Hypervelocity impacts on dry and wet sandstone: Observations of ejecta dynamics and crater growth

被引:49
作者
Hoerth, Tobias [1 ]
Schaefer, Frank [1 ]
Thoma, Klaus [1 ]
Kenkmann, Thomas [2 ]
Poelchau, Michael H. [2 ]
Lexow, Bernd [1 ]
Deutsch, Alexander [3 ]
机构
[1] EMI, Fraunhofer Inst Kurzzeitdynam, D-79104 Freiburg, Germany
[2] Univ Freiburg, Inst Geowissensch Geol, D-79104 Freiburg, Germany
[3] Univ Munster, Inst Planetol, D-48149 Munster, Germany
关键词
DEEP IMPACT; VELOCITY DISTRIBUTIONS; OBLIQUE IMPACTS; SCALING LAWS; TARGETS; WATER; SPALLATION; EVOLUTION; SAND; FLOW;
D O I
10.1111/maps.12044
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
This study deals with the investigation of highly dynamic processes associated with hypervelocity impacts on porous sandstone. For the impact experiments, two light-gas accelerators with different calibers were used, capable of accelerating steel projectiles with diameters ranging from 2.5 to 12 mm to several kilometers per second. The projectiles impacted on dry and water-saturated Seeberger Sandstone targets. The study includes investigations of the influence of pore water on the shape of the ejecta cloud as well as transient crater growth. The results show a significant influence of pore water on ejecta behavior. Steeper ejecta cone angles are observed if the impacts are conducted on wet sandstones. The transient crater grows at a faster rate and reaches a larger diameter if the target is water saturated. In our experiments, target porosity leads to smaller crater sizes compared with nonporous targets. Water within the pore space reduces porosity and counteracts this process. Power law fits were applied to the crater growth curves. The results show an increase in the scaling exponent mu with increasing pore space saturation.
引用
收藏
页码:23 / 32
页数:10
相关论文
共 44 条
[1]   Asymmetry of ejecta flow during oblique impacts using three-dimensional particle image velocimetry [J].
Anderson, JLB ;
Schultz, PH ;
Heineck, JT .
JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS, 2003, 108 (E8)
[2]   Experimental ejection angles for oblique impacts: Implications for the subsurface flow-field [J].
Anderson, JLB ;
Schultz, PH ;
Heineck, JT .
METEORITICS & PLANETARY SCIENCE, 2004, 39 (02) :303-320
[3]  
[Anonymous], ESA SPECIAL PUBLICAT
[4]  
[Anonymous], 1987, Int. J. Impact Eng, DOI DOI 10.1016/0734-743X(87)90069-8
[5]   Laboratory impacts into dry and wet sandstone with and without an overlying water layer: Implications for scaling laws and projectile survivability [J].
Baldwin, E. C. ;
Milner, D. J. ;
Burchell, M. J. ;
Crawford, I. A. .
METEORITICS & PLANETARY SCIENCE, 2007, 42 (11) :1905-1914
[6]  
Barnouin-Jha O. S., 1996, J GEOPHYS RES, V101, P99
[7]   Non-intrusive measurements of crater growth [J].
Barnouin-Jha, Olivier S. ;
Yamamoto, Satoru ;
Toriumi, Takashi ;
Sugita, Seiji ;
Matsui, Takafumi .
ICARUS, 2007, 188 (02) :506-521
[8]   Oblique incidence hypervelocity impacts on rock [J].
Burchell, MJ ;
Whitehorn, L .
MONTHLY NOTICES OF THE ROYAL ASTRONOMICAL SOCIETY, 2003, 341 (01) :192-198
[9]   INFLUENCE OF WATER IN ROCKS ON EFFECTS OF UNDERGROUND NUCLEAR EXPLOSIONS [J].
BUTKOVICH, TR .
JOURNAL OF GEOPHYSICAL RESEARCH, 1971, 76 (08) :1993-+
[10]   Ejection-velocity distributions from impacts into coarse-grained sand [J].
Cintala, MJ ;
Berthoud, L ;
Hörz, F .
METEORITICS & PLANETARY SCIENCE, 1999, 34 (04) :605-623