|
Glittering
Stones >> Colors Of Gemstones
Colors of gemstones
The most common cause of color in the gemstones
is its presence of a very small amount of a transition
metal ion. These transition metal ions
normally have an incomplete set of 3d electrons. Changes in the
energy of these electrons correspond to the energy of its visible
light. When white light passes through the colored gemstone
and is reflected by it, some of the energy of the visible light
is also absorbed, causing 3d electrons in the transition metal
ion to undergo its energy change. The light that is transmitted
and reflected appears colored because those colors are corresponding
to 3d-electron energy transitions have also been absorbed. The
table lists several common gemstones, which has
chemical compositions, colors, and the origins of these colors.
A ruby is a crystal form of
alumina, aluminum oxide, containing a trace of chromium (III)
ions replacing some of these aluminum ions. In ruby,
each Al3+ ion and Cr3+ ion is surrounded by five oxide ions in
an octahedral arrangement. This arrangement splits the five 3d
orbitals of Cr3+ into two sets, the orbitals
and the dx2-y2 and dz2 orbitals. These two sets normally have
different energies. The energy difference between these sets corresponds
to its energy of visible light. When white light strikes the ruby,
the gem absorbs the light of energy corresponding
to the transition of an electron from the lower-energy set of
3d orbital’s to the higher-energy set.
| Gem |
Formula |
Color |
Origin of color |
| Ruby |
Al2O3 |
Red |
Cr3+ replacing Al3+ in its octahedral sites |
| Emerald |
Be3Al2(SiO3)6 |
Green |
Cr3+ replacing Al3+ in its octahedral site |
| Alexandrite |
Al2BeO4 |
Red/Green |
Cr3+ replacing Al3+ in its octahedral site |
| Garnet |
Mg3Al2(SiO4)3 |
Red |
Fe2+ replacing Mg2+ in its 8-coordinate site |
| Peridot |
Mg2SiO4 |
Yellow-green |
Fe2+ replacing Mg2+ in its 7-coordinate site |
| Tourmaline |
Na3Li3Al6(BO3)3(SiO3)6F4 |
Pink |
Mn2+ replacing Li+ and Al3+ in its octahedral site |
| Turquoise |
Al6(PO4)4(OH)8
• 4H2O |
Blue-green |
Cu2+ coordinated to 4 OH¯ and 2 H2O |
| Sapphire |
Al2O3 |
Blue |
Intervalence transition between Fe2+ and Ti4+ replacing Al3+ its adjacent octahedral sites |
| Aquamarine |
Be3Al2(SiO3)6 |
Blue |
Intervalence transition between Fe2+ and Fe3+ replacing Al3+ in adjacent octahedral sites |
| Diamond |
C |
Colorless |
Color centers from nitrogen atoms trapped in crystal |
|
|