Spatial Microstructural Ordering of Expansive Clay Minerals


Por: Lopez-Lara, T., Hernandez-Zaragoza, J. B., Carreon-Freyre, D., Cerca, M., Rojas-Gonzalez, E., Franco, A. G. Minor, Martinez-Barrera, G., Salgado-Delgado, R.

Publicada: 1 ene 2018
Categoría: Civil and structural engineering

Resumen:
The volumetric change within soils containing expanding clays depends upon their spatial ordering and their mineralogy. So this work studies the spatial microstructural ordering and mineralogy of different expanding clays in order to correlate them with some of their geotechnical properties (plasticity, classification, and expansion). The clay microstructure was obtained using X-ray diffraction, and sweeping electronic microscopy. Physical characterization includes pH analysis. Clays with greater swelling (12.1-14.6% expansion) present greater agglomeration (gathering) (20-50 microns) in a flocculated structure that mainly contained sodic montmorillonite with 14-22 angstrom openings and 8.28 average pH, which indicates high electron concentrations with border-face interactions. Clays with the least expansion (7.6%) present lower agglomerations (5-10 microns) with face-to-face contacts within a dispersed structure that mainly contained calcium montmorillonite with openings lower than 15 angstrom and pH 7.56, which indicates a low electron concentration and face-to-face interaction. Major clay expansion corresponds to a greater size agglomerates, greater opening between particles, and greater pH presenting border-face and face-to-face interactions of a flocculent structure. Yet, the soils with lower expansion only present face-to-face interactions corresponding to a dispersed structure.

Filiaciones:
Lopez-Lara, T.:
 Univ Autonoma Queretaro, Fac Ingenieria, Div Estudios Posgrad, Santiago De Queretaro 76010, Qro, Mexico

Hernandez-Zaragoza, J. B.:
 Univ Autonoma Queretaro, Fac Ingenieria, Div Estudios Posgrad, Santiago De Queretaro 76010, Qro, Mexico

Carreon-Freyre, D.:
 Univ Nacl Autonoma Mexico, Ctr Geociencias, Lab Mecan Multiescalar Geosistemas, Blvd Juriquilla 3001,Col Juriquilla, Queretaro De Artea 76230, Qro, Mexico

Cerca, M.:
 Univ Nacl Autonoma Mexico, Ctr Geociencias, Lab Mecan Multiescalar Geosistemas, Blvd Juriquilla 3001,Col Juriquilla, Queretaro De Artea 76230, Qro, Mexico

Rojas-Gonzalez, E.:
 Univ Autonoma Queretaro, Fac Ingenieria, Div Estudios Posgrad, Santiago De Queretaro 76010, Qro, Mexico

Franco, A. G. Minor:
 Univ Autonoma Nuevo Leon, Fac Ingn Civil, Avenida Univ Fidel Velazquez Ciudad Univ, San Nicol Ios Garza 66450, NL, Mexico

Martinez-Barrera, G.:
 Univ Autonoma Estado Mexico, Fac Quim, LIDMA, Km 12 Carretera Toluca Atlacomulco, San Cayetano 50200, MI, Mexico

Salgado-Delgado, R.:
 Inst Tecnol Zacatepec, Div Estudios Posgrad & Invest, Calzada Tecnol 27,Col Ctr, Zacatepec 62780, Mor, Mexico
ISSN: 16878086
Editorial
HINDAWI LTD, ADAM HOUSE, 3RD FLR, 1 FITZROY SQ, LONDON, W1T 5HF, ENGLAND, Estados Unidos America
Tipo de documento: Article
Volumen: 2018 Número:
Páginas:
WOS Id: 000430234900001

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