Particle Project Correction for Rock Avalanche: Particle Crushing in Aerzhai Rock Avalanche, China

被引:0
作者
Yang, Qingwen [1 ]
Cui, Shenghua [1 ,2 ]
Yang, Zheng [3 ]
Qian, Bo [3 ]
He, Shuang [1 ]
Wu, Hao [1 ]
机构
[1] Chengdu Univ Technol, State Key Lab Geohazard Prevent & Geoenvironm Pro, Chengdu 610059, Peoples R China
[2] Kyoto Univ, Disaster Prevent Res Inst, Uji, Kyoto 6110011, Japan
[3] Xichang Univ, Sch Civil & Hydraul Engn, Xichang 615000, Sichuan, Peoples R China
基金
美国国家科学基金会; 国家重点研发计划;
关键词
GRAIN-SIZE DISTRIBUTION; DEBRIS AVALANCHE; LANDSLIDE; MECHANISM; FLOW; STURZSTROMS; EARTHQUAKE; DYNAMICS; DEPOSITS; SICHUAN;
D O I
10.2113/2022/2974409
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Strong fluidized rock avalanches with various particle sizes are one of the typical disasters in the mountainous area of southwestern China. Statistical analysis on rock avalanche particles can help understand the traveling behavior, distance, and deposition of rock avalanche, which are useful for potential threat range prediction and disaster prevention. Rock avalanche deposit has more than one oblique slopes different in attitude. Image distortion will happen when particles on the slopes are projected to one plane. Area projection conversion coefficient Ki is applied in this paper to correct the distortion and improve the precision of the geometric dimension parameters of the rock avalanche particle. A rock avalanche (Aerzhai rock avalanche) with a volume of about 10 x 10(4) m(3) took place in Longxi Township, Wenchuan County, China, on April 8, 2018. Being corrected by the coefficient Ki, the mean area and the standard deviation of the particles within different zones have been obtained, and we analyzed their changes in vertical and transverse directions. Here, we show that the mean particle area decreases by about 61.1% from the source to deposition region and area standard deviation decreases by about 37.4%. The deposition region shows a higher proportion of small crashed particles than the source region. The proportion of small particles gets larger with the longitudinal motion distance and lateral distance. For big particles' significant potential energy driving ability and inertia advantages, the longitudinal motion routes can be maintained, and inertia decreases as the particles get smaller, while small particles offset from the center area laterally. These statistical characters are easy to be ignored if projection correction is not performed.
引用
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页数:15
相关论文
共 53 条
[1]  
[Anonymous], 2008, THESIS U CANTERBURY
[2]  
Bergstrom CH, 1963, P 5 S ROCK MECH, P155
[3]   The 17 February 2006 Guinsaugon rock slide-debris avalanche, Southern Leyte, Philippines: deposit characteristics and failure mechanism [J].
Catane, Sandra G. ;
Cabria, Hillel B. ;
Zarco, Mark Albert H. ;
Saturay, Ricarido M., Jr. ;
Mirasol-Robert, Aileen A. .
BULLETIN OF ENGINEERING GEOLOGY AND THE ENVIRONMENT, 2008, 67 (03) :305-320
[4]  
CRANDELL DR, 1984, GEOLOGY, V12, P143, DOI 10.1130/0091-7613(1984)12<143:CDAFAM>2.0.CO
[5]  
2
[6]   Fragmentation in the Val Pola rock avalanche, Italian Alps [J].
Crosta, Giovanni B. ;
Frattini, Paolo ;
Fusi, Nicoletta .
JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE, 2007, 112 (F1)
[7]  
Cui X., 2021, ENG GEOL, V295
[8]   Dynamic simulation of the motion of fragmenting rock avalanches [J].
Davies, TR ;
McSaveney, MJ .
CANADIAN GEOTECHNICAL JOURNAL, 2002, 39 (04) :789-798
[9]  
Dent J. D., 1983, Annals of Glaciology, V4, P42
[10]  
Dong Z., 2014, ADV MAT RES, V989-994, P2254