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Chapter 7 The Microscope
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Physical properties of light
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The Compound Microscope
Schematic diagram of stereoscopic microscope Two separate monocular microscopes Each has own set of lenses except for the lowest Objective lens common to both microscopes
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The Compound Microscope
Condenser: lens system under the microscope stage that focuses light onto the specimen THE MICROSCOPE
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The Comparison Microscope
Two independent objective lenses joined together by an optical bridge to a common eyepiece lens. The objects under investigation are observed side-by-side in a circular field that is equally divided into two parts Modern firearms examination Began with the introduction of the comparison microscope Ability to give the firearms examiner a side-by-side magnified view of bullets THE MICROSCOPE
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Comparison Microscopes
Are used to compare two specimens Consist of two compound microscopes connected by an optical bridge Provide a single eyepiece through which the examiner sees both images side by side Can be lighted from below the stage or via a vertical or reflected illumination system
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The Comparison Microscope
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The Stereoscopic Microscope
Two monocular compound microscopes Three-dimensional image of a specimen Use both eyepiece lenses Evidence not requiring very high magnification (10x–125x) Large working distance Microscopic examination of big, bulky items THE MICROSCOPE
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The Stereoscopic Microscope
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Double-refraction in Calcite:
-the “secret” key to PLM
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Polarizing microscopy
Birefringence Calcite produces two images when it is placed over the blue pencil. One of the images appears normally as when viewing an object through clear glass. The other pencil image appears displaced, due to the nature of doubly-refracted light. When anisotropic crystals refract light, the resulting rays are polarized and travel at different velocities. One of the rays travels with the same velocity in every direction through the crystal and is termed the ordinary ray. The other ray travels with a velocity that is dependent upon the structural properties of the crystal
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f = V/w f-frequency V-velocity of light w-wavelength
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Polarizing microscopy
Polarized light
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Polarizing Microscopy
Plane-polarized Light that is confined to a single plane of vibration Polarizing microscope Examination of the interaction of plane-polarized light with matter THE MICROSCOPE
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Polarizing Microscopy
Wide applications for the study of birefringent materials Materials that split a beam of light in two Each with its own refractive index value Determination of these refractive index data Provides information that helps to identify minerals present in a soil sample or the identity of a man-made fiber. THE MICROSCOPE
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Polarizing Microscopes
Include two polarizing filters, a polarizer lens (fixed below the specimen), and an analyzer lens (fixed above the specimen) The stage with the sample is rotated to determine how the polarized light interacts with the sample
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Polarizing microscope
Polarizer Analyzer
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Polarizing Microscopes
This can provide information about the shape, color, and size of minerals and it is used to identify hair, human-made fibers and paint. Hair Sample: Polarized Light Hair Sample: Natural Light
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Michel-Levy Chart of Birefringence
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f = V/w f-frequency V-velocity of light w-wavelength
f is nearly always constant, therefore is V changes, w must change as well. n (Refractive Index) = c/v c-speed of light in vacuum
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When light crosses boundary of 2 materials with
different refractive indices [n], it is bent
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Polarizing microscopy
Analyzer out of path = plane polarized light; gives specimen’s “true color” Analyzer in path = crossed polars; gives specimen’s interference color Polyester, plane-polarized light Polyester, under crossed polars
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Polarizing microscopy
Improves specimen contrast Stained plant fibers, left – stained; right – polarized light
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Polarizing microscopy
Many crystalline substances are birefringent Forensic analysis of soil components Many synthetic fibers are birefringent
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Refractive Index by the Becke Line Method
Note: when refractive index of mineral & liquid are close, relief if low.
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Plagioclase Feldspar showing albite twinning
-used to determine Plagioclase composition
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