Minerals in rock sections : $b The practical methods of identifying minerals in rock sections with the microscope, especially arranged for students in technical and scientific schoolsLuquer, Lea McIlvaine
Science
Minerals in rock sections : $b The practical methods of identifying minerals in rock sections with the microscope, especially arranged for students in technical and scientific schools
Luquer, Lea McIlvaine
Petrology -- Laboratory manuals
For the _nicol prism_ “a cleavage rhombohedron of calcite (the variety
Iceland spar is universally used in consequence of its transparency) is
obtained, having four large and two small rhombohedral faces opposite
each other. In place of the latter planes, two new surfaces are cut,
making angles of 68° (instead of 71°) with the obtuse vertical edges;
these then form the terminal faces of the prism. In addition to this,
the prism is cut through in the direction HH′, Fig. 3, the parts then
polished and cemented together again with Canada balsam. A ray of light,
_ab_, entering the prism, is divided into two rays polarized at right
angles to each other. One of these, _bc_, on meeting the layer of balsam
(whose refractive index is less than that of the ray _bc_), suffers
total reflection, and is deflected against the blackened sides of the
prism and extinguished. The other, _bd_, passes through and emerges at
_e_, a completely polarized ray of light, that is, a ray with vibrations
in one direction only, and that the direction of the shorter diagonal of
the prism.”[18] The vertical plane through the shorter diagonal may be
called the _plane_ of _vibration_[19] of the nicol.
[Illustration:
FIG. 2.
]
[Illustration:
FIG. 3.
]
The polarizer must be below the stage _c_, and is generally adjusted so
as to have its plane of vibration parallel to the N. and S. cross-wire
in the eye-piece _o_. It is important to know the direction of the plane
of vibration of the polarizer or lower nicol, as we can then determine,
when absorption of light occurs in a mineral, the direction in this
mineral parallel to which the absorbed rays are vibrating. The polarizer
slides in an outer shell or frame, and, by means of a lever _d_, can
easily be raised or lowered.
A convenient test for the location of this plane of vibration of the
polarizer is as follows: Make use of a section of biotite, cut at right
angles to the basal plane, hence showing the basal cleavage cracks.
Biotite has the property of absorbing to a marked extent the light
vibrating parallel to these cleavage cracks. Rotate such a section on
the stage of the microscope until the position of maximum darkness is
reached and when such is the case the plane of vibration of the
polarizer must be parallel to these cleavage cracks.
On the top of the nicol is placed the _condensing lens_ for getting
_convergent_ light, and the adjustments are so arranged that when the
nicol is up as far as it will go, the condensing lens[20] is brought
almost in contact with the lower surface of the transparent section
resting on the stage.
Public-domain text, read in full here on John Shaqi.
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