2019
DOI: 10.1080/19475705.2019.1694230
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Characteristics and mechanisms of coupled road and rainfall-induced landslide in Sichuan China

Abstract: Field reconnaissance, geological mapping and photographic interpretation are utilized to study the failure mechanisms of July 2 catastrophic debris slide in 2017. The results suggested that the landslide was a reactivation of an ancient landslide after periods of relative dormancy, as manifestation of a retrogressive motion, which is triggered by the continuous engineering excavation as leads to rock mass unloading and decrease of mechanical properties of rock-soil mixture. The reactivated zone dominantly spre… Show more

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Cited by 25 publications
(5 citation statements)
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“…Figure 16 shows four typical entrainment modes due to the impacting force: (i) intact impact and scraping, (ii) fragmented impact and plough, (iii) flow-like entrainment, and (iv) overloading and entrainment [38,39]. In the ZHC landslide, after the materials slid from the source area, due to the topographic and material constraints, it loaded successively and accumulated on the middle and lower slopes in the overloading and entrainment zone, thus led to sequent failure continuously [40,41]. This entrainment mode is mainly caused by the energy of the upper landslide, which is similar to the second Baige landslide [37].…”
Section: Discussionmentioning
confidence: 99%
“…Figure 16 shows four typical entrainment modes due to the impacting force: (i) intact impact and scraping, (ii) fragmented impact and plough, (iii) flow-like entrainment, and (iv) overloading and entrainment [38,39]. In the ZHC landslide, after the materials slid from the source area, due to the topographic and material constraints, it loaded successively and accumulated on the middle and lower slopes in the overloading and entrainment zone, thus led to sequent failure continuously [40,41]. This entrainment mode is mainly caused by the energy of the upper landslide, which is similar to the second Baige landslide [37].…”
Section: Discussionmentioning
confidence: 99%
“…In addition, rainfall also reduces the shear strength of the soil and increases the self-weight of the slope. According to a large number of experimental studies (He et al 2019), the internal friction and cohesion will decrease with the increase of water content. The increase of the self-weight of the slope will also promote the force of the slide.…”
Section: Rainfall In Ltration Stagementioning
confidence: 99%
“…Diverse failure consequences can be observed in a varying soil slope consisting of weak materials (e.g., weak intercalation layer) because the failure surface tends to seek out the weakest path. In many occasions, due to extensive runout motions of landslides during the post-failure stage, substantial destruction can be observed on nearby structures (Yin et al 2009(Yin et al , 2016, which leads to severe threat and significant damages to human life and properties (Ma et al 2018;He et al 2019;Wang et al 2021). Studying the post-failure responses in heterogeneous soil slopes is rather complicated due to large deformations and interdependencies in spatially varying shear strengths.…”
Section: Introductionmentioning
confidence: 99%