4.7 Article

The Azijue debris flow induced by rainfall on 30 August 2020 in Ganluo County, Sichuan Province, southwestern China

Related references

Note: Only part of the references are listed.
Article Engineering, Geological

The Wuxie debris flows triggered by a record-breaking rainstorm on 10 June 2021 in Zhuji City, Zhejiang Province, China

Fawu Wang et al.

Summary: On 9 June 2021, Zhuji experienced the largest rainfall ever recorded, triggering several debris flows that caused casualties and the closure of a scenic area. The extreme rainfall event, complex topography, and abundant diluvium were the main contributing factors to the disastrous damage. Steep eluvial slopes and geometric properties of the gullies interacted significantly with diluvium erosion, resulting in mass enlargement and long-runout movement of the debris flows. Reasonable countermeasures played a role in reducing and mitigating such geodisasters.

LANDSLIDES (2022)

Article Engineering, Geological

Runout modeling and calibration of friction parameters of Kurichermala debris flow, India

Minu Treesa Abraham et al.

Summary: The study focused on the geotechnical investigation and back analysis of debris flows in Wayanad district, Kerala, India, caused by heavy rains during the monsoon seasons. The research provides important information for predicting the shape of possible debris flows and quantitative risk assessment in the future.

LANDSLIDES (2021)

Article Engineering, Geological

Discussions on the transformation conditions of Wangcang landslide-induced debris flow

Jian Guo et al.

Summary: The landslide-induced debris flow in Wangcang County, Sichuan Province on August 14, 2020, resulted in three deaths and two destroyed houses. Factors such as continuous rainfall, interbedded marlstone with structural planes, and changes in slope gradient contributed to the disaster. The study findings may serve as a reference for future research on geohazard chains.

LANDSLIDES (2021)

Article Engineering, Geological

Catastrophic debris flows triggered by the 20 August 2019 rainfall, a decade since the Wenchuan earthquake, China

Fan Yang et al.

Summary: Enhanced debris flow activity has been observed in Sichuan Province, Southwest China after the 2008 Wenchuan earthquake, with intense activity still present more than a decade later. A heavy rainstorm in August 2019 triggered catastrophic debris flows in the epicentral area. Analysis revealed that the 2019 debris flows were mainly initiated by concentrated runoff erosion, differing from previous events.

LANDSLIDES (2021)

Article Geography, Physical

Debris flows triggered from melt of seasonal snow and ice within the active layer in the semi-arid Andes

Ivan Vergara Dal Pont et al.

PERMAFROST AND PERIGLACIAL PROCESSES (2020)

Article Engineering, Environmental

Earthquake loading response of a slope with an inclined weak intercalated layer using centrifuge modeling

Kongming Yan et al.

BULLETIN OF ENGINEERING GEOLOGY AND THE ENVIRONMENT (2019)

Review Geosciences, Multidisciplinary

Debris-flow monitoring and warning: Review and examples

Marcel Hurlimann et al.

EARTH-SCIENCE REVIEWS (2019)

Article Engineering, Geological

Visualization of dominant stress-transfer mechanisms in experimental debris flows of different particle-size distribution

Nicoletta Sanvitale et al.

CANADIAN GEOTECHNICAL JOURNAL (2017)

Article Materials Science, Multidisciplinary

Numerical investigation of reverse segregation in debris flows by DEM

Gordon G. D. Zhou et al.

GRANULAR MATTER (2010)

Review Geochemistry & Geophysics

Instability and surge development in debris flows

Barbara Zanuttigh et al.

REVIEWS OF GEOPHYSICS (2007)

Article Geography, Physical

Recent debris flow occurrences associated with glaciers in the Alps

Marta Chiarle et al.

GLOBAL AND PLANETARY CHANGE (2007)

Article Engineering, Geological

Rainfall induced debris flows in pyroclastic deposits, Campania (southern Italy)*

F Fiorillo et al.

ENGINEERING GEOLOGY (2004)