Drained Residual Strength of Texcoco Clays Under Different Testing Conditions

This research presents the results of a study into the drained residual strength of high plastic remoulded clays from Valley of Mexico, specifically (a) former Lake Texcoco, located northeast of Mexico City, and (b) Academy of San Carlos, situated in the city center. Using a standard ring shear device following several testing procedures (single stage, multistage, pre-shear and flush). Specimens were subjected to torsional shear stresses with a displacement rate of 0.10 mm/min. The procedure that was adopted in this study was a single stage test. Tests performed using displacement rates of 0.01, 0.10, and 1.00 mm/min with different interfaces (porous stone, mortar, and steel) showed that the increase in displacement rate caused an increase in the residual friction angle, regardless of the type of interface. Other tests performed consolidating the samples under the same normal stress and sheared under the same displacement rate showed that increasing the consolidation time led to an increase in peak strength while the residual strength remained practically unchanged. This same behaviour was observed in another series of tests performed with OCR values of 1, 2, and 3.

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Publication Details

Journal
Geotechnical and Geological Engineering
Published
2026-02-25
DOI
https://doi.org/10.1007/s10706-025-03603-3
Citations
1
Primary Topic
Landfill Environmental Impact Studies
Type
article
Field-Weighted Citation Impact
35.31

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article

Drained Residual Strength of Texcoco Clays Under Different Testing Conditions

Ovando Shelley Efraín, Hernández Guadarrama F. Javier
1 citations
Geotechnical and Geological Engineering
Landfill Environmental Impact Studies
35.31
article

Drained Residual Strength of Texcoco Clays Under Different Testing Conditions

Ovando Shelley Efraín, Hernández Guadarrama F. Javier
article en
1 citations

Abstract

This research presents the results of a study into the drained residual strength of high plastic remoulded clays from Valley of Mexico, specifically (a) former Lake Texcoco, located northeast of Mexico City, and (b) Academy of San Carlos, situated in the city center. Using a standard ring shear device following several testing procedures (single stage, multistage, pre-shear and flush). Specimens were subjected to torsional shear stresses with a displacement rate of 0.10 mm/min. The procedure that was adopted in this study was a single stage test. Tests performed using displacement rates of 0.01, 0.10, and 1.00 mm/min with different interfaces (porous stone, mortar, and steel) showed that the increase in displacement rate caused an increase in the residual friction angle, regardless of the type of interface. Other tests performed consolidating the samples under the same normal stress and sheared under the same displacement rate showed that increasing the consolidation time led to an increase in peak strength while the residual strength remained practically unchanged. This same behaviour was observed in another series of tests performed with OCR values of 1, 2, and 3.

Geotechnical and Geological EngineeringVol. 44(3)
Universidad Nacional Autónoma de México (MX)
Consejo Nacional de Ciencia y Tecnología
Openalex Percentile: Top 0%
Landfill Environmental Impact Studies
35.31
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Drained Residual Strength of Texcoco Clays Under Different Testing Conditions — Ovando Shelley Efraín, Hernández Guadarrama F. Javier · Geotechnical and Geological Engineering (2026) | TGRS Research Map | TGRS