Photo electic Photometry Lab

1 Ob jectives

To learn how to make precise measurements of stellar brightnesses, and how the Earth's atmo-

sphere a ects our ability to measure brightness.

1. Learn how to measure stellar brightness with a photo electric photometer

2. Get go o d familiarity with the celestial sphere

3. Analysis of data, estimation of errors

4. Learn ab out Standards in measurement and calibration

5. Learn how the atmosphere e ects starlight that passes through it

2 Skills Required

This is an advanced lab b ecause it requires some knowledge of observing so that the team is

ecient enough to get all the required data, and will require extensive data analysis. The

equipment used in this lab is very easy to use. Skills used:

 Polar Alignment of telescop e, use of setting circles

 Ability to nd things using charts

 Statistical Analysis

 Spherical Trigonometry

 Understanding Sidereal time, Hour Angle, Airmass

 Linear Least Squares ts

3 Background

Photometry is a quantitativeway to measure the brightness of a star. Photometry is imp ortant

in photography, astronomy, and illumination engineering. Instruments used for photometry are

called photometers. Lightwaves stimulate the human eye in di erent degrees, dep ending on the

wavelength of the light. Because it is dicult to make an instrument with the same sensitivity

for di erent wavelengths as the human eye, photometers need sp ecial colored lters to make

them resp ond like the human eye.

Photometry is very imp ortant in astronomy b ecause it gives the astronomer a direct measure

of the energy output of , or of the amount of light re ected or scattered by surfaces of

planets and other small b o dies. Colors, or measurements of the amount of light through lters

centered at di erentwavelengths can give information on the temp eratures of stars. 1

3.1 The Photomultiplier

The key to the op eration of the photomultiplier is called the photoelectric e ect, discovered in

1887 by H. Hertz. When light strikes a metal surface, electrons are released, the numb er released

b eing prop ortional to the intensity of the light. Electrons are b ound to the metal by electric

forces, and light with sucient energy can lib erate the electrons. The way a photometer works

is that light enters the instrument and strikes the photo catho de made of a metal chosen so

that optical light exceeds the threshold for release of the electrons. For typical materials the

quantum eciency is ab out 10, meaning for every 100 incident photons, only 10 electrons

are released. In order to get enough electrons to measure as a current, the photo catho de is places

in a multiplier tub e. A series of dyno des are kept at electric p otentials less negative than the

photo catho de, thus the released electrons are accelerated and travel toward the dyno de. The

impacts of the electrons on the dyno de release ab out 4-5 times as many electrons, and these

are accelerated to another dyno de at an even less negative p otential. This pro cess is rep eased

many times until there is a large cascade of electrons which can b e measured at the last dyno de

called the ano de. At the end of the multiplication chain, 1 initial electron can deliver ab out 4

10

 10 electrons at the ano de!

Figure 1: Diagram of a photomultiplier, from N. Gin

4 Exp eriment

In this lab you will measure the brightness of some variable stars, and fully calibrate them.

Figure 2 shows an example of an unusual typ e of , called an R Coronis Borealis

star. It varies irregularly in brightness { usually b eing very bright, but o ccasionally growning

faint. For this typ e of star, dust in the star's atmosphere condenses out o ccasionally and blo cks

the starlight. The star gets bright again when the star heats up and vap orizes the dust or blows

it o .

We will rep ort our brightnesses in the standard V visual and R red astronomical mag-

nitude system. Magnitudes arose historically from the ancient greeks who listed the brightest

stars in the sky as having \ rst imp ortance" or rst magnitude. The next brightest as having

\second imp ortance" or second magnitude. The eye is actually a logarithmic detector, and this

system as b een formalized such that each magnitude di erence is a factor of 2.5 in brightness.

We will b e measuring an electric current or counts photons p er second, C , from the star, and

this has to b e converted into a magnitude m system. This is done with the following equation: 2

Figure 2: Data on R Coronis Borealis from mid 1966 through mid 1996.

m = 2:5 logC  1

4.1 Eclipsing Binaries

Eclipsing Binaries are a typ e of variable which is not varying intrinsically. Instead

the apparent brightness variation is caused by the geometry as viewed from earth of a pair of

orbiting stars. As one star passes in front of another the starlight dims. There will b e 2 eclipses

each p erio d, and the eclipse with the greatest light loss will b e called the primary eclipse. This

o ccurs when the hotter, brighter star is blo cked from view. The light curves are imp ortant to

study b ecuase they contain information ab out the star's sizes, their shap es, mass exchange, and

star sp ots.

Information ab out sp eci c eclipsing binary systems in Table 1 are listed b elow:

 The AW UMa system is probably either a triple or quadruple star system. The masses of

the primary stars are M = 1.790.14M , and M = 0.1430.011M . The third star

1 2

has an apparent mass of M = 0.850.13M .

1

  Lib is a chemically p eculiar close contact system.

 The star 68 Herculis u Herculis, HD 156633, SAO 65913 is a Beta Lyrae typ e eclipsing

binary. It was discovered to be variable by J. Schmidt in 1869, and was found to be an

eclipsing binary in 1909 by Baker. The maximum magnitude of the system is ab out 4.7

and the minima alternate b etween ab out 5.0 and 5.4. Figure 3 shows a set of observations

made by Phil McJunkins Texas A&M Univ. and Dan Bruton Austin State Univ.. 3

Figure 3: Lightcurve of eclipsing binary 68 u Her.

4.2 Intrinsic Variable Stars

Intrinsic variables are stars whichvary in brightness b ecause of internal changes which can cause

pulsations. Some of the pulsations can b e very long overayear while others can b e short. For

this lab we will select only short-p erio d variables of the following typ es:

  Scuti stars {low amplitude, sinusoidal b ehavior with p erio ds < 0.3 dy.

 Dwarf Cepheids { Amplitudes < 1 mag, p erio ds < 0.3 day and can have asymmetric light

curves.

 RR Lyrae stars { Similar the Dwarf Cepheids, with p erio ds b etween 0.3 to 1.0 day.

Below is a description of the intrinsic variable stars which might be observed during the

lab.

Below are some brief descriptions of the intrinsic variable stars included in this lab.

 The Bo otes variable star is a rapidly rotating A-typ e dwarf star which has avery small

p erio dicity 38 min and probable low amplitude variation thus is not our rst choice for

a target. This star p ossesses a circumstellar dust disk.

 V703 Sco is a p ost-main sequence red giant star, adwarf Cepheid.

 X Sgr is a sp ectroscopic binary system with a cepheid variable star. The orbital p erio d of

the companion star is 507.25 days.

Note: the columns with 7UT, 8UT and 9UT show the airmass and altitude of the ob jects

as a function of time. 4

Table 1: Candidate Variable Stars

Name 2000  2000 V Typ e Per 7UT 8UT 9UT

AW UMa 11:30:04 +29:57:53 WUMa 6.8-7.1 0.43 38044.782 1.4/46 1.8/33 2.9/20

Bo o 14:16:10 +51:22:02  Sct 6.5-7.1 0.267 39370.422 1.2/58 1.2/54 1.4/47

 Lib 15:00:58 {08:31:08 EA/SD 4.9-5.9 2.33 22852.360 1.1/61 1.1/61 1.2/53

68 u Her 17:17:20 +33:06:00 Lyr 4.7-5.4 2.05 27640.654 1.3/52 1.1/64 1.0/73

V703 Sco 17:42:17 {32:31:23 RRLyr 7.8-8.6 0.115 37186.365 2.4/24 1.8/33 1.6/40

X Sgr 17:47:34 {27:49:50  Cep 4.2-4.9 7.01 35643.31 1.8/32 1.4/44 1.2/52

W Sgr 18:05:01 {29:34:48  Cep 1.58-3.98 7.59 34587.26 2.0/30.2 1.5/42 1.3/52

4.3 Op en Clusters

Op en clusters are groupings of stars which physically reside in the same place in space i.e.

they are all at approximately the same distance from the earth, and formed at the same time.

Because they are at the same distance from us, their apparent relative brightnesses are the same

as their absolute relative brightnesses. The one main di erence between the stars will b e their

masses. Stars are gaseous balls, and would collapse under their own self gravity,ifitwere not for

the outward pressure from the hot interior gases where the thermonuclear reactions are taking

place. The more massive stars burn their fuel faster, in order to keep high enough pressure to

counteract gravity. We learned in the lecture on light and radiation that hotter stars are also

bluer stars. If we plot a diagram of temp erature or color versus the brightness of a star in a

cluster, we will see that the stars do not fall randomly on the plot. We can use this typ e of plot,

called a Hetzspring-Russell diagram, to determine the age of the cluster of stars. This typ e

of plot was rst develop ed indep endently in 1911-1913 by E. Hertzsprung and H. N. Russell.

Figure 4: Schematic HR Diagram. The diagonal line of stars is called the main sequence, where

stable H-fusion o ccurs.

As a star runs out of fuel in its core, it b egins to collapse and will eventually heat up enough

to start the fusion of He. At the end of the H-burning stage, the star moves o the Main

Sequence. Also, prior to the b eginning of H-burning, while the star is still forming, it will move 5

toward the main sequence as the core heats up. Star clusters will have stars of di erent masses,

hence stars at di erent stages of evolution, and by making a HR diagram, we can estimate the

age of the cluster.

Figure 5: Schematic HR Diagram for clusters of ages 1 million , 100 million years and a

globular cluster 10-16 billion years old.

Table 2: Candidate Op en Clusters

0

Name Constell 2000  2000 Mag Size [ ] 7UT 8UT 9UT

NGC 6231 Sco 16:54.0 {41:48 2.6 14 2.6/23 2.1/28 1.9/31

M6 Sco 17:40.4 {32:14 4.2 33 2.4/25 1.8/34 1.6/40

NGC 6475 Sco 17:53.9 {34:49 2.4/24 1.8/33 1.6/40

4.4 Standard Stars

While we can accurately measure the brightness of celestial ob jects with our photometer, to b e

useful scienti cally,we have to put our measurements on a standard scale. Not all devices will

pro duce the same C for the same ob jects b ecause of di erences in quantum eciency of the

detector, etc. In order to put things into a standard scale, we measure stars of known brightness,

called standars. Below are some stars we will use as standards.

Note: Some of the \Standard" stars are actually listed as variables!. These are ok for our

pro ject since the magnitude of variation is so small that we will not detect it  Leo: V =

0.07 mag; Vir: V = 0.05 mag.

4.5 Pro cedure

Follow the pro cedure outlined b elow to obtain calibrated data on your ob ject.

 Set up telescop e, and align the nder

 As so on as Polaris is visible, p olar align the telescop e 6

Table 3: Standard Stars

Cat  Name Name2 Sp ec 2000  2000 V R Comment

3982 Leo Regulus B8V 10:08:22 +11:58:02 1.36 1.38 Var?

4033  UMa HD89021 A2IV 10:17:06 +42:54:52 3.45 {

4534 Leo HD102647 A3V 11:49:04 +14:34:19 2.14 2.08 Var  Scuti

4983 43 Com 13:11:52 +27:52:41 4.26 3.77

4662 Crv HD106625 B8III 12:15:48 {17:32:31 2.60 2.64 Var

5072 70 Vir HD117176 G5V 13:28:26 +13:46:44 4.98 {

5056 Vir Spica B1V 13:25:12 {11:09:41 0.96 { Var

SA 92-336 13:45:21 +00:47:23 8.05 7.53

5340 16 Bo o 14:15:40 +19:10:56 -0.05 -1.04

6175 13 Oph 16:37:09 {10:34:01 2.56 2.46

 Find one of the bright stars in the standards list using a nding chart Norton's and set

the telescop e setting circles and turn on tracking

 mount the photometer, and nd your ob ject and center in the photometry ap erture and

fo cus the telescop e.

 Take 10 sets of measurements of the standard star you select and record the time Universal

Time, UT { which is the time in Greenwich = HST + 10 hr. Each measurement will b e

a reading of the count rate of the star, followed by a measurement of the blank sky next

to the star. Be sure to note the exp osure time and gain for b oth on logsheets provided.

 Go to your program ob ject and do a set of measurements.

 Try to get at least 3 measurements of your standard star at di erent times - i.e. telescop e

p ositions at di erent elevations a low and high elevation. The standard star will b e used

to measure the amount of atmospheric extinction.

 If you are observing a cluster, you must get observations in two lters.

5 Data Reduction

5.1 Means and Errors

If we make a measurement of the brightness of a star, we exp ect our measurement will be

approximately equal to its brightness, but not exactly equal. Because of random errors, if we

make a second measurement, it will be di erent from the rst, but also approximately equal

to the brightness of the star. With a large number of observations, we exp ect that on average

the measurements will be distributed around the correct value. The standard deviation is a

measure of howmuch scatter there is in the data, and gives us an estimate of howwell we know

the numb er. The formal de titions of mean and standard deviation,  , are: 7

X

1

x = x 2

i

N

X

1

2 2

 = x x  3

i

N 1

where N is the number of data p oints.

5.1.1 Spherical Trigonometry

When we are considering co ordinate systems in the night sky, on the celestial sphere, we need

to explore a new mathematical area called spherical trigonometry, b ecause we are dealing with

angles on a spherical surface. A spherical triangle is the intersection of 3 arcs. If the sides of a

spherical triangle are lab eled a, b, and c, and the opp osite angles A, B , and C , then we have 2

imp ortant rules which are relevantto astronomical co ordinate systems: the law of sines:

sins  sinc sins 

2 1

= = 4

sinA  sinA  sinA 

1 2 3

and the law of cosines:

coss  = coss  coss  + sins  sins  cosA  5

1 2 3 2 3 1

Figure 6: Spherical Traingle.

5.2 Calculating Airmass

The starlight that reaches our telescop e has passed through the Earth's atmosphere, and as

it do es so some of the light is lost due to scattering and absorbtion. The more atmosphere it

passes through, the more lightis lost. When a star is at our zenith, or on the meridian, it will

pass through the least amount of atmosphere, but on the horizon it will pass through more

atmosphere, and more light is lost. If we are going to make precise measurements of stellar

brightness, we need to correct for the amount of light which is lost, and this will dep end up on

where in the sky the star is. The measure of howmuch atmosphere the light is passing through

is called the airmass, . Airmass is given by the following formula:

1

= sec z  = [sin sin  + coscos  cosHA] 6

Here,  is the latitude of the observing site,  is the of the ob ject and HA is the

hour angle of the ob ject. This formula derives from the law of cosines in spherical trigonometry. 8

5.2.1 Hour Angle and Sidereal Time

The rst step to computing howmuch atmosphere the starlight has passed through is to calculate

what is called the hour angle, HA. The observer's meridian is an imaginary great circle passing

through the zenith p oint directly overhead and the North Celestial Pole NCP. The star will

b e at it's highest elevation ab ove the horizon when it crosses the meridian. The HA is an angular

measure from the intersection of the celestial meridian and the celestial equator westward along

the celestial equator. The units of measure are in hours rather than degrees. There are 24 hours



in a circle of 360 . For example, for an ob ject on the celestial meridian, HA=0. For an ob ject

on the W horizon HA=6 and on the E horizon HA=-6. We don't have to measure this angle,

we can calculate it.

HA = ST 7

where is the of the ob ject and ST is the sidereal time.

Greenwich mean time is regulated by the motion of the Sun. One solar day is the time

between two successive passages of the sun overhead. However, during the day the sun is

moving along its around the sun, so to reach the same place in the sky, the earth has to

rotate a little bit farther than 1 full rotation. Another typ e of day is called the sidereal day, and

this is the time b etween two successive passages of a star overhead. The solar day is 24 hours,

h m

but the sidereal day will be slightly shorter, 23 56 . This is why the stars rise 4 min earlier

each day. There are ab out 365.25 solar dyas in a , and during this time the Earth makes

366.25 rotations ab out its axis. Greenwich mean time nad Greenwich sidereal time agree at one

instantevery year at the autumnal equinox 9/22. The formal de nition of Sidereal time, ST,

is that it is the Hour Angle of the Vernal Equinox. Attached to the back of the lab is a table of

sidereal times for Greenwich England at 0UT on each day for the TOPS workshop.

5.3 Extinction Co ecients { Least Squares Fits

For small to mo derate airmasses, there is a simple linear relationship b etween the brightness or

m of an ob ject and its airmass. If you plot mag versus airmss, the slop e

obs

of the line will equal the extinction co ecient, k :

m = m k 8

i obs

Because of random errors, all the p oints won't fall exactly on a straight line. Ideally wewant

to have the b est straight line that represents the data. This is computed by computing the sum

of the di erences b etween the t line and the data and minimizing this. This technique is called

least squares tting. This is easy to do with a computer, but tedious with a calculator, so

for the lab, we could just plot things on graph pap er by hand and do an \eyeball" t. If you

are interested, the equations for tting a set of data, x, y ,   for the slop e, k and intercept b

are:

 !

X X X X

1 x y x y 1

i i i i

9 k =

2 2 2 2

    

i i i i

 !

2

X X X X

1 x y x x y

i i i i

i

b = 10

2 2 2 2

    

i i i i 9

where

! 

2

2

X X X

1 x x

i

i

= 11

2 2 2

  

i i i

5.4 Color Terms and Zero Points

Finally, the last step in our data reduction is to take account of the fact that our instrument

do es not give us a calibrated numb er. We use the standard star measurements to convert our

instrumental magnitudes, m to a true magnitude. The true magnitude is given by:

i

m = m k + V R+z 12

i

Here  is called the color term and z is a calibration zero p oint. If we rearrange this equation

to:

y = m m + k = V R+z 13

i

we see that this is just the equation of a straight line with a slop e of  and intercept z for

x-values of \V-R". We know the colors and magnitudes of our standard stars, so we plot them

and do another t to get  and z , our zero p oint. Once we know k , , and z we can plug these

into our equation ab ove to compute the true magnitudes from our instrumental magnitudes for

our ob jects of unknown brightness.

At this p oint, for variable stars, we will plot magnitude versus time, and for the clusters we

will plot magnitude versus color as our nal data pro duct.

6 Follow-up and Further work

If you would like to go the HOA sessions during rotation later you can use this software to help

analyze the data.

If you are really interested in pursuing this for your scho ol, the photo electric photometer is

available from Optec, Inc., 199 Smith Street, Lowell, MI, 49331, 616 897-9351, FAX: 616

897-8229, http://www.optecinc.com/. At the TOPS workshop, you used the SSP-3, which costs

$895.00  lters and carrying case are extra.

There are several go o d guide on how to do photometry for amateurs:

 Photoelectric Photometry of Variable Stars { A Practical Guide for the Smal ler Observa-

tory 2nd Ed., Ed. by Hall and Genet available from Willman Bell, Inc.,

http://www.willb ell.com/photo/photo3.htm, $24.95.

 Astronomical Photometry, Henden & Kaitchuck, $24.95.

 Software for Photometric Astornomy, Henden & Kaitchuck, $69.95.

There are numerous organizations where your data might be sent to make a real scienti c

contribution. The AAVSO http://www.aavso.org/ab out/ collects amateur photometry on

variable stars for use by professional astronomers. 10