2017
DOI: 10.1016/j.enggeo.2016.07.016
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Failures in transport infrastructure embankments

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Cited by 76 publications
(47 citation statements)
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“…These environmental cycles of wetting and drying cause cyclic volume change that 8 can lead to the accumulation of irrecoverable plastic strains resulting in mobilisation 9 of post-peak strength and progressive failure (Take, 2003;Take & Bolton, 2004;10 Take & Bolton, 2011). This mechanism of shallow first-time failure due to repeated 11 environmental stress cycles and progressive failure, known as seasonal ratcheting 12 (Take & Bolton, 2011), has been observed in high-plasticity clay rail infrastructure 13 slopes (Briggs, et al, 2017), and was shown conclusively through centrifuge 14 experimentation (Take & Bolton, 2011). The mechanism of seasonal ratcheting in 15 high-plasticity clay slopes is the focus of the study reported in this paper.…”
Section: List Of Notationmentioning
confidence: 84%
See 1 more Smart Citation
“…These environmental cycles of wetting and drying cause cyclic volume change that 8 can lead to the accumulation of irrecoverable plastic strains resulting in mobilisation 9 of post-peak strength and progressive failure (Take, 2003;Take & Bolton, 2004;10 Take & Bolton, 2011). This mechanism of shallow first-time failure due to repeated 11 environmental stress cycles and progressive failure, known as seasonal ratcheting 12 (Take & Bolton, 2011), has been observed in high-plasticity clay rail infrastructure 13 slopes (Briggs, et al, 2017), and was shown conclusively through centrifuge 14 experimentation (Take & Bolton, 2011). The mechanism of seasonal ratcheting in 15 high-plasticity clay slopes is the focus of the study reported in this paper.…”
Section: List Of Notationmentioning
confidence: 84%
“…′ = Bishop's generalised effective stress (kPa) = total stress (kPa) = pore air pressure (kPa) = pore water pressure (kPa) χ = is a parameter considering the area over which matric suction acts = matric suction (kPa) = degree of saturation = saturation = residual saturation = van Genuchten fitting parameter (kPa -1 ) = van Genuchten fitting parameter = saturated hydraulic conductivity = relative hydraulic conductivity of water phase (m/s) = relative hydraulic conductivity of air phase (m/s) * = nonlocal plastic strain = weighted volume ′ = is the weighting function = local plastic strain = global coordinate ′ = local coordinate = internal length = distance from the stress point to adjacent stress points = bulk modulus (kPa) = shear modulus (kPa) = specific volume = gradient of the swelling line = gradient of normal consolidation line = reference pressure (kPa) = specific volume at reference pressure following the swelling line = original specific volume at reference pressure ′ = Poisson's ratio = void ratio , = vertical saturated hydraulic conductivity (m/s) ,ℎ = horizontal saturated hydraulic conductivity (m/s) = overconsolidation ratio Introduction 1 Long-term deterioration of high-plasticity clay slopes due to seasonal wetting and 2 drying induced pore water pressure fluctuations driving effective stress cycles, has 3 been attributed as the cause of shallow (i.e. less than 2.5m deep) first-time failures in 4 clay infrastructure slopes (Take & Bolton, 2011;Briggs, et al, 2017). Within this 5 study, pore water pressure fluctuations and resulting effective stress cycles due to 6 environmental boundary conditions are referred to as environmental stress cycles.…”
Section: List Of Notationmentioning
confidence: 99%
“…This information obtained from instrumentation may be vital in understanding deterioration and modes of failure (of which there may be many); this information can feed back into improved conceptual and numerical models that seek to identify assets that may be at risk. In some geologies and environments, deterioration mechanisms are complex, and there is considerable progress still to be made in working out how to monitor these and incorporate them in models (Dijkstra & Dixon 2010;Springman et al 2012;Briggs et al 2017).…”
Section: Received 23 August 2016; Accepted 4 May 2017mentioning
confidence: 99%
“…1. Deep-seated failures typically occur due to weak foundation soils or after long periods of heavy rainfall, whereas shallow failures commonly occur due to short periods of intense rainfall [7,8]. The type of failure can be governed by pavement thickness, soil initial condition (embankment and subgrade) and the type of loading applied on the road pavement.…”
Section: Introductionmentioning
confidence: 99%
“…Driving forces include; external loading from recurring traffic loading and geohazards from rainfall, erosion and earthquakes. Such embankment failures can be identified as a slope failure which can either occur through the embankment as shallow slope failure or deep-seated slope failure [6,7], as showed in Fig. 1.…”
Section: Introductionmentioning
confidence: 99%