We have studied the high-field magnetization up to 14.5 T and magnetic susc
eptibility in the temperature range 1.6-400 K of three different samples of
natural kunzite crystals, being a variety of spodumene (LiAlSi2O6) and con
taining transition metal ions. It appears that the total magnetization and
susceptibility consist of the paramagnetic contribution following from the
temperature-dependent Brillouin- type behavior of magnetic ions and tempera
ture-independent diamagnetic contribution of the spodumene matrix which we
have found as being equal to -3.5 x 10(-7) emu/g. We have identified the Mn
2+ ions as the dominant ones in the kunzites studied and we have determined
the molar concentration of these ions as lying in the range 0.2-0.4%. (C)
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