Dust Production from the Hypervelocity Impact Disruption of Hydrated Targets

Details Dust Production from the Hypervelocity Impact Disruption of Hydrated Targets Dust Production from the Hypervelocity Impact Disruption of Hydrated Targets

Dec 2005

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2005em%26p...97..213f&link_type=abstract

Earth, Moon, and Planets, Volume 97, Issue 3-4, pp. 213-231

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4

Asteroids, Cratering, Disruption, Hydrated Targets, Interplanetary Dust, Meteorites, Micrometeorites

Scientific paper

More than half of the C-type asteroids, which are the dominant type of asteroid in the outer half of the main belt, show evidence of hydration in their reflectance spectra. In order to understand the collisional evolution of asteroids, the production of interplanetary dust, and to model the infrared signature of small particles in the Solar System it is important to characterize the dust production from primary impact disruption events, and compare the disruption of hydrous and anhydrous targets. We performed impact disruption experiments of three “greenstone” targets, a hydrothermally metamorphosed basalt, and compared the results of these disruptions to our previous disruption experiments on porous, anhydrous basalt targets and to literature data on the disruption of non-porous, anhydrous basalt targets. The greenstone targets were selected because their major hydrous alteration phase is serpentine, the same hydrous alteration phase found in hydrous CM meteorites, like Murchison. The porous, anhydrous basalt targets were selected because their structure, consisting of millimeter-size olivine phenocrysts in a more porous, anhydrous matrix is similar to the structure of anhydrous chondritic meteorites, which consist of millimeter-size olivine chondrules embedded in a more porous, anhydrous matrix. The disruption measurements indicate the threshold collisional specific energy, Q D * , is 570 J/kg for the greenstone, which is lower than the literature values for non-porous basalt targets, and significantly lower than the value of 2500 J/kg that we have measured for porous anhydrous basalt targets. We determined the mass-frequency distribution of the debris from the disruption of the greenstone targets, which ranged in mass from 80 to 280 g, over a nine order-of-magnitude mass range, from ~10-9 g to the mass of the largest fragment. The cumulative mass-frequency distribution from the greenstone targets is fit by two power law segments, one for masses >10-2 g, which is significantly steeper than the corresponding segment from the disruption of similar-sized anhydrous basalt, and one in the range from 10-9 to 10-2 g, which is significantly flatter than the corresponding segment from the disruption of similar size anhydrous basalt. These hydrous greenstone targets overproduce small fragments (10-4 to 100 g) compared to anhydrous basalt targets, but underproduce dust-size grains (10-9 to 10-4 g) compared to anhydrous basalt targets.

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