Abstract
Purpose
The phosphate adsorption on natural adsorbents is of particular importance in regulating the transport and bioavailability of phosphates in environmental system. In soils, oxides are often associated with organic matter and form mineral-organic complexes. The aim of the present paper was to investigate the mechanisms of phosphate adsorption on these complexes.
Materials and methods
Phosphate adsorption on uncoated and humic acid (HA)-coated iron oxide complexes was investigated at different ionic strengths and pH by isotherm experiments and attenuated total reflectance Fourier transform infrared (ATR-FTIR) spectroscopy.
Results and discussion
Results showed that HA-coated iron oxide complexes caused a decrease in the specific surface area (SSA) and the isoelectric point (IEP) of oxides. Phosphate adsorption on iron oxides was insensitive to changes of ionic strength, while it increased on the complexes with increasing ionic strength. The presence of HA decreased the maximum adsorption and the affinity of phosphate on the complexes. The zeta potential of phosphate-bound iron oxides linearly reduced with the increment of phosphate surface coverage, while the zeta potential of complexes with adsorbed phosphate kept at the same level. ATR-FTIR analysis suggested the formation of phosphate-metal complexation. The presence of HA promotes the formation of the monodentate phosphate complexes at pH 4.5 and significantly influenced phosphate species at pH 8.5.
Conclusions
The amount of phosphate adsorbed was reduced, and the phosphate speciation was also influenced when phosphate was adsorbed on HA-coated iron oxide complexes compared with phosphate adsorption on pure goethite and hematite.
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Acknowledgments
We are grateful to the National Natural Science Foundation of China (Grant Nos. 41071165 and 30890130) for the financial support to the research. Thanks to Dr. Edward C. Mignot, Shandong University, for the linguistic advice.
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Responsible editor: Zhenli He
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Wang, H., Zhu, J., Fu, Q. et al. Phosphate adsorption on uncoated and humic acid-coated iron oxides. J Soils Sediments 16, 1911–1920 (2016). https://doi.org/10.1007/s11368-016-1383-8
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DOI: https://doi.org/10.1007/s11368-016-1383-8