Interaction of aminotriazole with montmorillonite and Mg-vermiculite at pH 4

The interaction of aminotriazole (AMT) al pH 4 on Wyoming monimorillunite (mainly with Na ions) and Mg-vermiculite has been studied by X-ray diffraction and infrared spectroscopy. The AMT is adsorbed on montmorillonite in the cationic form by cation exchange. The amount of pesticide adsorbed was 71 mEq/100 g, which comprises ∼91% of the CEC of this sample (78.2 mEq/100 g). Saturation was reached in 24 h, giving rise to a complex with basal spacing 12.5 Å. Vermiculite adsorbs 167 mEq/100 g, almost 20% greater than the CEC (141 mEq/100 g). and the basal spacing was stabilited at 13.68 Å after five weeks of treatment with AMT. A part of the AMT is adsorbed in cationic form, displacing a great pan of the exchangeable Mg2+ cations. The rest is adsorbed in molecular form by coordination to the Mg2+ cations which remain in the interlamellar space, removing a great amount of water, and remaining in the interlamellur space of vermiculite after wushing with water, probably because of a steric hindrance from the AMT cations adsorbed.

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Main Authors: Morillo González, Esmeralda, Pérez Rodríguez, José Luis, Rodríguez-Rubio, P., Maqueda Porras, Celia
Format: artículo biblioteca
Language:English
Published: Mineralogical Society (Great Britain) 1997
Online Access:http://hdl.handle.net/10261/62189
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spelling dig-irnas-es-10261-621892018-09-13T07:49:12Z Interaction of aminotriazole with montmorillonite and Mg-vermiculite at pH 4 Morillo González, Esmeralda Pérez Rodríguez, José Luis Rodríguez-Rubio, P. Maqueda Porras, Celia The interaction of aminotriazole (AMT) al pH 4 on Wyoming monimorillunite (mainly with Na ions) and Mg-vermiculite has been studied by X-ray diffraction and infrared spectroscopy. The AMT is adsorbed on montmorillonite in the cationic form by cation exchange. The amount of pesticide adsorbed was 71 mEq/100 g, which comprises ∼91% of the CEC of this sample (78.2 mEq/100 g). Saturation was reached in 24 h, giving rise to a complex with basal spacing 12.5 Å. Vermiculite adsorbs 167 mEq/100 g, almost 20% greater than the CEC (141 mEq/100 g). and the basal spacing was stabilited at 13.68 Å after five weeks of treatment with AMT. A part of the AMT is adsorbed in cationic form, displacing a great pan of the exchangeable Mg2+ cations. The rest is adsorbed in molecular form by coordination to the Mg2+ cations which remain in the interlamellar space, removing a great amount of water, and remaining in the interlamellur space of vermiculite after wushing with water, probably because of a steric hindrance from the AMT cations adsorbed. Peer Reviewed 2012-12-07T22:12:36Z 2012-12-07T22:12:36Z 1997 2012-12-07T22:12:36Z artículo http://purl.org/coar/resource_type/c_6501 issn: 0009-8558 e-issn: 1471-8030 Clay Minerals 32(2): 307-313 (1997) http://hdl.handle.net/10261/62189 10.1180/claymin.1997.032.2.11 en http://dx.doi.org/10.1180/claymin.1997.032.2.11 open Mineralogical Society (Great Britain)
institution IRNAS ES
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country España
countrycode ES
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libraryname Biblioteca del IRNAS España
language English
description The interaction of aminotriazole (AMT) al pH 4 on Wyoming monimorillunite (mainly with Na ions) and Mg-vermiculite has been studied by X-ray diffraction and infrared spectroscopy. The AMT is adsorbed on montmorillonite in the cationic form by cation exchange. The amount of pesticide adsorbed was 71 mEq/100 g, which comprises ∼91% of the CEC of this sample (78.2 mEq/100 g). Saturation was reached in 24 h, giving rise to a complex with basal spacing 12.5 Å. Vermiculite adsorbs 167 mEq/100 g, almost 20% greater than the CEC (141 mEq/100 g). and the basal spacing was stabilited at 13.68 Å after five weeks of treatment with AMT. A part of the AMT is adsorbed in cationic form, displacing a great pan of the exchangeable Mg2+ cations. The rest is adsorbed in molecular form by coordination to the Mg2+ cations which remain in the interlamellar space, removing a great amount of water, and remaining in the interlamellur space of vermiculite after wushing with water, probably because of a steric hindrance from the AMT cations adsorbed.
format artículo
author Morillo González, Esmeralda
Pérez Rodríguez, José Luis
Rodríguez-Rubio, P.
Maqueda Porras, Celia
spellingShingle Morillo González, Esmeralda
Pérez Rodríguez, José Luis
Rodríguez-Rubio, P.
Maqueda Porras, Celia
Interaction of aminotriazole with montmorillonite and Mg-vermiculite at pH 4
author_facet Morillo González, Esmeralda
Pérez Rodríguez, José Luis
Rodríguez-Rubio, P.
Maqueda Porras, Celia
author_sort Morillo González, Esmeralda
title Interaction of aminotriazole with montmorillonite and Mg-vermiculite at pH 4
title_short Interaction of aminotriazole with montmorillonite and Mg-vermiculite at pH 4
title_full Interaction of aminotriazole with montmorillonite and Mg-vermiculite at pH 4
title_fullStr Interaction of aminotriazole with montmorillonite and Mg-vermiculite at pH 4
title_full_unstemmed Interaction of aminotriazole with montmorillonite and Mg-vermiculite at pH 4
title_sort interaction of aminotriazole with montmorillonite and mg-vermiculite at ph 4
publisher Mineralogical Society (Great Britain)
publishDate 1997
url http://hdl.handle.net/10261/62189
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AT rodriguezrubiop interactionofaminotriazolewithmontmorilloniteandmgvermiculiteatph4
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