Impact on porous targets: Penetration, crater formation, target compaction, and ejection

Using a granular-mechanics code, we study the impact of a sphere into a porous adhesive granular target, consisting of monodisperse silica grains. The model includes elastic repulsive, adhesive, and dissipative forces, as well as sliding, rolling, and twisting friction. Impact velocities of up to 30...

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Authors: Ringl, Christian; Bringa, Eduardo Marcial; Urbassek, Herbert M.
Format: Article
Status:Published version
Publication date:2012
Country:Argentina
Institution:Consejo Nacional de Investigaciones Científicas y Técnicas
Repository:CONICET Digital (CONICET)
Language:English
OAI Identifier:oai:ri.conicet.gov.ar:11336/20473
Online Access:http://hdl.handle.net/11336/20473
Access Level:Open access
Keyword:Grains
Craters
https://purl.org/becyt/ford/1.3
https://purl.org/becyt/ford/1
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author Ringl, Christian
author2 Bringa, Eduardo Marcial
Urbassek, Herbert M.
author2_role author
author
author_browse Bringa, Eduardo Marcial
Ringl, Christian
Urbassek, Herbert M.
author_facet Ringl, Christian
Bringa, Eduardo Marcial
Urbassek, Herbert M.
author_role author
collection CONICET Digital (CONICET)
description Using a granular-mechanics code, we study the impact of a sphere into a porous adhesive granular target, consisting of monodisperse silica grains. The model includes elastic repulsive, adhesive, and dissipative forces, as well as sliding, rolling, and twisting friction. Impact velocities of up to 30 m/s and target filling factors (densities) between 19% and 35% have been systematically studied. We find that the projectile is stopped by an effective drag force which is proportional to the square of its velocity. Target adhesion influences projectile stopping only below a critical velocity, which increases with adhesion. The penetration depth depends approximately logarithmically on the impact velocity and is inversely proportional to the target density. The excavated crater is of conical form and is surrounded by a compaction zone whose width increases but whose maximum value decreases with increasing target density. Grain ejection increases in proportion with impactor velocity. Grains are ejected which have originally been buried to a depth of 8Rgrain below the surface; the angular distribution favors oblique ejection with a maximum around 45◦. The velocity distribution of ejected grains features a broad low-velocity maximum around 0.5–1 m/s but exhibits a high-velocity tail up to ∼15% of the projectile impact velocity.
eu_rights_str_mv openAccess
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id AR_bb9a44232bf2a0dd3c8d73dc4e776147
identifier_str_mv Ringl, Christian; Bringa, Eduardo Marcial; Urbassek, Herbert M.; Impact on porous targets: Penetration, crater formation, target compaction, and ejection; American Physical Society; Physical Review E: Statistical, Nonlinear And Soft Matter Physics; 86; 6; 12-2012; 61313-61321
1539-3755
CONICET Digital
CONICET
institution Consejo Nacional de Investigaciones Científicas y Técnicas
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
language eng
network_acronym_str AR
network_name_str Argentina
oai_identifier_str oai:ri.conicet.gov.ar:11336/20473
publishDate 2012
publishDateSort 2012
publisher American Physical Society
publisherStr American Physical Society
reponame_str CONICET Digital (CONICET)
spelling Impact on porous targets: Penetration, crater formation, target compaction, and ejection Ringl, Christian Bringa, Eduardo Marcial Urbassek, Herbert M. Grains Craters https://purl.org/becyt/ford/1.3 https://purl.org/becyt/ford/1 Using a granular-mechanics code, we study the impact of a sphere into a porous adhesive granular target, consisting of monodisperse silica grains. The model includes elastic repulsive, adhesive, and dissipative forces, as well as sliding, rolling, and twisting friction. Impact velocities of up to 30 m/s and target filling factors (densities) between 19% and 35% have been systematically studied. We find that the projectile is stopped by an effective drag force which is proportional to the square of its velocity. Target adhesion influences projectile stopping only below a critical velocity, which increases with adhesion. The penetration depth depends approximately logarithmically on the impact velocity and is inversely proportional to the target density. The excavated crater is of conical form and is surrounded by a compaction zone whose width increases but whose maximum value decreases with increasing target density. Grain ejection increases in proportion with impactor velocity. Grains are ejected which have originally been buried to a depth of 8Rgrain below the surface; the angular distribution favors oblique ejection with a maximum around 45◦. The velocity distribution of ejected grains features a broad low-velocity maximum around 0.5–1 m/s but exhibits a high-velocity tail up to ∼15% of the projectile impact velocity. Fil: Ringl, Christian. Universität Kaiserslautern; Alemania Fil: Bringa, Eduardo Marcial. Universidad Nacional de Cuyo. Facultad de Ciencias Exactas y Naturales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza; Argentina Fil: Urbassek, Herbert M.. Universität Kaiserslautern; Alemania American Physical Society http://hdl.handle.net/11336/20473 Ringl, Christian; Bringa, Eduardo Marcial; Urbassek, Herbert M.; Impact on porous targets: Penetration, crater formation, target compaction, and ejection; American Physical Society; Physical Review E: Statistical, Nonlinear And Soft Matter Physics; 86; 6; 12-2012; 61313-61321 1539-3755 CONICET Digital CONICET
spellingShingle Impact on porous targets: Penetration, crater formation, target compaction, and ejection
Ringl, Christian
Grains
Craters
https://purl.org/becyt/ford/1.3
https://purl.org/becyt/ford/1
status_str publishedVersion
title Impact on porous targets: Penetration, crater formation, target compaction, and ejection
title_full Impact on porous targets: Penetration, crater formation, target compaction, and ejection
title_fullStr Impact on porous targets: Penetration, crater formation, target compaction, and ejection
title_full_unstemmed Impact on porous targets: Penetration, crater formation, target compaction, and ejection
title_short Impact on porous targets: Penetration, crater formation, target compaction, and ejection
title_sort Impact on porous targets: Penetration, crater formation, target compaction, and ejection
topic Grains
Craters
https://purl.org/becyt/ford/1.3
https://purl.org/becyt/ford/1
topic_facet Grains
Craters
https://purl.org/becyt/ford/1.3
https://purl.org/becyt/ford/1
url http://hdl.handle.net/11336/20473