2019
DOI: 10.1007/s12665-019-8767-1
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Triggering mechanism and reactivation probability of loess-mudstone landslides induced by rainfall infiltration: a case study in Qinghai Province, Northwestern China

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Cited by 16 publications
(7 citation statements)
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“…Xu et al [17,18] studied the effect of periodic water circulation on rock mass by P-Wave Velocity and found that the water-rock interaction changed the porosity of the rock pores and then affected its mechanical properties. Mu [19] studied the triggering mechanism and reactivation probability of a loess-mudstone landslide induced by rainwater infiltration, and concluded that shear strength of media is very sensitive to water content because of water-rock interaction, and landslide reactivation is controlled by the water sensitivity of media, especially the original sliding zone.…”
Section: Introductionmentioning
confidence: 99%
“…Xu et al [17,18] studied the effect of periodic water circulation on rock mass by P-Wave Velocity and found that the water-rock interaction changed the porosity of the rock pores and then affected its mechanical properties. Mu [19] studied the triggering mechanism and reactivation probability of a loess-mudstone landslide induced by rainwater infiltration, and concluded that shear strength of media is very sensitive to water content because of water-rock interaction, and landslide reactivation is controlled by the water sensitivity of media, especially the original sliding zone.…”
Section: Introductionmentioning
confidence: 99%
“…All the parameters used in this study contributed to the landslides' occurrence. According to various studies, moisture (precipitation) and topographical properties play a significant role in triggering landslides [76][77][78][79]. The excessive moisture in the soil increases the pore pressure, which decreases the shear strength of the soil and leads to slope failure [78].…”
Section: Landslide Early Warning System (Lews) and Land System Proces...mentioning
confidence: 99%
“…Sandstone forms a permeable layer, the mudstone is relatively water-resistant, and the contact zone between the two is made up of a highly watersaturated zone [25]. Studies have revealed that the presence of stagnant water in the residual soil layer and the increase in pore water pressure were the main reasons for rainfallinduced landslides [26]. The geological structure of Longquan Mountain is predominantly composed of a soft rock "red layer."…”
Section: Study Area Descriptionmentioning
confidence: 99%
“…Continuous rainfall is the primary cause of red bed landslides [26]. As shown in Figure 14, the field measurement date was February 2, 2021.…”
Section: Geofluidsmentioning
confidence: 99%