Pore surface energy corrected P-α like models and the anomalous behaviour of porous materials

被引:0
作者
Arena, S. E. [1 ]
Speith, R. [1 ]
机构
[1] Univ Tubingen, Inst Astron & Astrophys, D-72076 Tubingen, Germany
来源
PLASMAS IN THE LABORATORY AND IN THE UNIVERSE: INTERACTIONS, PATTERNS, AND TURBULENCE | 2010年 / 1242卷
关键词
Planetesimal formation; Porosity models; SIMULATIONS; COMPACTION; POROSITY; IMPACTS; PHYSICS; BODIES;
D O I
10.1063/1.3460137
中图分类号
O59 [应用物理学];
学科分类号
摘要
Accurate models for the description of porous materials are necessary in simulations of collisions between pre-planetesimals which are required to study the viability of collisional growth as a mechanism leading to the formation of planetesimals. We have compared two porosity models that have been used in the related field of impact cratering, and we have found that they suffer two problems when applied to high porosity materials that are likely to show the so called anomalous behaviour. To overcome the observed problems we have proposed a correction of the internal energy of the porous material considering the contribution of the surface energy of the pores.
引用
收藏
页码:294 / 299
页数:6
相关论文
共 16 条
[1]  
ARENA SE, 2009, ICARUS UNPUB
[2]   Experiments on sticking, restructuring, and fragmentation of preplanetary dust aggregates [J].
Blum, J ;
Wurm, G .
ICARUS, 2000, 143 (01) :138-146
[3]   RANKINE-HUGONIOT RELATION FOR SHOCK-WAVES IN VERY POROUS-MEDIA [J].
BOLKHOVITINOV, LG ;
KHVOSTOV, YB .
NATURE, 1978, 274 (5674) :882-883
[4]   Comparative study of analytical methods for Hugoniot curves of porous materials [J].
Boshoff-Mostert, L ;
Viljoen, HJ .
JOURNAL OF APPLIED PHYSICS, 1999, 86 (03) :1245-1254
[5]   The physics of dust coagulation and the structure of dust aggregates in space [J].
Dominik, C ;
Tielens, AGGM .
ASTROPHYSICAL JOURNAL, 1997, 480 (02) :647-673
[6]   CONSTITUTIVE EQUATION FOR DYNAMIC COMPACTION OF DUCTILE POROUS MATERIALS [J].
HERRMANN, W .
JOURNAL OF APPLIED PHYSICS, 1969, 40 (06) :2490-&
[7]   Numerical simulations of impacts involving porous bodies I. Implementing sub-resolution porosity in a 3D SPH hydrocode [J].
Jutzi, Martin ;
Benz, Willy ;
Michel, Patrick .
ICARUS, 2008, 198 (01) :242-255
[8]   Growth and form of planetary seedlings: Results from a sounding rocket microgravity aggregation experiment [J].
Krause, M ;
Blum, J .
PHYSICAL REVIEW LETTERS, 2004, 93 (02) :021103-1
[9]   Spitzer spectral observations of the Deep Impact ejecta [J].
Lisse, C. M. ;
VanCleve, J. ;
Adams, A. C. ;
A'Hearn, M. F. ;
Fernandez, Y. R. ;
Farnham, T. L. ;
Armus, L. ;
Grillmair, C. J. ;
Ingalls, J. ;
Belton, M. J. S. ;
Groussin, O. ;
McFadden, L. A. ;
Meech, K. J. ;
Schultz, P. H. ;
Clark, B. C. ;
Feaga, L. M. ;
Sunshine, J. M. .
SCIENCE, 2006, 313 (5787) :635-640
[10]   A ballistics analysis of the Deep Impact ejecta plume: Determining Comet Tempel 1's gravity, mass, and density [J].
Richardson, James E. ;
Melosh, H. Jay ;
Lisse, Carey M. ;
Carcich, Brian .
ICARUS, 2007, 190 (02) :357-390