Some aspects of the glyphosate adsorption on montmorillonite and its calcined form
Influences of pH and ionic strength on the aggregation of montmorillonite particles in the presence or absence of glyphosate (PMG) were studied. Adsorption isotherms and X-ray diffraction indicated that ligand exchange is the main mechanism of PMG adsorption. The surface coverage increased with the...
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2007
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| LEADER | 13542caa a22013577a 4500 | ||
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| 001 | PAPER-6637 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518203620.0 | ||
| 008 | 190411s2007 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-33947125896 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 030 | |a ACLSE | ||
| 100 | 1 | |a Damonte, M. | |
| 245 | 1 | 0 | |a Some aspects of the glyphosate adsorption on montmorillonite and its calcined form |
| 260 | |c 2007 | ||
| 270 | 1 | 0 | |m dos Santos Afonso, M.; Departamento de Química Inorgánica, Analítica y Química Física, INQUIMAE, Facultad de Ciencias Exactas y Naturales, Ciudad Universitaria, Pabellon II, C1428EHA Buenos Aires, Argentina; email: dosantos@qi.fcen.uba.ar |
| 506 | |2 openaire |e Política editorial | ||
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| 520 | 3 | |a Influences of pH and ionic strength on the aggregation of montmorillonite particles in the presence or absence of glyphosate (PMG) were studied. Adsorption isotherms and X-ray diffraction indicated that ligand exchange is the main mechanism of PMG adsorption. The surface coverage increased with the ionic strength and was more noticeable at high PMG concentration indicating inner-sphere surface complexation. At low PMG concentration the inner-sphere surface complexes are located of the external clay mineral surface while at high PMG concentration the surface complexes are also formed in the interlayer space. © 2006 Elsevier B.V. All rights reserved. |l eng | |
| 536 | |a Detalles de la financiación: Universidad de Buenos Aires | ||
| 536 | |a Detalles de la financiación: Secretaría de Ciencia y Técnica, Universidad de Buenos Aires, UBACyT X043, PICT 13-08893 | ||
| 536 | |a Detalles de la financiación: Authors acknowledge Universidad de Buenos Aires, Secretaría de Ciencia y Técnica and ANPCyT-FONCyT for financial support through UBACyT X043 and PICT 13-08893 projects respectively. Dr. Rosa M Torres Sánchez is a member of CONICET. Authors also acknowledge thereviewers for their comments that improve the discussion. | ||
| 593 | |a Departamento de Química Inorgánica, Analítica y Química Física, INQUIMAE, Facultad de Ciencias Exactas y Naturales, Ciudad Universitaria, Pabellon II, C1428EHA Buenos Aires, Argentina | ||
| 593 | |a CETMIC, Camino Centenario y 506, (b1897ZCA) M.B. Gonnet, Argentina | ||
| 690 | 1 | 0 | |a ADSORPTION |
| 690 | 1 | 0 | |a GLYPHOSATE |
| 690 | 1 | 0 | |a MONTMORILLONITE |
| 690 | 1 | 0 | |a THERMAL REACTION |
| 690 | 1 | 0 | |a ADSORPTION |
| 690 | 1 | 0 | |a ADSORPTION ISOTHERMS |
| 690 | 1 | 0 | |a AGGLOMERATION |
| 690 | 1 | 0 | |a COMPLEXATION |
| 690 | 1 | 0 | |a IONIC STRENGTH |
| 690 | 1 | 0 | |a PARTICLES (PARTICULATE MATTER) |
| 690 | 1 | 0 | |a PH EFFECTS |
| 690 | 1 | 0 | |a X RAY DIFFRACTION ANALYSIS |
| 690 | 1 | 0 | |a CALCINED FORM |
| 690 | 1 | 0 | |a GLYPHOSATE |
| 690 | 1 | 0 | |a SURFACE COMPLEXATION |
| 690 | 1 | 0 | |a THERMAL REACTION |
| 690 | 1 | 0 | |a CLAY MINERALS |
| 690 | 1 | 0 | |a ADSORPTION |
| 690 | 1 | 0 | |a AGGREGATION |
| 690 | 1 | 0 | |a CONCENTRATION (COMPOSITION) |
| 690 | 1 | 0 | |a GLYPHOSATE |
| 690 | 1 | 0 | |a IONIC COMPOSITION |
| 690 | 1 | 0 | |a ISOTHERM |
| 690 | 1 | 0 | |a LIGAND |
| 690 | 1 | 0 | |a MONTMORILLONITE |
| 690 | 1 | 0 | |a X-RAY DIFFRACTION |
| 650 | 1 | 7 | |2 spines |a PH |
| 700 | 1 | |a Torres Sánchez, R.M. | |
| 700 | 1 | |a dos Santos Afonso, M. | |
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