04-basic interferometry and optical testing · 2016. 8. 4. · page 2 4.0 basic interferometry and...
TRANSCRIPT
4.0 Basic Interferometry and Optical Testing
Page 2
4.0 Basic Interferometry and Optical Testing
n 4.1 Two-Beam Interference n 4.2 Pioneer Fizeau Interferometer n 4.3 Twyman-Green Interferometer n 4.4 Fizeau Interferometer - Laser-Source n 4.5 Mach-Zehnder Interferometer n 4.6 Typical Interferograms n 4.7 Interferograms and Moiré Patterns n 4.8 Classical techniques for getting data into
the computer
Page 3
4.1 Two-Beam Interference Fringes
I = I 1 + I 2
+ 2 I 1 I 2 cos ( α 1 - α 2 )
α 1 - α 2 is the phase difference between
the two interfering beams
α 1 - α 2
= ( 2 π
λ ) ( optical path difference )
Page 4
Sinusoidal Interference Fringes
I = I1 + I2 + 2 I1I2 cos(α1 −α2 )2 4 6 8
0.2
0.4
0.6
0.8
1
0.6
0.2
0.4
0.8
1.0
0.0 1 2 3 4 5 6
Page 5
4.2 Pioneer Fizeau Interferometer
1862
Page 6
Typical Interferogram Obtained using Fizeau Interferometer
Page 7
Relationship between Surface Height Error and Fringe Deviation
Surface height error = ( )( )λ2
ΔS
S
Δ (x,y)
Page 8
Fizeau Fringes
For a given fringe the separation
between the two surfaces is a
constant.
Height error = (λ/2)(Δ/S)
Valley
Top View
1 2 3 4 5 6 7
S Δ
Test Reference
Interferogram
Bump
Top View
Δ
Test Reference
1 2 3 4 5 6 7
S
Interferogram
Page 9
Newton’s Rings
Page 10
Fizeau Fringes for Concave and Convex Surfaces
CONCAVE SPHERE CONVEX SPHERE
Thick Part of Wedge
Thin Part of Wedge
Reference Flat Test
Sample Test
Sample
Reference Flat
Page 11
4.3 Twyman-Green Interferometer (Flat Surfaces)
Reference Mirror
Imaging Lens Beamsplitter
Interferogram
Test Mirror
Laser
1918
Page 12
Use of Rotating Ground Glass to Limit Spatial Coherence of Source
Page 13
Use of Rotating Ground Glass in Imaging Optics
Page 14
Polarization Beam Splitter (PBS) Twyman-Green Interferometer
Page 15
Twyman-Green Interferometer (Spherical Surfaces)
Incorrect Spacing Correct Spacing
Laser
Reference Mirror
Test Mirror
Interferogram
Diverger Lens
Imaging Lens Beamsplitter
Page 16
Typical Interferogram
Page 17
4.4 Fizeau Interferometer - Laser Source (Flat Surfaces)
Laser
Beam Expander
Reference Surface
Test Surface
Interferogram
Imaging Lens
Page 18
Fizeau Interferometer - Laser Source (Spherical Surfaces)
Laser
Beam Expander
Reference Surface
Test Mirror
Interferogram
Diverger Lens
Imaging Lens
Page 19
Testing High Reflectivity Surfaces
Laser
Beam Expander
Reference Surface
Test Mirror
Interferogram
Diverger Lens
Imaging Lens
Attenuator
Page 20
Laser
Beam Expander
Reference Surface
Test Mirror
Interferogram
Diverger Lens Imaging Lens
Interferogram
1 2 3 4 5 6 7
Hill or Valley?
Fringe Motion
Push in on mirror
Hill
Page 21
4.5 Mach-Zehnder Interferometer
Testing samples in transmission
Imaging Lens
Beamsplitter
Interferogram
Sample
Laser
Page 22
Laser Beam Wavefront Measurement
Pinhole
Reference Arm
Test Arm Detector Array
Input Source
Page 23
4.6 Interferograms, Interferograms Spherical Aberration
Page 24
Interferograms Small Astigmatism, Sagittal Focus
Page 25
Interferograms Large Astigmatism, Sagittal Focus
Page 26
Interferograms Large Astigmatism, Medial Focus
Page 27
Interferograms Large Coma, Varying Tilt
Page 28
Interferograms Changing Focus
Page 29
Interferograms Combined Aberrations
Page 30
4.7 Interferograms and Moiré Patterns
n In optics moiré refers to a beat pattern produced between two gratings of approximately equal spacing.
n Moiré is a useful technique for aiding in the understanding of interferometry.
Ref: Chapter 16 of Malacara’s Optical Shop Testing book
Page 31
Calculating Moiré Pattern for Arbitrary Gratings
Let the transmission function for two gratings f1(x,y) and f2(x,y) be given by φ(x,y) is the function describing the basic shape of the lines. The b coefficients determine the profile of the lines. When these two gratings are superimposed, the resulting intensity function is given by the product.
f1 x, y( ) = a1 + b1nCos nφ1 x, y( )!" #$n=1
∞
∑
f2 x, y( ) = a2 + b2mCos mφ2 x, y( )!" #$m=1
∞
∑
Page 32
Two Gratings Superimposed
f1 x, y( ) f2 x, y( ) = a1a2 + a1 b2mCos mφ2 x, y( )!" #$m=1
∞
∑ + a2 b1nCos nφ1 x, y( )!" #$n=1
∞
∑
+ b1nn=1
∞
∑ b2mCos nφ1 x, y( )!" #$Cos mφ2 x, y( )!" #$m=1
∞
∑
Term #4 = 12b11b21Cos φ1 x, y( )−φ2 x, y( )"# $%+
12
b1nn=1
∞
∑ b2mCos nφ1 x, y( )−mφ2 x, y( )"# $%m=1
∞
∑
n and m both ≠ 1
+12
b1nn=1
∞
∑ b2mCos nφ1 x, y( )+mφ2 x, y( )"# $%m=1
∞
∑
The first term represents the difference between the fundamental pattern making up the two gratings.
Page 33
Moiré for Two Straight Line Patterns
φ1 x, y( ) = 2πλ
xCos α[ ]+ ySin α[ ]( )
φ2 x, y( ) = 2πλ
xCos α[ ]− ySin α[ ]( )
φ1 x, y( )−φ2 x, y( ) =M2π
Mλ = 2ySin α[ ]
Two gratings of line spacing λ with an angle of 2α between them
the fringe centers are given by
Same result as for interfering two plane waves tilted at an angle of 2α with respect to each other.
Page 34
Interference of Two Spherical Waves
Spherical Wave
Interference
Plane A
Plane B
Page 35
Moiré of Two Zone Plates
Page 36
Moiré Between Two Interferograms 20 λ tilt, and 20 λ tilt + 4 λ defocus
Page 37
Moiré Patterns Showing Third-Order Aberrations
22λ tilt, 4λ sph, -2 defocus 20λ tilt, 5λ coma 20λ tilt, 7λ ast, -3.5 defocus
Moiré of above with 20λ tilt
Note: Tilt pattern on previous slide
Page 38
Moiré Pattern by Superimposing Two Identical Interferograms
Same orientation with slight rotation
One pattern is flipped
Page 39
Moiré Pattern Formed Using Two Identical Interferograms with Shear
Vertical Shear
Vertical Shear plus Rotation
Horizontal Shear
Horizontal Shear plus Rotation
Original Pattern: 22λ tilt, 4λ spherical, -2 defocus
Page 40
Comments on Moiré Patterns
n Moiré patterns are produced by multiplying two patterns.
n A moiré pattern is not obtained if two intensity functions are added because the difference term shown in the derivation of moiré patterns is not present.
n The only way to get a moiré pattern by adding two intensity functions is to use a nonlinear detector that produces terms proportional to the product of the two intensity functions. For example
Nonlinear Response = a(I1 + I2 )+ b(I1 + I2 )2 +
Page 41
4.8 Classical Techniques for Getting Data into the Computer
n Elementary analysis of interferograms
n Computer analysis of interferograms
Page 42
Typical Interferogram
Classical Analysis Measure positions of fringe centers.
Deviations from straightness and equal spacing gives aberration.
Surface Error = (λ/2) (Δ/S)
Page 43
Elementary Interferogram Analysis
n Estimate peak to valley (P-V) by looking at interferogram.
n Dangerous to only estimate P-V because one bad point can make optics look worse than it actually is.
n Better to use computer analysis to determine additional parameters such as root-mean-square (RMS).
Page 44
Computer Analysis of Interferograms
Largest Problem Getting interferogram data into
computer
Solutions • Graphics Tablet • Scanner • CCD Camera • Phase-Shifting Interferometry
Page 45
Digitization
Page 46
Automatic Interferogram Scanner
One solution Video system and computer automatically
finds locations of two sides of interference fringe where intensity reaches a given value.
Fringe center is average of two edge locations.
Page 47
Computer Analysis Categories
n Determination of what is wrong with optics being tested and what can be done to make the optics better.
n Determination of performance of optics if
no improvement is made.
Page 48
Minimum Capabilities of Interferogram Analysis Software
• RMS and P-V • Removal of desired aberrations • Average of many data sets • 2-D and 3-D contour maps • Slope maps • Spot diagrams and encircled energy • Diffraction calculations - PSF and MTF • Analysis of synthetic wavefronts