The zodiacal light is the dominant source of the mid-infrared sky brightness
seen from Earth, and exozodiacal light is the dominant emission from planetary
and debris systems around other stars. We observed the zodiacal light spectrum
with ISOCAM over 5-16 over a wide range of orientations relative to the Sun and
the ecliptic. We present theoretical models for a wide range of particle size
distributions and compositions. The observed temperature is as expected for
large (>10 um radius), low-albedo (< 0.08), rapidly-rotating, grey particles 1
AU from the Sun. In addition to the continuum, we detect a weak excess in the
9-11 um range, with an amplitude of 6% of the continuum. The shape of the
feature can be matched by a mixture of silicates: amorphous forsterite/olivine,
dirty crystalline olivine, and a hydrous silicate (montmorillonite). The
presence of hydrous silicate suggests the parent bodies of those particles were
formed in the inner solar nebula. Large particles dominate the size
distribution, but at least some small particles (radii ~1 um) are required to
produce the silicate emission feature. To compare the properties of zodiacal
dust to dust around other main sequence stars, we reanalyzed the exozodiacal
light spectrum for Beta Pic. The exozodiacal spectra are dominated by cold
dust, with emission peaking in the far-infrared, while the zodiacal spectrum
peaks around 20 um. The shape of the silicate feature from Beta Pic is nearly
identical to that derived from the ISO spectrum of 51 Oph; both exozodiacal
features are very different from that of the zodiacal light. The exozodiacal
features are roughly triangular, peaking at 10.3 um while the zodiacal feature
is more boxy.Comment: accepted to Icaru
