Wang Naiang, Li Xiaoqiang, Ye Hao, Zhao Liqiang, Zhao Xiaoyang, Lu Rongzhu, Wang Yuchen
At 23:59 on December 18, 2023, an earthquake with a magnitude of MS 6.2 occurred in Jishishan County, Gansu Province, and at the same time a mudflow secondary geologic disaster broke out in Qijiagou, Zhongchuan Township, Minhe County, Qinghai Province, which is a typical secondary geological disaster of the same earthquake and transformed into a disaster by the coupling and superposition of multiple disasters such as earthquake, landslide and mudflow, and its impact and effect are much greater than that of a single disaster. Through all kinds of methods such as field survey and measurement, remote sensing image analysis, empirical formula estimation and villagers’ interviews so as to recover and reappear the chain process consisting of “agricultural irrigation-static liquefaction-local plastic deformation-potential slip formation” and “earthquake-dynamic liquefaction-seismic slip through-slump slip-mudflow”. This article discusses the geomorphological characteristics and occurrence process of mudflow in Qijiagou, and conducts a preliminary discussion on its causes. The results showed that: 1) The Qijiagou mudflow, with a total length of about 3.0 km and a disaster-forming area of about 0.478 km2, there are all kinds of types of landforms, so it is a typical mudflow-hazard geomorphologic process with a full range of geomorphologic types. 2) the instantaneous maximum flow rate of the first wave of viscous mudflow in Qijiagou was above 10 m/s, and the mudflow head reaches Caotan Village in Zhongchuan Township almost at the same time as the earthquake, and the subsequent intermittent mudflow velocity was about 7.1, 6.0 and 5.8 m/s, compared with the mudflow head, it’s twice as small and gradually decreased; 3) Irrigation over a long period of time, leakage of water channels and pre-earthquake winter irrigation led to the pre-saturation of loess layer in mudflow formation area, and seismic oscillation load causes the liquefaction of underground saturated loess layer, earthquake triggered a sudden increase of excess pore water, the mudflow high speed, low slope drag reduction movement pressure may be the key mechanism for the formation of high-speed mudflow. 4) Winter irrigation on agricultural land and failure to close the electric switch in time after earthquake were the main hydrodynamic conditions of subsequent intermittent mudflow, as well as the human factors that led to mudflow disasters. The co-seismic mudflow is formed by the coupling of multiple factors so it’s very special for research, we should increase our efforts to protect this rare geological site. It is recommended to be protected as geological disaster relics, we should carry out protection zoning, and strengthen the assessment of geologic disaster risk of water conservancy projects in the Yellow River plateau irrigation area, pay attention to preventing the occurrence of loess landslides.