 Hydrostatic balance: the process rests on the
Archimedes' principle, it' necessary to know the volume of the gem. The formula is as follows:
one divides the weight of the stone by his volume. For example, if we have a gemstone which weighs in
the air 5.8 grams and water 3.5
grams, the difference would be of (5.8 - 3.5
= 2.3 grams), that is to say a volume of 2.3
cm3 water. To find its density it would then be enough to divide its weight in the air by its
volume, that is to say (5.8/2.3 =
2.5), this stone would thus have a density of 2.5. |
 Specific gravity: it's a very precise method some which is
dimensions of the specimen. The principle remains very simple: a mineral runs in a liquid of which
the gravity is less, but it will remain in suspension if the gravities are equal and
will float if the liquid with a stronger gravity. To determine the specific gravity of a stone, it will
thus be necessary to find the specific gravity in which the gem will remain in suspension. There are
several specific gravity liquid set in the trade, for example: the broforme (density = 2.90),
liquid of Thoulet (3.19), the iodide of méthylème (3.33),
the solution of Clerici (5). |