Abstract
The final distribution of the CaO within Ca-treated clays was determined many years after the original treatment, i.e., when the soil-CaO reaction was completed, along with a study of evolution of the corresponding pH. The results reveal that the value of pH accepted in the literature as an indication of the end of the reaction, may not be the actual case.
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Castaño M.V., López-Lara T., López C.C. An study on laboratory-aged CaO-treated soils. Paper sent to publication to the Electronic Journal of Geotechnical Engineering, http://geotech.civen.okstate.edu/ejge/, UAQ, México, (2000).
Castaño M.V., López-Lara T., López C.C. Comparative study of the effectiveness of different additives on the expansion behavior of clays. Vol. 4, Electronic Journal of Geotechnical Engineering, http://geotech.civen.okstate.edu/ejge/Ppr9904/lopez9904.htm, UAQ, México (1999).
Castaño, M. V., López-Lara, T., & López, C. C. (2000b). Reaction kinetics of an expansive soil stabilized with calcium oxide. UAQ, México: Paper sent to publication to the Soils and Foundations.
Fernández Loaiza, Carlos –Mejoramiento y Estabilización de Suelos- Ed. Limusa, México City, (1982).
Joint Committee on Power Diffraction Standards del International Center for Diffraction Data. Pennsylvania, USA (1950–1988).
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López-Lara, T., López-Cajún, C., Alcocer, S. et al. Final Distribution of CaO and pH Evolution in CaO-treated Clays. Water Air Soil Pollut 225, 2068 (2014). https://doi.org/10.1007/s11270-014-2068-9
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DOI: https://doi.org/10.1007/s11270-014-2068-9