Ww. Duley et Da. Williams, WATER ICE FORMATION ON INTERSTELLAR CARBON DUST - WET HAC (WHAC), Monthly Notices of the Royal Astronomical Society, 272(2), 1995, pp. 442-446
A quantitative threshold for the radiative conversion of hydrogenated
amorphous carbon (HAC) to amorphous carbon (aC) has been identified fr
om laboratory data. This threshold, which can be expressed as a critic
al ultraviolet exposure [E](c) similar or equal to 10 J cm(-2), is rea
ched after exposure of dust to the standard interstellar radiation fie
ld for similar to 10(6) yr when A(V)(0)=2.3 mag. The conversion from H
AC to aC involves a change in surface structure, which may inhibit the
bonding of gaseous molecules when A(V) < A(V)(0). This suggests that
the threshold for ice formation on dust grains may be related to the H
AC-aC conversion. We also conclude that HAC should contain an apprecia
ble quantity of structural H2O, which is distinct from condensed H2O i
ce. Infrared absorption due to this structural H2O should be detectabl
e near 2.9 and 5.9 mu m.