Hybrid modeling of multiphysical processes for particle-based volcano animation

被引:5
作者
Zhang, Shenfan [1 ]
Kong, Fanlong [1 ]
Li, Chen [1 ]
Wang, Changbo [1 ]
Qin, Hong [2 ]
机构
[1] East China Normal Univ, Sch Comp Sci & Software Engn, Shanghai, Peoples R China
[2] SUNY Stony Brook, Stony Brook, NY 11794 USA
关键词
heat transfer; multiphysical interaction and coupling; multiphysical processes; volcano animation; LAVA; SIMULATION;
D O I
10.1002/cav.1758
中图分类号
TP31 [计算机软件];
学科分类号
081202 ; 0835 ;
摘要
Many complex natural phenomena with dramatic spatial and temporal variation are difficult to animate accurately with anticipated performance in many graphics tasks and applications, because oftentimes in prior art, a single type of physical process could not afford high fidelity and effective scene production. Volcano eruption and its subsequent interaction with earth is one such complicated phenomenon that must depend on multiphysical processes and their tight coupling. This paper documents a novel and effective particle-based solution for volcano animation that embraces multiphysical processes and their tight unification. First, we introduce a governing physical model consisting of multiphysical processes enabling flexible state transition among solid, fluid, and gas. This computational physics model is dictated by temperature and accommodates dynamic viscosity that is changing according to the temperature. Second, we propose an augmented smoothed particle hydrodynamics as the underlying numerical model to simulate the behavior of lava and smoke with several required physical attributes. Third, multiphysical quantities are tightly coupled to support the interaction with surroundings including fluid-solid coupling, ground friction, and lava-smoke coupling. We also develop a temperature-directed rendering technique with nearly no extra computational cost and demonstrate realistic graphics effects of volcano eruption and its interaction with earth with visual appeal.
引用
收藏
页数:9
相关论文
共 29 条
[1]   Versatile Rigid-Fluid Coupling for Incompressible SPH [J].
Akinci, Nadir ;
Ihmsen, Markus ;
Akinci, Gizem ;
Solenthaler, Barbara ;
Teschner, Matthias .
ACM TRANSACTIONS ON GRAPHICS, 2012, 31 (04)
[2]  
Bilotta G., 2010, EGU GEN ASSEMBLY, V12, P12233
[3]   The simulation model SCIARA: the 1991 and 2001 lava flows at Mount Etna [J].
Crisci, GM ;
Rongo, R ;
Di Gregorio, S ;
Spataro, W .
JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH, 2004, 132 (2-3) :253-267
[4]   Modelling lava flows by Cellular Nonlinear Networks (CNN): Preliminary results [J].
Del Negro, C ;
Fortuna, L ;
Vicari, A .
NONLINEAR PROCESSES IN GEOPHYSICS, 2005, 12 (04) :505-513
[5]   THE EFFECT OF CRYSTALLIZATION ON THE RHEOLOGY AND DYNAMICS OF LAVA FLOWS [J].
DRAGONI, M ;
TALLARICO, A .
JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH, 1994, 59 (03) :241-252
[6]  
Favalli M, 2005, GEOPHYS RES LETT, V32, P259
[7]  
Fedkiw R, 2001, COMP GRAPH, P15, DOI 10.1145/383259.383260
[8]  
Harada T., 2007, P COMP GRAPH INT RIO, V4, P671
[9]   FLOWGO: a kinematic thermo-rheological model for lava flowing in a channel [J].
Harris, AJL ;
Rowland, SK .
BULLETIN OF VOLCANOLOGY, 2001, 63 (01) :20-44
[10]  
Herault A., 2010, EGU GEN ASSEMBLY, V15, P183