functional groups of soil organic matter (SOM). Phenolic and carboxylic groups, N‐heterocyclic compounds, and lignin decomposition products were tentatively assigned as preferred binding sites using statistical analysis of pyrolysis–mass spectra and adsorption coefficients. Adsorption of sulfonamides to mineral soil colloids was weaker and resulted in a stronger desorption from clay‐size fractions. Moreover, steric accessibility of organic–mineral complexes in clay‐size fractions was significantly reduced. With a quantitative structure–property relationship (QSPR) model, combining the organic carbon concentration, the sulfonamides' chromatographic capacity factor (k′), and nondissociated species concentration (CFa), distribution coefficients (Kd) were estimated with a cross‐validated regression coefficient Q2 = 0.71. Modeling and molecular mechanics calculations of antibiotic–SOM complexes showed preferred site‐specific sorption via hydrogen bonds and van der Waals interactions. Distinct chemical structural properties, such as aromaticity and van der Waals volumes, correlated with the sorption data.Keywords
Funding Information
- GlaxoSmithKline
This publication has 41 references indexed in Scilit:
- Nonsingular Sorption of Organic Compounds in Soil: The Role of Slow KineticsJournal of Environmental Quality, 2000
- Thermal stability and composition of mineral‐bound organic matter in density fractions of soilEuropean Journal of Soil Science, 1999
- Three-dimensional, Molecular Structures of Humic Acids and Their Interactions with Water and Dissolved ContaminantsInternational Journal of Environmental Analytical Chemistry, 1996
- Incorporating Nonextractable Atrazine Residues into Soil Size Fractions as a Function of TimeSoil Science Society of America Journal, 1996
- Effect on plants of sulphadimethoxine used in intensive farming (Panicum miliaceum, Pisum sativum and Zea mays)Agriculture, Ecosystems & Environment, 1995
- COMPONENTS AND PARTICLE SIZE FRACTIONS INVOLVED IN ATRAZINE ADSORPTION BY SOILS1Soil Science, 1984
- Adsorption of Diuron and 2,4,5‐T on Soil Particle‐Size SeparatesJournal of Environmental Quality, 1983
- ADSORPTION OF SUBSTITUTED PHENOLS BY SOILSoil Science, 1982
- Iron Oxide Removal from Soils and Clays by a Dithionite-Citrate System Buffered with Sodium BicarbonateClays and clay minerals (National Conference on Clays and Clay Minerals), 1958
- Adsorption of Gases in Multimolecular LayersJournal of the American Chemical Society, 1938