TY - JOUR
T1 - Influence of mesoporosity on the sorption of 2,4-dichlorophenoxyacetic acid onto alumina and silica
AU - Goyne, Keith W.
AU - Chorover, Jon
AU - Zimmerman, Andrew R.
AU - Komarneni, Sridhar
AU - Brantley, Susan L.
N1 - Funding Information:
The authors thank Mary Kay Amistadi for assistance, Drs. Bharat Newalkar and Stephen Stout for mineral synthesis and preparation, Dr. Towhid Hasan and Robin Guynn for performing ICPMS analyses, and Dr. Sunkyung Choi for performing XRD analyses. Financial support was provided by the Penn State Biogeochemical Research Initiative for Education (BRIE) sponsored by NSF (IGERT) Grant DGE-9972759 and the Penn State Materials Research Science and Engineering Center (MRSEC) sponsored by NSF Grant DMR-0080019.
PY - 2004/4/1
Y1 - 2004/4/1
N2 - Two SiO2 and three Al2O3 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 SiO2 solid, presumably because of electrostatic repulsion, but it did adsorb onto positively charged Al2O 3 adsorbents, resulting in concave isotherms. The Al 2O3 adsorbent of highest mesoporosity consistently adsorbed more 2,4-D per unit surface area than did the nonporous and less mesoporous Al2O3 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 Al2O3 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.
AB - Two SiO2 and three Al2O3 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 SiO2 solid, presumably because of electrostatic repulsion, but it did adsorb onto positively charged Al2O 3 adsorbents, resulting in concave isotherms. The Al 2O3 adsorbent of highest mesoporosity consistently adsorbed more 2,4-D per unit surface area than did the nonporous and less mesoporous Al2O3 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 Al2O3 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.
KW - 2,4-D
KW - ATR-FTIR spectroscopy
KW - Adsorption/desorption isotherms
KW - Freundlich isotherm
KW - Frumkin-Fowler-Guggenheim isotherm
KW - Mesoporosity
KW - Mineral transformation
KW - Mineral-organic interactions
KW - X-ray diffraction
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U2 - 10.1016/j.jcis.2003.12.040
DO - 10.1016/j.jcis.2003.12.040
M3 - Article
C2 - 14985017
AN - SCOPUS:1242270568
SN - 0021-9797
VL - 272
SP - 10
EP - 20
JO - Journal of Colloid And Interface Science
JF - Journal of Colloid And Interface Science
IS - 1
ER -