We show analytically that large abundances of NH2D and NHD2 can be produced
by gas-phase chemistry in the interiors of cold dense clouds. The calculat
ed fractionation ratios are in good agreement with the values that have bee
n previously determined in L134N and suggest that triply deuterated ammonia
could be detectable in dark clouds. Grain-surface reactions may lead to si
milar NH2D and NHD2 enhancements but, we argue, are unlikely to contribute
to the deuteration observed in L134N.