方群生, 唐川, 王毅, et al. A Calculation Method for Predicting Dynamic Reserve and the Total Amount of Material Source of the Debris Flows in the Wenchuan Meizoseismal Area[J]. 2016, 36(6): 1008-1014.
方群生, 唐川, 王毅, et al. A Calculation Method for Predicting Dynamic Reserve and the Total Amount of Material Source of the Debris Flows in the Wenchuan Meizoseismal Area[J]. 2016, 36(6): 1008-1014. DOI: 10.13409/j.cnki.jdpme.2016.06.023.
A Calculation Method for Predicting Dynamic Reserve and the Total Amount of Material Source of the Debris Flows in the Wenchuan Meizoseismal Area
There is great difference between the types of Debris flow material in earthquake-affected areas and the traditional material in scale
quantity and distribution after the Wenchuan earthquake.The method of traditional statistical material could not meet the needs of engineering design for debris flow currently.Therefore
this paper uses the data from field investigation in examining 48 debris flow gullies to find the volume
the area and the dynamic reserve of the avalanches landslide
the channel material and the slope material.The regression analysis of the avalanches landslide
the channel material and the slope material volume and area with dynamic reserve and the total amount of material source in debris flow basin is made by using the software Matlab.It is found that not only volume and area of the avalanches landslide
the channel material and the slope material and dynamic reserve and the total amount of material source of the channel material have an obvious power function correlation
but also the total amount of material source of the avalanches landslide and the slope material have an obvious quadratic term function and cubic function correlation with dynamic reserve.This model is established
which can predict the dynamic reserve and the total amount of material source of debris flows.
An empirical–statistical model for predicting debris-flow runout zones in the Wenchuan earthquake area [J] . Chuan Tang,Jing Zhu,Ming Chang,Jun Ding,Xin Qi. Quaternary International . 2010
Rainfall-triggered debris flows following the Wenchuan earthquake [J] . C. Tang,J. Zhu,W. L. Li,J. T. Liang. Bulletin of Engineering Geology and the Environment . 2009 (2)
Impacts of September 21, 1999 Chi-Chi earthquake on the characteristics of gully-type debris flows in central Taiwan [J] . Chia-Nan Liu,Hsiao-Fung Huang,Jia-Jyun Dong. Natural Hazards . 2008 (3)
Impacts of the Chi-Chi earthquake on subsequent rainfall-induced landslides in central Taiwan [J] . Ching-Weei Lin,Shou-Heng Liu,Sen-Yuan Lee,Cheng-Chien Liu. Engineering Geology . 2006 (2)
The influence of landsliding on sediment supply and channel change in a steep mountain catchment [J] . Peter Schuerch,Alexander L. Densmore,Brian W. McArdell,Peter Molnar. Geomorphology . 2006 (3)
Landslide inventories and their statistical properties [J] . Bruce D.Malamud,Donald L.Turcotte,FaustoGuzzetti,PaolaReichenbach. Earth Surf. Process. Landforms . 2004 (6)
Wildfire-related debris-flow initiation processes, Storm King Mountain, Colorado [J] . Susan H. Cannon,Robert M. Kirkham,Mario Parise. Geomorphology . 2001 (3)
The role of debris supply conditions in predicting debris flow activity [J] . Michael J.Bovis,MatthiasJakob. Earth Surf. Process. Landforms . 1999 (11)