کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
1781626 | 1022293 | 2011 | 5 صفحه PDF | دانلود رایگان |
Experiments to entrain dust with electrostatic and fluid-dynamic forces result in particulate clouds of aggregates rather than individual dust grains. This is explained within the framework of Griffith-flaw theory regarding the comminution/breakage of weak solids. Physical and electrical inhomogeneities in powders are equivalent to microcracks in solids insofar as they facilitate failure at stress risers. Electrical charging of powders induces bulk sample stresses similar to mechanical stresses experienced by strong solids, depending on the nature of the charging. A powder mass therefore “breaks” into clumps rather than separating into individual dust particles. This contrasts with the expectation that electrical forces on the Moon will eject a submicron population of dust from the regolith into the exosphere. A lunar regolith will contain physical and electrostatic inhomogeneities similar to those in most charged powders.
Research Highlights
► Natural dust tends to break into clods rather than individual grains.
► Breakage model has parallels with Griffith-fracture theory for strong solids.
► Electrical stress in lunar regolith may be similar to mechanical stress in solids.
Journal: Planetary and Space Science - Volume 59, Issue 14, November 2011, Pages 1744–1748