Influence of mesoporosity on the sorption of 2,4-dichlorophenoxyacetic acid onto alumina and silica

被引:26
作者
Goyne, KW
Chorover, J
Zimmerman, AR
Komarneni, S
Brantley, SL
机构
[1] Univ Arizona, Dept Soil Water & Environm Sci, Tucson, AZ 85721 USA
[2] Penn State Univ, Dept Crop & Soil Sci, University Pk, PA 16802 USA
[3] Penn State Univ, Dept Geosci, University Pk, PA 16802 USA
[4] Penn State Univ, Mat Res Inst, University Pk, PA 16802 USA
基金
美国国家科学基金会;
关键词
mesoporosity; X-ray diffraction; mineral transformation; 2,4-D; adsorption/desorption isotherms; Freundlich isotherm; Frumkin-Fowler-Guggenheim isotherm; ATR-FrIR spectroscopy; mineral-organic interactions;
D O I
10.1016/j.jcis.2003.12.040
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Two SiO(2) and three Al(2)O(3) adsorbents with varying degrees of mesoporosity (pore diameter 2-50 nm) were reacted with 2,4-dichlorophenoxyacetic acid (2,4-D) at pH 6 to investigate the effects of intraparticle mesopores on adsorption/desorption. Anionic 2,4-D did not adsorb onto either SiO(2) solid, presumably because of electrostatic repulsion, but it did adsorb onto positively charged Al(2)O(3) adsorbents, resulting in concave isotherms. The Al(2)O(3) adsorbent of highest mesoporosity consistently adsorbed more 2,4-D per unit. surface area than did the nonporous and less mesoporous Al(2)O(3) adsorbents over a range of initial 2,4-D solution concentrations (0.025-2.5 mM) and reaction times (30 min-55 d). Differences in adsorption efficiency were observed despite equivalent surface site densities on the three Al(2)O(3) adsorbents. Hysteresis between the adsorption/desorption isotherms was not observed, indicating that adsorption is reversible. Attenuated total reflectance-Fourier transform infrared (ATR-FTIR) spectroscopy studies confirm that 2,4-D adsorption does not occur via ligand exchange, but rather via electrostatic interaction. The results indicate that adsorbent intraparticle mesopores can result in consistently greater 2,4-D adsorption, but the amount adsorbed is dependent upon surface charge and the presence of adsorbent mesoporosity. The data also suggest that when mineral pores are significantly larger than the adsorbate, they do not contribute to diffusion-limited adsorption/desorption hysteresis. Adsorbent transformations through time are discussed. (C) 2004 Elsevier Inc. All rights reserved.
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页码:10 / 20
页数:11
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