Contrary to a widespread assumption, deuterium is not simply destroyed in s
tars: deuterium is also synthesized in the atmospheres of active stars. Thi
s nonprimordial synthesis of D arises when protons accelerated in flares in
teract with the atmosphere, create a flux of free neutrons, and these neutr
ons then undergo radiative capture on atmospheric protons. Radiative captur
e does not result in excess production of Li, Be, or B. Ejection of flare-p
rocessed material contaminates the interstellar medium (ISM), as was origin
ally suggested by Coleman & Worden. Estimates of the amount of flare-create
d D are subject to considerable uncertainties, but we find, using stellar p
arameters within permitted ranges, that flares may contribute significantly
to the current ISM D content. Observational data indicate that different c
louds of gas in the ISM exhibit variations in the value of D/H. We suggest
that contamination of the ISM by D-enriched material ejected from stellar f
lares contributes to the observed D/H inhomogeneity. More precise estimates
of the efficiency of D ejection from flares into the solar wind are requir
ed to evaluate this suggestion.