X-ray emission was discovered in comet Hyakutake (C/1996 B2) by the Ro
ntgen satellite in 1996, and these emissions were attributed to the ex
citation of high charge state solar wind ions due to electron capture
from cometary molecules or atoms. Using the plasma flow in the coma of
Hyakutake calculated by a three-dimensional adaptive magneto-hydrodyn
amic model, the density distribution of solar wind ions in the coma an
d the resulting x-ray emission were computed. The calculated High Reso
lution imager count rate of 4.4 per second and the spatial distributio
n of the x-ray emission agree with the observations. A detailed energy
spectrum of cometary x-rays is predicted in the 80 to 2000 electronvo
lt energy range. Cometary x-rays present a sensitive tool to monitor c
ometary activity and solar wind ion composition.