2009
DOI: 10.3208/sandf.49.421
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Experimental Study on the Cyclic Resistance of a Natural Loess from Northern France

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Cited by 21 publications
(3 citation statements)
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“…In this area, loess deposits were formed under periglacial conditions during the Quaternary period by the aeolian transport of silt particles eroded by a constant North West wind (Antoine 2002(Antoine , 2003, resulting in loess deposits characterized by a relative homogeneity, a low plasticity, a high porosity and a loose microstructure. These features explain the loess susceptibility to collapse when exposed to intense rainfall or accidental water leaking (Cui et al 2004, Delage et al, 2005, Yang et al, 2008, Munoz-Castelblanco et al 2011 as well as its liquefaction behaviour under cyclic loading (Karam et al 2009).…”
Section: Tested Loessmentioning
confidence: 99%
“…In this area, loess deposits were formed under periglacial conditions during the Quaternary period by the aeolian transport of silt particles eroded by a constant North West wind (Antoine 2002(Antoine , 2003, resulting in loess deposits characterized by a relative homogeneity, a low plasticity, a high porosity and a loose microstructure. These features explain the loess susceptibility to collapse when exposed to intense rainfall or accidental water leaking (Cui et al 2004, Delage et al, 2005, Yang et al, 2008, Munoz-Castelblanco et al 2011 as well as its liquefaction behaviour under cyclic loading (Karam et al 2009).…”
Section: Tested Loessmentioning
confidence: 99%
“…Indeed, in the case of northern line (Paris-Lille), a sub-grade of loess is involved. Under the effects of rainfall and dynamic loading, track instability problems were identified, leading to an extensive study to identify the main instability mechanisms (collapse upon wetting, cementation degradation upon cyclic loading and liquefaction in the saturated sate) and to find out an appropriate reinforcement technique such as grouting (Cui et al, 2007;Yang et al, 2008;Karam et al, 2009;Munoz-Castelblanco et al, 2011;2012a;2012b). In the case of Mediterranean Line (Paris-Marseille), a sub-grade of marl was encountered and its swelling due to the coupled effect of water infiltration and excavation-related unloading was revealed to be one of the main mechanisms for the significant track heave identified (Tang et al, 2009).…”
Section: Introductionmentioning
confidence: 99%
“…Indeed, in the case of northern line (ParisLille), a subgrade of loess is involved. Under the effects of rainfall and dynamic loading, track instability problems were identified, leading to an extensive study to identify the main instability mechanisms (collapse upon wetting, fatigue under large number of loading cycles and liquefaction in the saturated sate) [1][2][3][4][5][6]. In the case of Mediterranean Line (Paris -Marseille), a subgrade of marl was encountered and its swelling due to the coupled effect of water infiltration and excavation-related unloading was revealed to be one of the main mechanisms for the significant track heave identified [7].…”
Section: Introductionmentioning
confidence: 99%