Multiphase flow modelling of volcanic ash particle settling in water using adaptive unstructured meshes

被引:23
作者
Jacobs, C. T. [1 ,2 ]
Collins, G. S. [2 ]
Piggott, M. D. [2 ,3 ]
Kramer, S. C. [1 ,2 ]
Wilson, C. R. G. [4 ]
机构
[1] Univ London Imperial Coll Sci Technol & Med, Inst Shock Phys, London SW7 2AZ, England
[2] Univ London Imperial Coll Sci Technol & Med, Dept Earth Sci & Engn, London SW7 2AZ, England
[3] Univ London Imperial Coll Sci Technol & Med, Grantham Inst Climate Change, London SW7 2AZ, England
[4] Columbia Univ, Lamont Doherty Earth Observ, New York, NY 10964 USA
基金
英国自然环境研究理事会;
关键词
Numerical solutions; Non-linear differential equations; Volcaniclastic deposits; NUMERICAL-SIMULATION; SEDIMENTATION; INSTABILITY; COLUMNS;
D O I
10.1093/gji/ggs059
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
Small-scale experiments of volcanic ash particle settling in water have demonstrated that ash particles can either settle slowly and individually, or rapidly and collectively as a gravitationally unstable ash-laden plume. This has important implications for the emplacement of tephra deposits on the seabed. Numerical modelling has the potential to extend the results of laboratory experiments to larger scales and explore the conditions under which plumes may form and persist, but many existing models are computationally restricted by the fixed mesh approaches that they employ. In contrast, this paper presents a new multiphase flow model that uses an adaptive unstructured mesh approach. As a simulation progresses, the mesh is optimized to focus numerical resolution in areas important to the dynamics and decrease it where it is not needed, thereby potentially reducing computational requirements. Model verification is performed using the method of manufactured solutions, which shows the correct solution convergence rates. Model validation and application considers 2-D simulations of plume formation in a water tank which replicate published laboratory experiments. The numerically predicted settling velocities for both individual particles and plumes, as well as instability behaviour, agree well with experimental data and observations. Plume settling is clearly hindered by the presence of a salinity gradient, and its influence must therefore be taken into account when considering particles in bodies of saline water. Furthermore, individual particles settle in the laminar flow regime while plume settling is shown (by plume Reynolds numbers greater than unity) to be in the turbulent flow regime, which has a significant impact on entrainment and settling rates. Mesh adaptivity maintains solution accuracy while providing a substantial reduction in computational requirements when compared to the same simulation performed using a fixed mesh, highlighting the benefits of an adaptive unstructured mesh approach.
引用
收藏
页码:647 / 665
页数:19
相关论文
共 47 条
[1]  
[Anonymous], 2005, MULTIPHASE FLOW HDB
[2]  
[Anonymous], 2000, INCOMPRESSIBLE FLOW
[3]   A high-order accurate discontinuous finite element method for the numerical solution of the compressible Navier-Stokes equations [J].
Bassi, F ;
Rebay, S .
JOURNAL OF COMPUTATIONAL PHYSICS, 1997, 131 (02) :267-279
[4]  
BRADLEY WH, 1969, LIMNOL OCEANOGR, V14, P1
[5]   VERTICAL DENSITY CURRENTS [J].
BRADLEY, WH .
SCIENCE, 1965, 150 (3702) :1423-&
[6]  
Carey S, 1997, GEOLOGY, V25, P839, DOI 10.1130/0091-7613(1997)025<0839:IOCSOT>2.3.CO
[7]  
2
[8]  
Carey S.N., 2011, DEV SEDIMENTOL, V63, P457
[9]   NUMERICAL SOLUTION OF NAVIER-STOKES EQUATIONS [J].
CHORIN, AJ .
MATHEMATICS OF COMPUTATION, 1968, 22 (104) :745-&
[10]   LBB stability of a mixed Galerkin finite element pair for fluid flow simulations [J].
Cotter, Colin J. ;
Ham, David A. ;
Pain, Christopher C. ;
Reich, Sebastian .
JOURNAL OF COMPUTATIONAL PHYSICS, 2009, 228 (02) :336-348