WEN Haitao, WEI Chaohua, LIAO Liping, et al. Occurrence and Temporal-spatial Distribution Characteristics of Geological Hazards in Rongxian County in Southeast Guangxi Zhuang Autonomous Region[J]. Bulletin of Soiland Water Conservation, 2017, 37(5): 182-188.
DOI:
WEN Haitao, WEI Chaohua, LIAO Liping, et al. Occurrence and Temporal-spatial Distribution Characteristics of Geological Hazards in Rongxian County in Southeast Guangxi Zhuang Autonomous Region[J]. Bulletin of Soiland Water Conservation, 2017, 37(5): 182-188. DOI: 10.13961/j.cnki.stbctb.20170919.001.
Occurrence and Temporal-spatial Distribution Characteristics of Geological Hazards in Rongxian County in Southeast Guangxi Zhuang Autonomous Region
[Objective] The occurrence condition of geological hazards was analyzed in order to provide a scientific reference for the prevention and control of regional geological hazards in Rongxian County
Guangxi Zhuang Autonomous Region.[Methods] The occurrence and temporal-spatial distribution features were analyzed by adopting a statistical method based on the detailed data of field surveys over the past ten years.[Results] There were 4 types of geological hazard:landslide
collapse
unstable slope and debris flow. Their occurrence scales were small
and occurrence rates accounted for 40.57%
26.87%
32.30% and 0.26% of the total hazards respectively. The movement ways were tractive in the landslide
tractive and sliding in the collapse. The unstable slope manifested three types:partial collapse slope
partial erosive slope
and high steep slope. Geological hazards were significantly influenced by local heavy rainfall and typhoon rainfall
and concentrated in the period of June and August
having time lag effect and always happened suddenly in summer rainy season. The geological hazards distributed in the whole region but happened more frequently in some townships. Most of the hazards occurred in low hilly region and granite region
and presented a local linear distribution along the geological structural belt. However
the geological structure had no remarkable impact on these geological hazards.[Conclusion] The occurrence and distribution features are influenced by three aspects