Abstract
Deep into the night of 9 June 2021, a high-intensity and short-duration rainstorm, the largest rainfall ever recorded in Zhuji, struck the entire city. The abrupt rainfall triggered several debris flows, which killed four residents and closed a highly ranked national scenic area for over three months. The debris flows, triggered by record-breaking rainfall, occurred in a rhyolite porphyry area that was not recognised as an area prone to frequent debris flow. Thus, detailed field investigations were conducted on three debris flow gullies. It was demonstrated that an extreme rainfall event, complex topographic profiles and abundant diluvium in the gullies were the main contributing factors in the disastrous damage. In particular, steep eluvial slopes with a high gradient of over 30° failed under heavy rainfall, which was one of the major factors in the initiation of debris flows. In addition, geometric properties, such as the curved travelling path, natural cliff and cross-sectional shape of the gullies, interacted significantly with the deep and lateral erosions of diluvium in the gullies, which promoted mass enlargement and the long-runout movement of the debris flows. Furthermore, reasonable countermeasures made some contribution to the reduction and mitigation of this kind of geo-disasters.
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Acknowledgements
The Hydrological Centre of Zhuji Water Resource Bureau provided the meteorological data. Mr. Ye Chen of Tongji University participated in the field investigations.
Funding
This study was supported by the National Natural Science Foundation of China (Grant No. 42107170), the China Postdoctoral Science Foundation (Grant No. BX2021214 and 2021M702493), the Shanghai Post-doctoral Excellence Program (Grant No. 2020423) and the Fundamental Research Funds of China for the Central Universities.
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Wang, F., Yan, K., Nam, K. et al. The Wuxie debris flows triggered by a record-breaking rainstorm on 10 June 2021 in Zhuji City, Zhejiang Province, China. Landslides 19, 1913–1934 (2022). https://doi.org/10.1007/s10346-022-01903-w
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DOI: https://doi.org/10.1007/s10346-022-01903-w