Haojie Wang
Current Organizations / Institutes
The organizations/institutes from the scholar's latest article
Research Subjects
Haojie Wang has a total of 17 co-authors. Here are the top co-authors by number of shared publications:
- Ping Sun
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing, China
6 shared publications - Jian Ren
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing, China
2 shared publications - Jian Ren
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing, China
2 shared publications - Shuai Zhang
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing, China
2 shared publications - Tao Wang
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing, China
2 shared publications - Chaoying Ke
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing, China
1 shared publication
Latest Publications
- 27 May 2026
- Published by Springer Nature in Landslides
- Vol. 23 (10) , 1-21
Dynamic-process-based quantitative hazard assessment for earthquake-induced landslide clusters in the Northern Mountain of Tianshui
- 27 May 2026
- Published by Springer Nature in Landslides
- Vol. 23 (10) , 1-21
Dynamic-process-based quantitative hazard assessment for earthquake-induced landslide clusters in the Northern Mountain of Tianshui
- 8 March 2023
- Published by Springer Nature in Landslides
- Vol. 20 (5) , 999-1011
Reactivation mechanism and run-out processes of the Wangqi landslide induced by water leakage on April 30, 2022, in Tianshui City, Gansu Province, China
- 8 March 2023
- Published by Springer Nature in Landslides
- Vol. 20 (5) , 999-1011
Reactivation mechanism and run-out processes of the Wangqi landslide induced by water leakage on April 30, 2022, in Tianshui City, Gansu Province, China
- 9 September 2022
- Published by Springer Nature in Landslides
- Vol. 19 (12) , 2983-2996
Evolutionary and dynamic processes of the Zhongzhai landslide reactivated on October 5, 2021, in Niangniangba, Gansu Province, China
- 9 September 2022
- Published by Springer Nature in Landslides
- Vol. 19 (12) , 2983-2996
Evolutionary and dynamic processes of the Zhongzhai landslide reactivated on October 5, 2021, in Niangniangba, Gansu Province, China
- Open Access
Hazard Zonation and Risk Assessment of a Debris Flow under Different Rainfall Condition in Wudu District, Gansu Province, Northwest China
Debris flows induced by heavy rainfall are a major threat in Northwest and Southwest China, due to its abrupt occurrence and long runout. In light of this, this work presents the runout simulation and risk assessment of the Boshuigou debris flow under different rainfall conditions in Wudu district, Gansu Province, Northwest China. Based on field reconnaissance, the geomorphological feature and main source of the Boshuigou debris flow were described. With the application of the FLO-2D simulation, the potential flow depth and flow extent of the Boshuigou debris flow under 100-year return-period rainfall and 50-year return-period rainfall were calculated. The maximum flow velocities of the Boshuigou debris flow under the 100-year return-period rainfall and 50-year return-period rainfall were 5.46 and 5.18 m/s, respectively. Accordingly, the maximum flow depths were 5.85 and 5.57 m. Then, the hazard zonation was conducted in combination of the construction and other properties within the potential impact zone, and the risk assessment of the Boshuigou debris flow under the 100-year return-period rainfall and 50-year return-period rainfall was finally completed. This work presents a method for debris flow risk assessment considering the solid source and water flow, which can provide a basic reference for mitigation and reduction of geohazards induced by torrential rainfall.
Open AccessHazard Zonation and Risk Assessment of a Debris Flow under Different Rainfall Condition in Wudu District, Gansu Province, Northwest China
Debris flows induced by heavy rainfall are a major threat in Northwest and Southwest China, due to its abrupt occurrence and long runout. In light of this, this work presents the runout simulation and risk assessment of the Boshuigou debris flow under different rainfall conditions in Wudu district, Gansu Province, Northwest China. Based on field reconnaissance, the geomorphological feature and main source of the Boshuigou debris flow were described. With the application of the FLO-2D simulation, the potential flow depth and flow extent of the Boshuigou debris flow under 100-year return-period rainfall and 50-year return-period rainfall were calculated. The maximum flow velocities of the Boshuigou debris flow under the 100-year return-period rainfall and 50-year return-period rainfall were 5.46 and 5.18 m/s, respectively. Accordingly, the maximum flow depths were 5.85 and 5.57 m. Then, the hazard zonation was conducted in combination of the construction and other properties within the potential impact zone, and the risk assessment of the Boshuigou debris flow under the 100-year return-period rainfall and 50-year return-period rainfall was finally completed. This work presents a method for debris flow risk assessment considering the solid source and water flow, which can provide a basic reference for mitigation and reduction of geohazards induced by torrential rainfall.