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Interferometry is the technique of superposing (interfering) two
or more waves, to detect differences between them. Interferometry is applied in a wide variety of
fields, including astronomy, fiber
optics, optical metrology, oceanography,
seismology, quantum mechanics and plasma
physics.
Interferometer
An interferometer works because two waves with the same frequency that have the same
phase will add to each other while two waves that have opposite phase will cancel out,
assuming both have the same amplitude. Early interferometers principally used white light sources (e.g., Young's double slit experiment of 1805). Modern researchers often
use monochromatic light sources like lasers, and even the wave
character of matter can be exploited to build interferometers (e.g. with electrons,
neutrons, atoms, or even
molecules).
Types of Interferometers
-
There are many types of interferometers, but all work on the same basic principle.
Michelson Interferometer
-
A Michelson interferometer.
In a Michelson (or Michelson-Morley) type interferometer, the basic building
blocks are a monochromatic source (emitting light or matter waves), a detector, two mirrors and one semitransparent
mirror (often called beam splitter). These are put together as shown in the figure.
There are two paths from the (light) source to the detector. One reflects off the semi-transparent mirror, goes to the top mirror and then reflects back, goes through the semi-transparent mirror, to the detector. The other one goes
through the semi-transparent mirror, to the mirror on the right, reflects back to the semi-transparent mirror, then reflects from
the semi-transparent mirror into the detector.
If these two paths differ by a whole number (including 0) of wavelengths, there is
constructive interference and a strong signal at the detector. If they differ by a
whole number and a half wavelengths (e.g., 0.5, 1.5, 2.5 ...) there is destructive interference and a weak signal. This might
appear at first sight to violate conservation of energy. However energy is conserved, because there is a re-distribution of
energy at the detector in which the energy at the destructive sites are re-distributed to the constructive sites. The effect of
the interference is to alter the share of the reflected light which heads for the detector and the remainder which heads back in
the direction of the source.
This type of interferometer was used in the Michelson-Morley experiment,
to disprove the existence of the Luminiferous aether. Michelson interferometers are also used in astronomical interferometers (see astronomical
section below) and gravitational wave detectors.
Mach-Zehnder interferometer
A Mach-Zehnder interferometer.
-
Interferometers are used in integrated optical circuits, in the form of a
Mach-Zehnder interferometer, in which light interferes between two branches
of a waveguide that are (typically) externally modulated
to vary their relative phase. This interferometer's configuration consists of two beam splitters and two completely reflective
mirrors. The source beam is split and the two resulting waves travel down separate paths. A slight tilt of one of the beam
splitters will result in a path difference and a change in the interference pattern. The Mach-Zehnder interferometer can be very difficult to align, however its improved sensitivity
enables a diverse number of applications.[1] The Mach-Zehnder interferometer can be
the basis of a wide variety of devices, from RF modulators to sensors to optical switches.
Sagnac interferometer
-
A Sagnac Interferometer is an interferometry configuration in which a beam of light is split and the two beams are made to
follow a trajectory in opposite directions. To act as a ring the trajectory must enclose an area. On return to the point of entry
the light is allowed to exit the apparatus in such a way that an interference
pattern is obtained.
In the Sagnac configuration, the position of the interference fringes is dependent on angular velocity of the setup. This dependence is caused by the rotation effectively shortening the
path distance of one of the beams, while lengthening the other. A Sagnac interferometer has been used by Albert Michelson and Henry Gale to determine the angular
velocity of the Earth. It can be used in navigation as a ring laser gyroscope,
which is commonly found on fighter planes[2].
Fabry-Perot interferometer
A Fabry-Pérot interferometer or etalon
-
A Fabry-Pérot interferometer or etalon is typically made of a transparent plate with two reflecting surfaces, or two parallel highly-reflecting mirrors. (Technically the former is an
etalon and the latter is an interferometer, but the terminology is often used
inconsistently.) Its transmission spectrum as a function of wavelength exhibits peaks of large transmission corresponding to resonances of the etalon. It is named after
Charles Fabry and Alfred Pérot.
Fabry-Pérot interferometers are widely used in telecommunications, lasers and spectroscopy for controlling and measuring the
wavelength of light. Recent advances in fabrication technique allow the creation of very precise tunable Fabry-Pérot
interferometers. Fabry-Pérot interferometers also form the most common type of optical cavity used in laser construction.
Types of Interferometry
Coherent interferometry
Coherent interferometry uses a coherent light source (for example, a helium-neon laser), and can make interference with large
difference between the interferometer path length delays. The interference is capable of very accurate (nanometer) measurement by
recovering the phase.
One of the most popular methods of interferometric phase recovery is phase-shifting by piezoelectric transducer (PZT) phase-stepping. By stepping the path length by a number of known
phases (minimum of three) it is possible to recover the phase of the interference signal, with 2π = λ /
2.
Coherent interferometry suffers from a 2π ambiguity problem: that is, if between any two
measurements the interferometric phase jumps by more than 2π the phase measurement is incorrect.
However by combining interferometry results obtained using multiple wavelengths of illumination, such as in digital
multi-wavelength holography, the ambiguity interval can be extended to indefinitely large dynamic ranges of measurement.
The applications of coherent interferometry are wide ranging: Nanometer surface profiling, Microfluidics, Mechanical stress/strain, Velocimetry, and high-definition metrology of large parts and assemblies in manufacturing.
Inertial navigation
In inertial navigation, ring laser
gyroscopes are used that can detect rotation through optical interferometry of laser beams travelling around a
circumference in opposite directions
Speckle Interferometry
-
In optical systems, a speckle pattern is a field-intensity pattern produced by the mutual interference of partially coherent
beams that are subject to minute temporal and spatial fluctuations. This speckling effect is most commonly observed in the fields
of fiber optics and astronomical speckle imaging.
Holography
A special application of optical interferometry using coherent light is holography, a
technique for photographically recording and re-displaying three-dimensional scenes. The technique also lends itself to
monitoring small deformations in single wavelength implementations as well as dimensional metrology of large parts and assemblies
and larger surface defect detection when used in multi-wavelength implementations..
Low-coherence interferometry
Low-coherence interferometry utilizes a light source with low temporal coherence such as white light (for example, LED/SLD,
halogen lamp) or high specification femtosecond lasers. Interference will only be achieved when the path length delays of the
interferometer are matched within the coherence time of the light source (note: using a femtosecond source is somewhat more
intricate).
The chief benefit of low-coherence interferometry is that it does not suffer from the 2π
ambiguity of coherent interferometry, and is therefore suited to profiling steps and rough surfaces. The axial resolution of the
system is determined by the coherence length of the light source and is typically in the micrometer range.
Optical coherence tomography is a medical imaging technique based in
low-coherence interferometry, where subsurface light reflections are resolved to give tomographic visualization. Recent advances
have striven to combine the nanometer phase retrieval with the ranging cabability of low-coherence interferometry.
Geodetic standard baseline measurements
A famous use of white light interferometry is the precise measurement of geodetic standard
baselines as invented by Yrjö Väisälä. Here, the light path is split in two, and one
leg is "folded" between a mirror pair 1 m apart. The other leg bounces once off a mirror 6 m away. Only if the second path is
precisely 6 times the first, will fringes be seen.
Starting from a standard quartz gauge of 1 m length, it is possible to measure distances up to
864 m by repeated multiplication. Baselines thus established are used to calibrate geodetic
distance measurement equipment on, leading to a metrologically traceable scale for
geodetic networks measured by these instruments.
More modern geodetic applications of laser interferometry are in calibrating the divisions on levelling staffs, and in monitoring the free fall of a reflective prism within a ballistic or absolute gravimeter, allowing determination of gravity, i.e., the acceleration of free fall, directly from the physical definition at a few parts in a billion accuracy.
Astronomical Interferometry
- See also: astronomical
interferometer
In astronomy interferometry is used to combine signals from two or more
telescopes to obtain measurements with higher resolution than could be obtained with either
telescopes individually. This technique is the basis for astronomical
interferometer arrays, which can make measurements of very small astronomical objects if the telescopes are spread out
over a wide area. If a large number of telescopes are used a picture can be produced which has resolution similar to a single telescope with the diameter of the combined spread of telescopes. These include radio telescope arrays such as
LOFAR and SKA, and more recently astronomical optical interferometer arrays such as COAST, NPOI and IOTA, resulting
in the highest resolution optical images ever achieved in astronomy. The VLT
Interferometer is expected to produce its first images using aperture
synthesis soon, followed by other interferometers such as the CHARA array and the
Magdalena Ridge Observatory Interferometer which may consist
of up to 10 optical telescopes. If outrigger telescopes are built at the Keck
Interferometer, it will also become capable of interferometric imaging.
Astronomical interferometers come in two types -- direct detection and heterodyne. These differ only in the way that the
signal is transmitted. Aperture synthesis can be used to computationally simulate a
large telescope aperture from either type of interferometer.
Astronomical direct-detection interferometry
A simple two-element optical interferometer.
A single large telescope with an
aperture mask over it (labelled
Mask), only allowing light through two small holes.
One of the first astronomical interferometers was built on the
Mount Wilson Observatory's reflector telescope in order to measure the
diameters of stars. This method was extended to measurements using separated telescopes by Labeyrie (1975) to the visible. The
red giant star Betelgeuse was among the first to have its diameter determined in this way. In
the late 1970's improvements in computer processing allowed for the first "fringe-tracking" interferometer, which operates fast
enough to follow the blurring effects of astronomical seeing, leading to the Mk I,
II and III series of interferometers. Similar techniques have now been applied at other astronomical telescope arrays, including
the Keck Interferometer and the Palomar Testbed Interferometer.
Techniques from Very Long Baseline Interferometry (VLBI), in which
a large aperture is synthesized computationally, were implemented at optical and
infrared wavelengths in the 1980s by the Cavendish Astrophysics Group. This
providing the first very high resolution images of nearby stars. In 1995 this technique was demonstrated on an array of separate optical telescopes as a Michelson Interferometer for
the first time, allowing a further improvement in resolution, and allowing even higher resolution imaging of
stellar surfaces. The same technique has now been applied at a number of other astronomical telescope arrays, including the
Navy Prototype Optical Interferometer and the IOTA array and soon the VLTI, CHARA and MRO Interferometers.
Projects are now beginning that will use interferometers to search for extrasolar
planets, either by astrometric measurements of the reciprocal motion of the star (as used by the Palomar Testbed Interferometer and the VLTI) or through the
use of nulling (as will be used by the Keck Interferometer and Darwin).
A detailed description of the development of astronomical optical interferometry can be found here. Impressive results were
obtained in the 1990s, with the Mark III measuring diameters of 100 stars and many accurate
stellar positions, COAST and NPOI producing many very high resolution images, and ISI measuring stars in the mid-infrared for the first time. Additional results include
direct measurements of the sizes of and distances to Cepheid variable stars, and
young stellar objects.
Interferometers are mostly seen by astronomers as very specialized instruments, capable of a very limited range of
observations. It is often said that an interferometer achieves the effect of a telescope the size of the distance between the
apertures; this is only true in the limited sense of angular resolution. The combined
effects of limited aperture area and atmospheric turbulence generally limit interferometers to observations of comparatively
bright stars and active galactic nuclei. However, they have proven useful for
making very high precision measurements of simple stellar parameters such as size and position (astrometry) and for imaging the nearest giant stars.
For details of individual instruments, see the list of astronomical interferometers at visible and
infrared wavelengths.
Astronomical heterodyne interferometry
Radio wavelengths are much longer than optical wavelengths, and the observing stations in radio astronomical interferometers
are correspondingly further apart. The very large distances do not always allow any usable transmission of radio waves received
at the telescopes to some central interferometry point. For this reason many telescopes instead record the radio waves onto a
storage medium. The recordings are then transferred to a central correlator station where the waves are interfered. Historically
the recordings were analog and were made on magnetic tapes. This was quickly superseded by the current method of digitizing the
radio waves, and then either storing the data onto computer hard disks for later shipping, or streaming the digital data directly
over a telecommunications network e.g. over the Internet to the correlator station. Radio arrays with a very broad bandwidth, and
also some older arrays, transmit the data in analogue form either electrically or through fibre-optics. A similar approach is
also used at some submillimetre and infrared
interferometers, such as the Infrared Spatial Interferometer. Some early
radio interferometers operated as intensity interferometers, transmitting
measurements of the signal intensity over electrical cables to a central correlator. A similar approach was used at optical
wavelengths by the Narrabri Stellar Intensity Interferometer
to make the first large-scale survey of stellar diameters in the 1970s.
At the correlator station, the actual interferometer is synthesized by processing the digital signals using correlator
hardware or software. Common correlator types are the FX and XF correlators. The current trend is towards software correlators
running on consumer PCs or similar commodity hardware. There also exist some radio astronomy amateur digital interferometers with
correlator, such as the ALLBIN of the European Radio Astronomy Club.
As the usual radio astronomy interferometer is digital it does have a few shortcomings, some due to sampling and quantization
effects, in addition to the obvious need for much more computing power, as compared to analog correlation. The output of both
digital and analog correlator can be used to computationally synthesize the interferometer
aperture in the same way as with direct detection interferometers (see above).
References
- John E. Baldwin and Chris A. Haniff. "The
application of interferometry to optical astronomical imaging." Phil. Trans. A, 360, 969-986, 2001. (download PostScript
file)
- J. E. Baldwin, "Ground-based interferometry — the past decade and the one to come" in Interferometry for Optical Astronomy
II, volume 4838 of Proc. SPIE, page 1. 22-28 August 2002, Kona, Hawaii, SPIE Press, 2003. (download PostScript
file)
- J. D. Monnier, Optical interferometry in astronomy, Reports on Progress in Physics, 66, 789-857, 2003 IoP. (download PDF file)
- P. Hariharan, Optical Interferometry, 2nd edition, Academic Press, San Diego, USA, 2003.
- Adolf F. Fercher, Wolfgang Drexler, Christoph K. Hitzenberger and Theo Lasser, "Optical coherence tomography — principles and
applications," Reports on Progress in Physics vol. 66, no. 2, pp. 239-303, 2003. Available: iop.org.
- E. Hecht, Optics, 2nd Edition, Addison-Wesley Publishing Co., Reading, Mass, USA, 1987.
Notes
See also
External links
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