Scientific American Supplement, No. 344, August 5, 1882Various
Science
Scientific American Supplement, No. 344, August 5, 1882
Various
Science -- Periodicals
_The Specific Gravity_.--In ascertaining the specific gravity the
following apparatus is necessary: a small pair of hand scales with a set
of weights, from one grain to one ounce. These can be procured from the
apparatus maker, the scales for about fifty cents, and the weights for
not much over the same amount. The scales are prepared for this work by
cutting two small holes in one of the scale pans, near together, with
a pointed piece of metal, and tying a piece of silk thread about eight
inches long into these. In a loop at the end of this thread the mineral
to be examined is suspended. It should be a pure representative of the
mineral it is taken from, should weigh about from one hundred grains to
an ounce, and be quite dry and free from dirt. If the piece of mineral
obtained is very large, this sized portion may be often taken from it
without injury; but it will not do to mar the beauty of a mineral to
ascertain its specific gravity, and it is generally only applicable
when a small piece is at hand. With more weights, however, a piece of a
quarter pound weight may be taken if necessary. The mineral is tied into
the loop and weighed, the weight being set down in the note book, either
in grains or decimal parts of an ounce. Call this result A. It is then
weighed in some water held in a vessel containing about a quart, taking
care while weighing it that it is entirely immersed, but at the same
time does not touch either the sides or bottom. Both weighings should
be accurate to a grain. This result we call B. The specific gravity is
found by subtracting B from A, and dividing A by the remainder. For
instance, if the mineral weighed eight hundred grains when weighed in
the air, and in the water six hundred, giving us the equation: 800
/ (800 - 600) = sp. gr., or 4, which is the specific gravity of
the mineral. If the mineral whose specific gravity is sought is an
incrustation on a rock, or a mixture of a number of minerals, or would
break to pieces in the water, the specific gravity is by this method of
course unattainable, and other data must be used.
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