4.7 Article

Surface reactivity of α-Al2O3 and mechanisms of phosphate sorption: In situ ATR-FTIR spectroscopy and ζ potential studies

期刊

JOURNAL OF COLLOID AND INTERFACE SCIENCE
卷 342, 期 2, 页码 437-444

出版社

ACADEMIC PRESS INC ELSEVIER SCIENCE
DOI: 10.1016/j.jcis.2009.10.057

关键词

Alumina-solution interface; Phosphate ions; Adsorption; Surface precipitation; In situ spectroscopy; zeta potential; Surface charge

资金

  1. REALISE
  2. Alsace Region Research Network in Environmental Sciences and Engineering
  3. GNR PARIS

向作者/读者索取更多资源

We have investigated the effect of solution parameters on the adsorption of phosphate ions and on charges and structures, i.e., on the nature of species, at the alpha-Al2O3 colloid/solution interface by using the batch method, potential measurements, and in situ ATR-FTIR spectroscopy. The uptake of phosphate decreases with the extent of surface deprotonation (i.e., pH), imparts negative charges to the colloid surface, and induces IEP shifts showing chemical sorption. Use of complementary techniques provides evidence that phosphate is sorbed at low pH (3.3) by a combination of surface reactions of complexation and precipitation, whose relative contributions depend on phosphate loading. Surface complexation includes fast reactions of ligand exchange with single coordinated hydroxyls, and electrostatic attraction of H2PO4 ions at positively charged surface sites. This is supported by experiments at low coverage showing sharp and linear decrease of potential (i.e., surface charge) with amount of phosphate sorbed. At high coverage, potential values are low and independent of phosphate loading. Formation of surface precipitates of AI-phosphate is inferred from the assignment of the ATR-FTIR absorption band at 1137 cm(-1), whose intensity increases with phosphate solution content and reaction time, to the P-O-stretching vibration mode for phosphate sorbed at high concentrations on alpha-Al2O3. In situ ATR-FTIR spectroscopy reveals also structural reorganizations of surface hydroxyls with time, due to surface hydration and to surface precipitation continuing over extended periods along alumina dissolution. (C) 2009 Elsevier Inc. All rights reserved.

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