Page 7 - Shimadzu RF-6000
P. 7

Chemicals




            Potential for Identifying the Source of Minerals

            Calcite is a clear and colorless mineral consisting primarily of lime
            rock. Any impurities in the calcite may cause coloration. This example   Calcite A
            shows 3D fluorescence measurement (Excitation vs Emission) data for
            three types of calcite. Calcite A and B are clear and yellow whereas
            calcite C is clear and pink. 3D fluorescence patterns of calcite A and B
            were the same. In contrast, on the 3D fluorescence patterns of calcite
            C, there was a fluorescence peak at about 370 nm (EX; about 205
            nm) and a strong fluorescence at about 430 nm (EX; about 225 nm).
            This fluorescence might be caused by metal-ions such as the
            manganese ion, which makes calcite pink. Because the fluorescence
            wavelengths caused by metal-ions are very sensitive against the size of
            the crystal field, they may readily show changes with mineral content.






                                                                    Calcite B





















                                                                    Calcite C





















                                                                                                     RF-6000
                                                                                                     Spectrofluorophotometer  7
   2   3   4   5   6   7   8   9   10   11   12