Stellar Photometry
by Terry Moon
March 2004
In the second century BC, the Greek astronomer Hipparchus, introduced a system
where the brightest star in each constellation was classified as first magnitude.
In 140AD Ptolemy refined Hipparchus' system by using a brightness scale of 1 to
6 where the brightest stars were called Magnitude 1 and the faintest, that is
those just visible to the naked eye, Magnitude 6. This scale is still used today
having been extended to objects fainter than 6th magnitude and brighter than 1st
magnitude. Accurate measurement of magnitudes, however, was only made possible
in the 20th century through the advent of photoelectric devices.
Stellar photometry is that branch of astronomy that deals with the accurate
measurement of the brightness of stars and the changes in their brightness over
time. It probably had its beginnings in the 18th Century with the techniques
introduced by Bouger in 1729 and Lambert in 1760. The era of well-determined,
reproducible measure-ments may be considered as starting in 1850 when Podgson
defined an increase of 1 magnitude as equivalent to a decrease in brightness of
0.4.1 Following this Zollner constructed the first visual stellar photometer in
1861. Photographic photometry was introduced in 1904 and the international
photoelectric system of Johnson and Morgan was established in 1951.
As photoelectric devices, such as photomultiplier tubes, photodiodes and
charge-coupled devices (CCDs), have replaced the photographic plate and visual
equipment in professional observatories, any discussion of the accurate
measurement of starlight now focuses on techniques using these devices.
Photoelectric Devices
Figure 1: Photomultiplier
Photoelectric detectors convert light into an electrical signal. There are
three detector types: the photomultiplier tube, photodiode and charge-coupled
device (CCD).
The photomultiplier (Figure 1) is a vacuum-tube device with a
special surface that gives off electrons when light falls on it. A chain of
diodes at different voltages gives rise to a cascade of electrons thus multiply
ing the original signal a million times or more. Photomultiplier tubes have high
gain and low noise but are prone to damage (both mechanical and through exposure
to very bright light) and respond to only a limited range of wavelengths.
In contrast the photodiode is a solid-state semiconductor device (Figure 2).
Light falling on it causes electrons to flow in the 'conduction band' of the
semiconductor material. Photodiodes are cheap, robust and respond to light from
the ultraviolet through to the infrared but are not as sensitive as
photomultiplier tubes. The avalanche photodiode is a different type of
solid-state detector that not only detects the light falling on it but also
amplifies the signal generated by a factor of fifty or more.
More recently astronomers have turned to CCDs (Figure 3). These are solid-state
devices with an array of picture elements called pixels. Each pixel is a tiny
detector – a CCD array can have tens of thousands to one million or more pixels!
In addition to providing excellent images of astronomical objects in much
shorter exposure times than photographic film, the charge accumulated in each
pixel from light falling on it can be readout and measured. In this way the
magnitudes of stars can be measured accurately. CCDs are very sensitive, respond
to light over a wide range of wavelengths from the ultraviolet to infrared, and
can measure many stars at once in contrast to photomultiplier tubes and
photodiodes that measure one star at a time.
Figure 2: Photodiode
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Figure 3: CCDs
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Measuring Colours
The difference in colours of stars can be seen visually but measuring such
differences can tell us about the lives and times of stars. By carefully
choosing filters that isolate certain wavelengths of light astronomers
determine the luminosities, surface temperatures and gravities of stars and
infer changes in radius and differences in chemical composition. For binaries
their orbital dynamics can be determined from the light curves obtained through
photoelectric measurements.
The most common system in use is that introduced by Johnson and Morgan in 1951
known as the UBV system. It comprises three wavelength bands isolated using
ultraviolet, blue and green filters.
Since its initial introduction it has been extended to include red (R) and
infrared (I) bands. Of particular importance are measurements in the V band that
can be related to a star's intrinsic brightness (luminosity), and the B-V colour
index, formed by taking the difference in measurements in the B and V bands.
The B-V colour index serves as a good indicator of a star’s surface temperature.
Looking Through the Atmosphere
Figure 4: Looking through atmosphere
The Earth's atmosphere affects the starlight that passes through it. In
addition to dimming stars, it changes their colours and introduces fluctuations
in brightness.
There are random fluctuations in both the observed position and intensity of a
star. The latter is known as scintillation and commonly referred to as
'twinkling' of stars. Usually astronomers refer to both effects collectively as
'seeing' and estimate how good or bad the observing conditions are by noting
the apparent size of the image of a star in seconds of arc.
In photoelectric photometry an estimate of the quality of the observing can be
made by taking a series of consecutive measurements then calculating how much
they vary from an average value.
Where the variations are 1% or less (corresponding to about 0.01 magnitude), the
conditions are considered to be 'photometric'.
As stars rise or set their brightness changes because they are being viewed
through different thicknesses of atmosphere. Figure 4 illustrates this – the
scale used is 'air masses' where an air mass = 1 corresponds to the thickness of
atmosphere through which a star is seen when it is overhead, i.e. at a Zenith
angle of 0º2
This change in the measured brightness of a star as it is viewed through
different thicknesses of atmosphere must be corrected for. Because the
transparency of the atmosphere may change from night to night measurements are
corrected, not to an air mass = 1, but to the magnitude that would be
observed in the absence of the atmosphere (i.e. air mass = 0). How much
easier would photo-electric photometry be on the Moon!
References
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AAVSO 2001, Manual for Visual Observing of Variable Stars, American
Association of Variable Star Observers, Cambridge, Massachusetts, USA,
Revised Edition – January 2001.
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Douglas George 1995, 'Starting Out Right', CCD Astronomy, pp. 18-23,
summer.
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Kenneth J. Kaufmann 2000, 'Light Levels and Noise Guide: Detector
Choices', Photonics Spectra, July.
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Albrecht Unsöld 1969, The New Cosmos, Springer-Verlag, New York.
1 This is often stated as a magnitude difference of 5 corresponding to a change in brightness of 100.
2 Zenith angle is measured from 0º directly overhead to 90º at the horizon.
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