BIROn - Birkbeck Institutional Research Online

    Laboratory impacts into dry and wet sandstone with and without an overlying water layer: implications for scaling laws and projectile survivability

    Baldwin, E.C. and Milner, D.J. and Burchell, M.J. and Crawford, Ian (2007) Laboratory impacts into dry and wet sandstone with and without an overlying water layer: implications for scaling laws and projectile survivability. Meteoritics & Planetary Science 42 (11), pp. 1905-1914. ISSN 1086-9379.

    Full text not available from this repository.

    Abstract

    Scaling laws describing crater dimensions are defined in terms of projectile velocity and mass, densities of the materials involved, strength of the target, and the local gravity. Here, the additional importance of target porosity and saturation, and an overlying water layer, are considered through 15 laboratory impacts of 1 mm diameter stainless steel projectiles at 5 km s−1 into a) an initially uncharacterized sandstone (porosity ˜17%) and b) Coconino Sandstone (porosity ˜23%). The higher‐porosity dry sandstone allows a crater to form with a larger diameter but smaller depth than in the lower‐porosity dry sandstone. Furthermore, for both porosities, a greater volume of material is excavated from a wet target than a dry target (by 27–30%). Comparison of our results with Pi‐scaling (dimensionless ratios of key parameters characterizing cratering data over a range of scales) suggests that porosity is important for scaling laws given that the new data lie significantly beneath the current fit for ice and rock targets on a πv versus π3 plot (πv gives cratering efficiency and π3 the influence of target strength). An overlying water layer results in a reduction of crater dimensions, with larger craters produced in the saturated targets compared to unsaturated targets. A water depth of approximately 12 times the projectile diameter is required before craters are no longer observed in the targets. Previous experimental studies have shown that this ratio varies between 10 and 20 (Gault and Sonett 1982). In our experiments ˜25% of the original projectile mass survives the impact.

    Metadata

    Item Type: Article
    School: Birkbeck Faculties and Schools > Faculty of Science > School of Natural Sciences
    Depositing User: Sarah Hall
    Date Deposited: 06 Aug 2019 15:14
    Last Modified: 02 Aug 2023 17:53
    URI: https://eprints.bbk.ac.uk/id/eprint/28470

    Statistics

    Activity Overview
    6 month trend
    0Downloads
    6 month trend
    265Hits

    Additional statistics are available via IRStats2.

    Archive Staff Only (login required)

    Edit/View Item Edit/View Item