The infrared transmission spectra and photochemical behavior of variou
s organic compounds isolated in solid N2 ices, appropriate for applica
tions to Triton and Pluto, are presented. It is shown that excess abso
rption in the surface spectra of Triton and Pluto, i.e., absorption no
t explained by present models incorporating molecules already identifi
ed on these bodies (N2, CH4, CO, and CO2), that starts near 4450 cm-1
(2.25 mum) and extends to lower frequencies, may be due to alkanes (C(
n)H2n+2) and related molecules frozen in the nitrogen. Branched and li
near alkanes may be responsible. Experiments in which the photochemist
ry of N2:CH4 and N2:CH4:CO ices was explored demonstrate that the surf
ace ices of Triton and Pluto may contain a wide variety of additional
species containing H, C, O, and N. Of these, the reactive molecule dia
zomethane, CH2N2, is particularly important since it may be largely re
sponsible for the synthesis of larger alkanes from CH4 and other small
alkanes. Diazomethane would also be expected to drive chemical reacti
ons involving organics in the surface ices of Triton and Pluto toward
saturation, i.e., to reduce multiple CC bonds. The positions and intri
nsic strengths (A values) of many of the infrared absorption bands of
N2 matrix-isolated molecules of relevance to Triton and Pluto have als
o been determined. These can be used to aid in their search and to pla
ce constraints on their abundances. For example, using these A values
the abundance ratios CH4/N2 almost-equal-to 1.3 x 10(-3), C2H4/N2 less
-than-or-equal-to 9.5 x 10(-7), and H2CO/N2 less-than-or-equal-to 7.8
x 10(-7) are deduced for Triton and CH4/N2 almost-equal-to 3.1 x 10(-3
), C2H4/N2 less-than-or-equal-to 4.1 x 10(-6), and H2CO/N2 less-than-o
r-equal-to 5.2 x 10(-6) deduced for Pluto. The small amounts of C2H4 a
nd H2CO in the surface ices of these bodies are in disagreement with t
he large abundances expected from many theoretical models.