Experimental study on the cyclic resistance of a natural loess from Northern France

TL;DR

This study investigates the cyclic resistance of natural loess from Northern France through laboratory tests, revealing how initial water content and soil saturation influence its stability under cyclic loading conditions.

Contribution

It provides new insights into how initial water content affects the cyclic resistance of loess, highlighting the densification process during cyclic loading.

Findings

Soil at 2.2 m depth has lowest cyclic resistance.

Lower initial water content increases cyclic resistance.

Densification occurs during initial cyclic loadings.

Abstract

In order to analyze the instability phenomenon observed along the Northern High Speed Line of R\'eseau Ferr\'e de France (RFF), soil blocks were taken at a site near the railway, at four different depths (1.2, 2.2, 3.5 and 4.9 m). Cyclic triaxial tests were carried out on saturated and unsaturated soil specimens. The results from tests on initially saturated specimens showed that the soil taken at 2.2 m depth has the lowest resistance to cyclic loading, in relation to its highest porosity and lowest clay fraction. This soil was then studied at unsaturated state with various initial water contents. Unsaturated soil specimens were first subjected to cyclic loadings to decrease their volume. These cyclic loadings was stopped when the volume decrease was approximately equal to the initial pore air volume, or when the pores filled by air were eliminated and the soil was considered to become saturated. Afterwards, the back-pressure tubing was saturated with de-aired water and cycles were applied under undrained condition. Significant effect of initial water content was evidenced: the lower the initial water content, the higher the cyclic resistance. This can be explained by the densification of the soil during the initial cyclic loadings.