The physical properties and beneficiation potential of wolframite (Fex
Mn1-x)WO4 have been shown to depend heavily upon x or the Fe/Mn ratio.
A series of wolframites with x varying between zero and one have been
synthesized and lattice parameters determined. Alkali-leaching of fer
berite (FeWO4) has been found to be topotactic, with selective removal
of tungsten and production of a high Fe/W ratio on the surface. The r
eplacement of iron with manganese in the wolframite structure seems to
result in a less compact lattice and faster and less selective dissol
ution.