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The Polariscope, here a pocket polariscope. |
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It is the usual means by which one differentiates on the one hand |
the unirefractives substances (amorphous or coming from the cubic |
system) and the birefractives substances, coming from the other |
systems of crystallization. |
This instrument is composed of two filters polarizing between which |
the stone is placed, and it is while turning the filter of the top that |
the analysis can be done. |
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The refractometer is used to determine the indexes of refraction |
of the stone. This instrument calculates speed with which luminous |
rays arise from the stone and indicates it on a scale. The gem is |
placed on a coated pane of a fine particle of liquid made up amongst |
other things of methylene iodide which shows an index of refraction |
of 1.81 (this liquid is toxic) |
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Dichroscope of which the principal part is made up of a tube |
comprising a window with the one of the ends and a lens with the |
other, between the two is assembled a piece of calcite, chosen |
because of its strong double refraction so that two images of the |
window appear side by side to the observer which looks in the |
eye-glass. The light of the adjacent images of the window vibrates |
in two perpendicular plans one to the other at a rate of one only plan |
for each image. The rotation of the stone is a significant factor |
during the control of dichroism, bus in all the double refraction |
stones, it exists one or two directions of unirefringence, known as |
optical axe. |
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The Chelsea color filter. There is a very effective means to |
reveal the subjacent differences in color, it is the use of colored |
filters. |
They are especially effective in the differentiation of natural and |
synthetic emerald. |
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The optical fiber lamp is useful to distinguish inclusions in rough |
stones. |
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Microscopes: the binocular one, i.e. to double objective is best |
adapted for gemology. The microscope is of first importance in |
the detection of counterfeits. Indeed, the study of inclusions |
which the stone can contain is a practical means to identify the |
gems while explaining to a certain extent the conditions under which |
they were formed in nature. |
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Malaya garnet discovery |
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The spectroscope concerns an extremely simple method which |
allow the identification of all the stones; rough or polished not being |
able to be seen with the refractometer and which even makes it |
possible to distinguish certain synthetic or glasses. This method |
makes it possible to analyze the nature of the dye of the stone. The |
way in which the spectroscope analyzes the various wavelengths of |
the light is in theory very simple; that depends on the different |
degree of refraction to which its subjected various rays of each color |
(wavelength) when they are propagated through a prism of glass or |
another transparent substance. After having passed through a |
prism, a narrow parallel beam of white light is spread out in a ribbon |
with the colors of the rainbow, the visible spectrum. |
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Let us note that a powerful instrument used in many fields of science |
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is at disposal of the gemologists, it is the microscope of Raman which |
spectroscopy supplements the traditional technology of the |
laboratory. This instrument can give information on samples lower |
than 1µm what is not accessible to any technique. The use of the |
Raman spectroscopy by imagery is unique in order to determine in a |
nondestructive way the molecular composition of inclusions present |
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in the gems. |
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