Analysis of massive sulphate attack to cement-treated compacted soils

The paper describes the heave experienced by two embankments providing access to a bridge located in a high-speed railway line. The compacted soil, a mixture of a low plasticity clay, sand and gravel, had a significant sulphate content (2 – 2.5%). The embankments received a reinforcing treatment by...

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Main Authors: Ramon-Tarragona Anna, Alonso Eduardo
Format: Article
Language:English
Published: EDP Sciences 2020-01-01
Series:E3S Web of Conferences
Online Access:https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/55/e3sconf_e-unsat2020_01009.pdf
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spelling doaj-9324f9d5bd77439da89671d0116bc1a72021-04-02T12:52:38ZengEDP SciencesE3S Web of Conferences2267-12422020-01-011950100910.1051/e3sconf/202019501009e3sconf_e-unsat2020_01009Analysis of massive sulphate attack to cement-treated compacted soilsRamon-Tarragona AnnaAlonso Eduardo0Centre Internacional de Mètodes Numèrics en EnginyeriaThe paper describes the heave experienced by two embankments providing access to a bridge located in a high-speed railway line. The compacted soil, a mixture of a low plasticity clay, sand and gravel, had a significant sulphate content (2 – 2.5%). The embankments received a reinforcing treatment by mixing the soil with cement in the proximity of the bridge abutments. In addition, a grid of grouting columns provided more stiffness to the embankments. The embankments experienced a fast heaving rate (around 4 mm/month) in the areas improved by cement mixing. Precision extensometers indicated that heave concentrated in the upper 6 – 8 m of the embankments. The sulphate content reduced sharply to 0.25% at increasing depth. No heave was detected in these deeper zones. The swelling was found to be associated with the development of thaumasite and ettringite minerals. The presence of clay, cement and sulphates in the compacted soils and the infiltration of water from rainfall events are ideal conditions for the growth of the mentioned minerals. Long-term tests performed on compacted samples provided a good evidence of the phenomena developing in situ. A chemical modelling of the mineral changes at the soil-cement interface provided an additional insight into the development of swelling, which could last for a long time (several years). Accordingly, it was decided to underpin the railway track and to excavate the upper active volume of the embankments. This solution went in parallel with train service, which was never interrupted.https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/55/e3sconf_e-unsat2020_01009.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Ramon-Tarragona Anna
Alonso Eduardo
spellingShingle Ramon-Tarragona Anna
Alonso Eduardo
Analysis of massive sulphate attack to cement-treated compacted soils
E3S Web of Conferences
author_facet Ramon-Tarragona Anna
Alonso Eduardo
author_sort Ramon-Tarragona Anna
title Analysis of massive sulphate attack to cement-treated compacted soils
title_short Analysis of massive sulphate attack to cement-treated compacted soils
title_full Analysis of massive sulphate attack to cement-treated compacted soils
title_fullStr Analysis of massive sulphate attack to cement-treated compacted soils
title_full_unstemmed Analysis of massive sulphate attack to cement-treated compacted soils
title_sort analysis of massive sulphate attack to cement-treated compacted soils
publisher EDP Sciences
series E3S Web of Conferences
issn 2267-1242
publishDate 2020-01-01
description The paper describes the heave experienced by two embankments providing access to a bridge located in a high-speed railway line. The compacted soil, a mixture of a low plasticity clay, sand and gravel, had a significant sulphate content (2 – 2.5%). The embankments received a reinforcing treatment by mixing the soil with cement in the proximity of the bridge abutments. In addition, a grid of grouting columns provided more stiffness to the embankments. The embankments experienced a fast heaving rate (around 4 mm/month) in the areas improved by cement mixing. Precision extensometers indicated that heave concentrated in the upper 6 – 8 m of the embankments. The sulphate content reduced sharply to 0.25% at increasing depth. No heave was detected in these deeper zones. The swelling was found to be associated with the development of thaumasite and ettringite minerals. The presence of clay, cement and sulphates in the compacted soils and the infiltration of water from rainfall events are ideal conditions for the growth of the mentioned minerals. Long-term tests performed on compacted samples provided a good evidence of the phenomena developing in situ. A chemical modelling of the mineral changes at the soil-cement interface provided an additional insight into the development of swelling, which could last for a long time (several years). Accordingly, it was decided to underpin the railway track and to excavate the upper active volume of the embankments. This solution went in parallel with train service, which was never interrupted.
url https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/55/e3sconf_e-unsat2020_01009.pdf
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