Energy Partitioning For Impacts Of Water, Sand, Rhodium And Iron Using Autodyn.

Details Energy Partitioning For Impacts Of Water, Sand, Rhodium And Iron Using Autodyn. Energy Partitioning For Impacts Of Water, Sand, Rhodium And Iron Using Autodyn.

Dec 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006dps....38.1316r&link_type=abstract

American Astronomical Society, DPS meeting #38, #13.16; Bulletin of the American Astronomical Society, Vol. 38, p.1295

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Collisions and following shock compressions of matter are frequent events in the Solar System. Many of natural solids are porous and their behavior under compression differs of non-porous solids. Here we want to investigate energy partitioning for several porous and non-porous materials.
Autodyn is used to consider energy partitioning for water, sand, rhodium and iron during hyper velocity impacts. The impact velocity ranges from 0.6 km/s to 80 km/s and pressure may change from 1 GPa to 3000 GPa.
The calculations also assume that the materials are porous ones with the distention (m=V00/V0) changing from 1.0 to 2.5 and use the P-alpha model for the description of porous materials.
We are also going to perform a low velocity (0.7 km/s) impact experiment at the Seismological laboratory of Caltech and compare the results with the result of the calculations.

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