Interplanetary and interstellar dust particles stream through the Jovi
an magnetosphere where their orbits are perturbed by the Lorentz force
. Energy and angular momentum exchange with the magnetosphere can lead
to capture of some submicron dust particles into dynamically stable o
rbits around Jupiter. The captured grains can be on prograde or retrog
rade orbits, and their final orbits are usually in the semimajor axis
range of 2 to 20 Jupiter radii, with eccentricities similar to 0.1-0.8
and inclinations less than or similar to 20 degrees. Captured grains
have radii between about 0.5 and 1.5 mu m. These captured dust particl
es form a diffuse band of material around Jupiter, outside the main Jo
vian ring, with a peak normal optical depth of tau less than or simila
r to 10(-9) While this is too low for optical detection, the Galileo d
ust detector has detected particles on prograde and retrograde orbits
around Jupiter whose sizes, orbital properties, and number density are
consistent with captured interplanetary and interstellar dust.