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 — John Shaqi
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
Characters Observed with both Polarizer and Analyzer[46] in Position,
that is with “Crossed Nicols.”
When the nicols are accurately crossed, the field should be quite dark,
and if this is not the case the adjustments must be looked to. The
condensing lens should be removed for these tests as they are to be made
with parallel light, but as a matter of convenience instead of removing
the condensing lens, the polarizer with the lens on top may be lowered,
when the results will be about the same as with parallel light. White
light is supposed to be used.
▄Isotropic Character.▄ Sections of isotropic crystals are perfectly dark
and remain so during a complete rotation of the stage through 360°. The
explanation is very simple. Light being transmitted by an isotropic
crystal in all directions without double refraction; it follows that the
light from the polarizer, after having passed through the section, comes
to the analyzer still vibrating in the plane of vibration of the
polarizer. Hence it is entirely cut out by the analyzer.
_Amorphous_ transparent substances act in the same way and remain dark
during complete rotation of the stage.
_Optical anomalies_, _i. e._, double refraction, may occur in isometric
crystals and in amorphous substances that have been subjected to
strains.
▄Anisotropic Character.▄ Sections of anisotropic crystals, having the
property of _double refraction_, produce in general some _interference_
or _polarization color_, except as mentioned later. The popular
explanation is as follows:
[Illustration:
FIG. 16.
]
In Fig. 16, let PP′ be the plane of vibration of the polarizer, and A′A
the plane of vibration of the analyzer. All the light, after it has
passed through the polarizer, is vibrating parallel to PP′ when it
reaches the lower side of the transparent crystal, _cdef_, on the stage
of the microscope. In this transparent section let _ob_ and _oa_ be the
two _directions_ of _vibration_, _i. e._, the only two directions
parallel to which rays of light can vibrate in passing through the
section.
Let _om_ represent the amplitude of vibration of a ray from the
polarizer. When this ray reaches the section it cannot get through it
vibrating in the direction _om_, but is doubly refracted and of the two
resulting rays, one gets through vibrating in the direction _ob_ and the
other vibrating in the direction _oa_. From _m_ draw perpendiculars to
_ob_ and _oa_. Then according to the law of the parallelogram of forces
_ob_ will represent the amplitude of vibration of the ray passing
through the crystal vibrating in the direction _ob_, and _oa_ will
represent the amplitude of vibration of the ray passing through the
crystal vibrating in the direction _oa_. We will thus have two rays
passing through the crystal, polarized at right angles to each other.
[Illustration:
FIG. 17.
]
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