The compression property of regolith reflects the strength and porosity of
the regolith layer on small bodies and their variations in the layer that
largely influence the collisional and thermal evolution of the bodies. We
conducted compression experiments and investigated the relationship between the
porosity and the compression using fluffy granular samples. We focused on a
low-pressure and high-porosity regime. We used tens of {\mu}m-sized irregular
and spherical powders as analogs of porous regolith. The initial porosity of
the samples ranged from 0.80 to 0.53. The uniaxial pressure applied to the
samples lays in the range from 30 to 4x10^5 Pa. The porosity of the samples
remained at their initial values below a threshold pressure and then decreased
when the pressure exceeded the threshold. We defined this uniaxial pressure at
the threshold as "yield strength". The yield strength increased as the initial
porosity of a sample decreased. The yield strengths of samples consisting of
irregular particles did not significantly depend on their size distributions
when the samples had the same initial porosity. We compared the results of our
experiments with a previously proposed theoretical model. We calculated the
average interparticle force acting on contact points of constituent particles
under the uniaxial pressure of yield strength using the theoretical model and
compared it with theoretically estimated forces required to roll or slide the
particles. The calculated interparticle force was larger than the rolling
friction force and smaller than the sliding friction force. The yield strength
of regolith may be constrained by these forces. Our results may be useful for
planetary scientists to estimate the depth above which the porosity of a
regolith layer is almost equal to that of the regolith surface and to interpret
the compression property of an asteroid surface obtained by a lander.Comment: Pages: 16, Tables: 3, Figures:
Inelastic collisions occur among regolith particles, such as those in the ejecta curtain from a crater, and may cause clustering or agglomeration of particles and thus produce discrete patterns of ejecta deposits around a crater. Previous studies have shown that clusters, and even agglomerates, are formed via mutual, inelastic collisions of spherical particles due to adhering forces between particles in granular streams. To investigate the condition of agglomerate formation in granular streams, we conducted laboratory experiments of granular streams using both spherical and irregular, non-spherical particles. Measurements of particle adhesion in this study were performed using a centrifugal separation method, in contrast to the previous study in which atomic force microscopy (AFM) was used. This enabled simultaneous measurements 1 of multiple particles of various shapes for a statistical analysis of the results. With similar relative velocities and adhesion values, irregular particles were found to form agglomerates much more easily than spherical particles. The axial ratio of the agglomerates of spherical particles and irregular particles was similar and was in accordance with those observed in previous laboratory studies, whereas the size of the agglomerates of irregular particles was larger than the size of spherical particles. The degree of agglomeration and the size of agglomerates can be used as an indicator of the shape or adhesive force of the particles in granular stream. Our findings on agglomeration in granular streams could provide new insights into the origin of rays on airless bodies and grooves on Phobos.
scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.