Previous investigations of sputtering of molecular nitrogen from Trito
n's atmosphere lead to estimates of escape rates of about 10(21) N-2 m
olecules s(-1). Here, the erosion of Triton's nitrogen atmosphere resu
lting from sputtering due to different plasma populations and particle
s from Neptune's magnetosphere is investigated. This investigation sho
ws that sputtering from Triton's nitrogen atmosphere could lead to N-2
escape rates during the plasma sheet crossing on the order of 5 x 10(
24) s(-1). This calculation shows that sputtering of Triton's nitrogen
atmosphere by magnetospheric particles is an efficient nonthermal esc
ape mechanism, similar to Saturn's large satellite Titan, and is an ad
ditional important process for the power input of the Neptune aurora.
The N-2 escape rates should be in a good agreement with the measured H
+/N+ ion ratio in Neptune's magnetosphere. The excess energy of the sp
uttered particles leads primarily to escape and supply to the Neptune
system rather than to ballistic orbits. Sputtering will yield, however
, a small N-2 corona on Triton.