Comparison of mixing properties in convection with the particle-line method

被引:17
作者
Ten, AA
Podladchikov, YY
Yuen, DA
Larsen, TB
Malevsky, AV
机构
[1] Univ Minnesota, Inst Supercomp, Dept Geol & Geophys, Minneapolis, MN 55415 USA
[2] Inst Mineral & Petrog, Novosibirsk 630090, Russia
[3] ETH Zurich, Inst Geol, CH-8092 Zurich, Switzerland
[4] Natl Survey & Cadastre, Geodynam Dept, DK-2400 Copenhagen NV, Denmark
[5] Univ Montreal, Dept Phys, Montreal, PQ H3X 2H9, Canada
[6] Univ Montreal, CERCA, Montreal, PQ H3X 2H9, Canada
关键词
D O I
10.1029/98GL51991
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Spatial resolution in mixing processes is an acute problem. We propose a line method, akin to the contour dynamics technique, which is an extension of the particle method but with the particles redistributed on the line with time. We have used up to 10(5) particles per line and ten lines to investigate the dynamical and structural properties of mixing for both Newtonian and non-Newtonian temperature-dependent viscosity convection in 2D geometry. The spatial structures and the time history of the lines formed in Newtonian convection are different from those produced in non-Newtonian convection, which has the tendency for producing long-living horizontal structures. Efficient mixing in the upper mantle would be inhibited by non-Newtonian rheology.
引用
收藏
页码:3205 / 3208
页数:4
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