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ll/tS/fcO

SATELLITE DRAG STUDY

G r a n t Number NSG 8 0 6 9
Final Report

F o r t he period 1 April 1979 to 3.1 July 1980
Principal Investigator
• J a c k W. Slowey

Prepared for
National Aeronautics and Space Administration
Marshall Space Flight Center, Alabama 35812

October 1980

Smithsonian Institution
Astrophysical Observatory
Cambridge, Massachusetts 02138

The S m i t h s o n i a n A s t r o p h y s i c a l O b s e r v a t o r y
and the Harvard College Observatory
a r e members o f t h e
Center for Astrophysics

The NASA T e c h n i c a l O f f i c e r f o r t h i s g r a n t i s D r . R . E . S m i t h , Code E S 8 1 ,
Space Science Laboratory, Marshall Space Flight Center, Marshall Space
Flight Center, Alabama 35812.

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�SATELLITE DRAG STUDY

G r a n t Number NSG 8069
F i n a l Report

For t h e p e r i o d 1 A p r i l 1979 t o 31 J u l y 1980
Principal Investigator
Jack W. Slowey

Prepared for
National A e r o n a u t i c s and Space A d m i n i s t r a t i o n
Marshall Space F l i g h t C e n t e r , Alabama 35812

O c t o b e r 1980

Smithsonian I n s t i t u t i o n
Astrophysical Observatory
Cambridge, M a s s a c h u s e t t s 02138

The S m i t h s o n i a n A s t r o p h y s i c a l O b s e r v a t o r y
and t h e Harvard C o l l e g e Observatory
a r e members o f t h e
Center for Astrophysics

The NASA Technical O f f i c e r f o r t h i s g r a n t i s Dr. R.E. S m i t h , Ctide ES81,
Space S c i e n c e L a b o r a t o r y , Marshall Space F l i g h t C e n t e r , Marshall Space
Flight Center, Alabama 35812.

��1.

Introduction

The Smithsonian Astrophysical Observatory (SAO), under a
grant from NASA (NSG8058), first began an analysis of the effects
of atmospheric drag on the Skylab satellite, 1973-27A, in the
fall of. 1977. Under that grant we determined, from orbital data
obtained from NORAD, the observed atmospheric drag on Skylab with
a resolution of 5 days or better in an interval that was
eventually to extend from March 1974 to the end of 1978.
At the
same time, we compared the observed drag with that predicted by
an atmospheric model and made numerous forecasts, based on
predicted solar and geomagnetic activity, of the orbital lifetime
of the satellite.
The current grant work at SAO is essentially a continuation
of the original grant work.
Under this grant we continued to
monitor the drag on Skylab and to make lifetime predictions up to
the time of final decay. These activities were described in some
detail in an earlier report and will not be covered again here.
We also continued to act as consultant to MSFC in matters
relating to our various atmospheric models and, in particular, to
the implementation at MSFC of our most recent (1977) model.
These activities have been conducted on a relatively informal
basis, by telephone and letter, and will not be described here.
We have also conducted a "post mortem" analysis to determine how
the techniques that we used on Skylab might be improved in the
future, especially with respect to the question of separating
possible variations in area-mass ratio from departures of the
atmospheric density from model values.
A short summary of this
work, together with some suggestions for future work, are given
in what follows.

2.

Technical Progress

We had hoped to utilize a second satellite in a comparative
analysis of atmospheric drag during the final portion of the
lifetime of Skylab.
The object was to see if the drag on a
second satellite
could
be
successfully
used
to
separate
variations in the observed drag on Skylab that might be due to
variations in the area-mass ratio from those that are due to
variations in atmospheric density. An atmospheric model alone is
not entirely adequate for this purpose since present models, as
good as they are in representing the large variations in density
that occur, are subject to appreciable systematic errors having
characteristic times of up to a month or more. These errors are
due mainly to failure of the decimetric solar flux to adequately
represent the variations in the solar EUV radiation that actually
heats the thermosphere and to similar inadequacy of the planetary
geomagnetic index as an indicator of the heating associated with
geomagnetic disturbance (and of present models of that very
complex phenomenon).
Except for short intervals in which

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�PAGE 2

geomagnetic disturbance may dominate, the densities determined
from drag on different satellites are generally quite consistent
among themselves. Thus it should be possible to infer density at
another location with greater accuracy from the drag on a
satellite of known area-mass ratio than is possible from any
model based on the usual geophysical parameters.
Of course, a
model would
still
be
required
to
provide
a
means
for
interpolating between the location of the probe satellite and the
desired location.
Unfortunately, the problems of data acquisition, program
development (mainly the conversion of several large programs to
run on a new computer), and processing proved to be too great to
carry out the projected analysis within the constraints of this
grant.
Instead, we made use of densities we had previously
obtained from the drag on the Explorer 32 satellite (1966-44A) to
make a comparison with the orbital accelerations of Skylab that
we had determined under the earlier grant (NSG 8058).
The
interval covered by this comparison was 265 days beginning in
late March, 1974.
The orbital acceleration (rates of change of the mean
motion) of Skylab that we determined from the available NORAD
orbits are plotted for this interval in Figure 1.
These were
obtained by drawing a smooth curve through the observed values of
the argument of latitude (M +w) and numerically differentiating
the curve using a 5-day time-step. In the same figure are shown
the corresponding accelerations determined by differentiation of
the results of numerical integration of the orbit using an
atmospheric model and, at the bottom, the ratios of the observed
accelerations to those computed from the orbit integration. The
model used in the integration was an updated version of Jacchia's
1970 model (Jacchia, 1970) and the assumed area-mass ratio was
0.0369 cm2/g. The drag coefficient was allowed- to vary around
the orbit, but the effective value was very close to 2.24
throughout the interval.
The relatively large short-term variations in the orbital
acceleration seen
in
Figure 1 are
due to variations
in
thermospheric heating by both solar EUV radiation and the
particle precipitation and/or ionospheric currents associated
with geomagnetic disturbance. In models, these two heat sources
are tied, in the first instance, to the 10.7-cm solar radio flux
and, in the second instance, to the Kp planetary geomagnetic
index.
In Figure 2, we have plotted 5-day means of both the
10.7-cm flux and the Kp geomagnetic index, on scales that are
roughly equal in terms or their expected effect on the exospheric
temperature of the atmosphere (the scale for Kp is slightly
exaggerated in this regard compared to that for *10#7). As can
be seen, the two indices are quite independent of each other and
may act either in unison or in opposition.

��PAGE 3

In Figure 4, we have plotted the exospheric temperature Tj
that results from . the 1970 model when only the short-term
variation in the 10.7-cm flux (the so-called "27 day" variation)
and the geomagnetic variation are taken into account.
These
temperatures were computed from
Tj = 665.2+1.8 (

P10#7 ~ 85.) +28 Kp+ 0.03 exp (Kp),

where F
Kpare the 5-day mean values from Figure 2.
We
7and
give them"here only to better illustrate the expected short-term
variations in density in the interval being studied.
Note that
these temperatures differ somewhat in detail from the computed
accelerations in Figure 1. This is because the values in Figure
1, as a result of the differentiation process, actually represent
means over a slightly longer interval than 5 days.
In comparing the observed acceleration of Skylab from Figure
1 with either the corresponding model values or the temperatures
of Figure 3, it will be noticed that several of the expected
sharp maxima or minima are missing in the observed values. It is
these points on the plot that result in the more prominent
"outlyers" in the ratio of observed to computed acceleration.
There is little doubt that some of th,ese apparent departures from
the model are, in fact, due mostly to errors in the observed
values resulting from the relatively crude method used to derive
them.
And, it follows that the scatter in the values of the
ratio is adversely effected generally for the same reason.
This
difficulty could, of course, be overcome by differentiating with
a considerably larger time step, but this would automatically
rule out the possibility of resolving shorter-term variations of
any kind.
In Figure 4 we have plotted 5—day means of atmospheric
densities obtained from analysis of the drag on the Explorer 32
satellite.
The densities are those at the effective height
(approximately 1/2 scale-height above
the
true height) of
perigee.
The average effective height in the interval plotted
was about 300 km.
These densities were obtained by direct
analysis of radar observations from selected sensors.
The
densities were originally determined with a general resolution of
1 day and a resolution of 0.5 day during larger geomagnetic
disturbances. The 5-day means plotted in the figure should have
a relative precision of close to 1%.
These densities confirm the accuracy of the model with
respect to 4 of the 5 worst values of the ratio in Figure 1. The
exception is the point at MJD 42205, where the minimum predicted
by the model and missing in the Skylab accelerations is also
missing in the densities determined from Explorer 32.
Other
differences in the Skylab accelerations are also confirmed as
being atmospheric in origin and not due to errors in the observed
values.

�V

�PAGE 4

At t h i s p o i n t we s h o u l d m e n t i o n t h a t our o l d e r a t m o s p h e r i c
models a r e n o t c u r r e n t l y o p e r a t i o n a l a t SAO due p r i m a r i l y t o a
change i n c o m p u t e r s .
I t was o u r i n t e n t i o n i n t h e p r e s e n t
analysis t o compute model v a l u e s f o r both S k y l a b and E x p l o r e r 32
using our most r e c e n t a t m o s p h e r i c model ( J a c c h i a , 1 9 7 7 ) , which i s
operational, and t o make a c o m p a r i s o n between t h e two s a t e l l i t e s
using the r a t i o s t o t h e s e v a l u e s . Much t o our s u r p r i s e , however,
the o r b i t a l a c c e l e r a t i o n s of S k y l a b computed w i t h t h e new model
did not agree i n d e t a i l w i t h t h e o b s e r v e d v a l u e s a s w e l l a s d i d
those from t h e o l d e r model n o r d i d t h e d e n s i t i e s computed f o r
Explorer 32 r e p r e s e n t t h e d e t a i l s of t h e o b s e r v e d v a l u e s a s w e l l
as i t was e x p e c t e d t h e y would.
I t i s n o t y e t known w h e t h e r t h i s a p p a r e n t d i f f i c u l t y w i t h
the new model i s i n t r i n s i c o r i s somehow due t o t h e way i t was
implemented i n t h e p a r t i c u l a r c i r c u m s t a n c e s .
The o n l y o t h e r
application of t h e model t h a t we have made i n a d r a g s i t u a t i o n
was during t h e f i n a l d e c a y of S k y l a b . I t seemed t o perform q u i t e
well in t h a t c a s e .
T h a t was h a r d l y a d e f i n i t i v e t e s t , however,
and i t may w e l l b e t h a t t h e most i m p o r t a n t r e s u l t of t h e p r e s e n t
analysis i s t h a t
it
revealed
a
major
difficulty in
the
model-related, a p p a r e n t l y ,
t o t h e "improved" model of
the
geomagnetic v a r i a t i o n t h a t i t i n c o r p o r a t e s .
When means of t h e computed d e n s i t i e s f o r E x p l o r e r 32 were
taken over 10-day i n t e r v a l s , t h e y were q u i t e smooth and d i d
reproduce most of t h e s y s t e m a t i c d e p a r t u r e s o b s e r v e d i n t h e
ratios for S k y l a b .
I n view of t h e d i f f i c u l t i e s w i t h t h e model,
we do not f e e l t h a t we a r e j u s t i f i e d i n p r e s e n t i n g t h o s e r e s u l t s
as proven f a c t , however.
We m u s t , a t l e a s t f o r t h e time b e i n g ,
consider t h e a n a l y s i s t o have been " i n c o n c l u s i v e " .

3.

Conclusions and Recommendations

an
Our e x p e r i e n c e w i t h S k y l a b d e m o n s t r a t e d t h e need
automated p r o c e d u r e f o r t h e h i g h - r e s o l u t i o n d e t e r m i n a t i o n of
densities from s a t e l l i t e d r a g .
For r e a s o n s of e f f i c i e n c y ,
should be an a n a l y t i c p r o c e d u r e a n d , l i k e t h e program t h a t
previously e x i s t e d a t SAO, s h o u l d be based on d i r e c t a n a l y s i s of
the individual o b s e r v a t i o n s of t h e p a r t i c u l a r s a t e l l i t e i n o r d e r
to yield t h e g r e a t e s t p o s s i b l e p r e c i s i o n and t i m e r e s o l u t i o n . As
a p r a c t i c a l m a t t e r , i t s h o u l d b e f u l l y a u t o m a t i c and f r e e of
reliance on hand methods of any k i n d .
I t would be e x t r e m e l y
valuable i n a v a r i e t y of programs i n o r b i t a l dynamics, such a s
the s t u d i e s we made of t h e d r a g on S k y l a b and t h e kind of
comparative a n a l y s i s we s u g g e s t i s f e a s i b l e i n t h e c a s e of
s a t e l l i t e s w i t h unknown o r v a r y i n g a r e a - m a s s r a t i o s , and a s a
research t o o l
that
could contribute
significantly
to the
improvement of models of t h e t h e r m o s p h e r e and e x o s p h e r e .
We
recommend t h a t MSFC s e r i o u s l y c o n s i d e r t h e development of such a
program.

�'

�PAGE 5
We would a l s o recommend t h a t c o n s i d e r a t i o n be g i v e n t o t h e
possibility of u t i l i z i n g t h i s program i n a p r o j e c t t o monitor a
small number of s a t e l l i t e s on a c o n t i n u o u s b a s i s .
No d e n s i t i e s
from s a t e l l i t e d r a g have been d e t e r m i n e d i n any a p p r e c i a b l e
quantity s i n c e 1 9 7 4 .
T h e r e a r e , however, some problems i n
thermospheric s t r u c t u r e and model development t h a t would b e n e f i t
greatly from t h e a v a i l a b i l i t y of s u c h d e n s i t i e s . There i s s t r o n g
evidence i n measurements of s o l a r EUV i r r a d i a n c e , f o r example, of
major d i f f e r e n c e s between t h e c u r r e n t s o l a r c y c l e and t h e
previous one ( H i n t e r e g g e r , 197 9 ) .
Our a n a l y s i s of S k y l a b
revealed t h a t t h e r e s p o n s e of t h e a t m o s p h e r e r e l a t i v e t o t h e
decimetric f l u x was n o t g r e a t l y d i f f e r e n t i n t h e two c y c l e s . The
exact nature of what d i f f e r e n c e may e x i s t remains t o be s e e n ,
however, and i t would seem t h a t d r a g a n a l y s i s o f f e r s t h e o n l y
means by which i t can be a c c u r a t e l y d e t e r m i n e d .
Densities
determined from d r a g h a v e t h e a d v a n t a g e of c o n t i n u i t y ( t h e d r a g
record extends back t o 1958) and freedom from t h e problems of
cross-calibration
between
experiments
that
is
lacking
in
densities
determined
by
mass-spectrometers
and
other
satellite-borne i n s t r u m e n t s .

�•

�PAGE 6

References

Hinteregger, H.E.
1979 Development of s o l a r c y c l e 21 o b s e r v e d i n EUV spectrum and
J.
Geophys.
R e s . , 84, pp
atmospheric a b s o r p t i o n s .
1933-1938.
Jacchia, L.G.
1970 New s t a t i c models of t h e t h e r m o s p h e r e and e x o s p h e r e w i t h
empirical t e m p e r a t u r e p r o f i l e s .
Smithsonian Astrophys.
Obs. Spec. R p t .
No. . 3 1 3 , 87 p p .
1977 Therraospheric t e m p e r a t u r e , d e n s i t y , and c o m p o s i t i o n :
models.
Smithsonian Astrophys.
Obs.
Spec.
Rpt.
375, 106 p p .

new
No.

��PAGE 7
These captions pertain to the following figures (1-4).
Figure 1.

Observed orbital acceleration
of
Skylab
(top),
acceleration
computed
from an atmospheric model
(middle), and
ratio
of
observed
to
computed
acceleration (bottom).

Figure 2.

5-day means of 10.7 cm solar
Kpgeomagnetic index (bottom).

Figure 3.

Exospheric temperature computed for just
variation and the geomagnetic variation.

the

27-day

Figure 4.

5-day means of observed densities at effective
for the Explorer 32 satellite.

height

flux

(top)

and

��PAGE 8

42125

. MJD

42225

42325

1974
Figure 1

��PAGE 9

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&lt;p&gt;Perhaps the Saturn V’s greatest claim to fame is the Apollo Program, specifically Apollo 11. Several manned and unmanned missions that tested the rocket preceded the Apollo 11 launch. Apollo 11 was the United States’ ultimate victory in the space race with the Soviet Union; the spacecraft successfully landed on the moon, and its crew members were the first men in history to set foot on Earth’s rocky satellite.&lt;/p&gt;
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                  <text>&lt;p&gt;The Saturn V was a three-stage launch vehicle and the rocket that put man on the moon. (Detailed information about the Saturn V's three stages may be found&lt;span&gt; &lt;/span&gt;&lt;a href="https://www.nasa.gov/centers/johnson/rocketpark/saturn_v_first_stage.html"&gt;here,&lt;span&gt; &lt;/span&gt;&lt;/a&gt;&lt;a href="https://www.nasa.gov/centers/johnson/rocketpark/saturn_v_second_stage.html"&gt;here,&lt;span&gt; &lt;/span&gt;&lt;/a&gt;and&lt;span&gt; &lt;/span&gt;&lt;a href="https://www.nasa.gov/centers/johnson/rocketpark/saturn_v_third_stage.html"&gt;here.&lt;/a&gt;) Wernher von Braun led the Saturn V team, serving as chief architect for the rocket.&lt;/p&gt;
&lt;p&gt;Perhaps the Saturn V’s greatest claim to fame is the Apollo Program, specifically Apollo 11. Several manned and unmanned missions that tested the rocket preceded the Apollo 11 launch. Apollo 11 was the United States’ ultimate victory in the space race with the Soviet Union; the spacecraft successfully landed on the moon, and its crew members were the first men in history to set foot on Earth’s rocky satellite.&lt;/p&gt;
&lt;p&gt;A Saturn V rocket also put Skylab into orbit in 1973. A total of 15 Saturn Vs were built, but only 13 of those were used.&lt;/p&gt;</text>
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                  <text>&lt;p&gt;Werner Hans Sieber (March 27, 1912 to April 3, 1995) was a guided missiles expert during WWII (Wade). He received his education from Technical University, Hanover (Lundquist). Sieber was taken to the United States through Operation Paperclip, where he joined von Braun's Rocket Team. By 1960, [Sieber was the] “Head of Measuring Consoles and Instrumentation Division, NASA Marshall Space Flight Center, Test Division, NASA Marshall Space Flight Center" (Wade). “In the February 1969 MSFC Directory (five months before the first lunar landing) he is listed as Chief of the Test Instrumentation and Control Division of the Test Laboratory” (Lundquist).&lt;/p&gt;
&lt;p&gt;&lt;/p&gt;
&lt;p&gt;Sources:&lt;br /&gt;Lundquist, Charles. "Transplanted Rocket Pioneers," 2015.&lt;br /&gt;&lt;br /&gt;Wade, Mark. "Sieber, Werner." &lt;em&gt;Encyclopedia Astronautica&lt;/em&gt;, &lt;a href="http://www.astronautix.com/s/sieber.html"&gt;http://www.astronautix.com/s/sieber.html&lt;/a&gt;.&lt;/p&gt;</text>
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                  <text>&lt;p&gt;The Saturn V was a three-stage launch vehicle and the rocket that put man on the moon. (Detailed information about the Saturn V's three stages may be found&lt;span&gt; &lt;/span&gt;&lt;a href="https://www.nasa.gov/centers/johnson/rocketpark/saturn_v_first_stage.html"&gt;here,&lt;span&gt; &lt;/span&gt;&lt;/a&gt;&lt;a href="https://www.nasa.gov/centers/johnson/rocketpark/saturn_v_second_stage.html"&gt;here,&lt;span&gt; &lt;/span&gt;&lt;/a&gt;and&lt;span&gt; &lt;/span&gt;&lt;a href="https://www.nasa.gov/centers/johnson/rocketpark/saturn_v_third_stage.html"&gt;here.&lt;/a&gt;) Wernher von Braun led the Saturn V team, serving as chief architect for the rocket.&lt;/p&gt;
&lt;p&gt;Perhaps the Saturn V’s greatest claim to fame is the Apollo Program, specifically Apollo 11. Several manned and unmanned missions that tested the rocket preceded the Apollo 11 launch. Apollo 11 was the United States’ ultimate victory in the space race with the Soviet Union; the spacecraft successfully landed on the moon, and its crew members were the first men in history to set foot on Earth’s rocky satellite.&lt;/p&gt;
&lt;p&gt;A Saturn V rocket also put Skylab into orbit in 1973. A total of 15 Saturn Vs were built, but only 13 of those were used.&lt;/p&gt;</text>
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                  <text>&lt;p&gt;The Saturn V was a three-stage launch vehicle and the rocket that put man on the moon. (Detailed information about the Saturn V's three stages may be found&lt;span&gt; &lt;/span&gt;&lt;a href="https://www.nasa.gov/centers/johnson/rocketpark/saturn_v_first_stage.html"&gt;here,&lt;span&gt; &lt;/span&gt;&lt;/a&gt;&lt;a href="https://www.nasa.gov/centers/johnson/rocketpark/saturn_v_second_stage.html"&gt;here,&lt;span&gt; &lt;/span&gt;&lt;/a&gt;and&lt;span&gt; &lt;/span&gt;&lt;a href="https://www.nasa.gov/centers/johnson/rocketpark/saturn_v_third_stage.html"&gt;here.&lt;/a&gt;) Wernher von Braun led the Saturn V team, serving as chief architect for the rocket.&lt;/p&gt;
&lt;p&gt;Perhaps the Saturn V’s greatest claim to fame is the Apollo Program, specifically Apollo 11. Several manned and unmanned missions that tested the rocket preceded the Apollo 11 launch. Apollo 11 was the United States’ ultimate victory in the space race with the Soviet Union; the spacecraft successfully landed on the moon, and its crew members were the first men in history to set foot on Earth’s rocky satellite.&lt;/p&gt;
&lt;p&gt;A Saturn V rocket also put Skylab into orbit in 1973. A total of 15 Saturn Vs were built, but only 13 of those were used.&lt;/p&gt;</text>
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                <text>The Saturn I booster which is powered by a cluster of eight rocket engines has been successfully flown on four successive flights.  The early success of this large launch vehicle is a strong indication of the soundness of its base heating program. This paper summarizes the thinking that went into the design of our base configuration. Flight test results indicate that pressures, temperatures and heating rates were generally as expected.  New techniques have been investigated for generating design data.  It has been found experimentally that pressure and thermal fields establish themselves in one to three milliseconds and that data from the "short duration" technique compare favorably with "long duration" type tests. As a result, the new "short duration" technique has become the standard for generating design data for the Saturn vehicle.</text>
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                <text>Wilson, Homer B.</text>
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                <text>University of Alabama in Huntsville Archives, Special Collections, and Digital Initiatives, Huntsville, Alabama</text>
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                <text>This material may be protected under U. S. Copyright Law (Title 17, U.S. Code) which governs the making of photocopies or reproductions of copyrighted materials. You may use the digitized material for private study, scholarship, or research. Though the University of Alabama in Huntsville Archives and Special Collections has physical ownership of the material in its collections, in some cases we may not own the copyright to the material. It is the patron's obligation to determine and satisfy copyright restrictions when publishing or otherwise distributing materials found in our collections.</text>
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                  <text>&lt;p&gt;The Saturn V was a three-stage launch vehicle and the rocket that put man on the moon. (Detailed information about the Saturn V's three stages may be found&lt;span&gt; &lt;/span&gt;&lt;a href="https://www.nasa.gov/centers/johnson/rocketpark/saturn_v_first_stage.html"&gt;here,&lt;span&gt; &lt;/span&gt;&lt;/a&gt;&lt;a href="https://www.nasa.gov/centers/johnson/rocketpark/saturn_v_second_stage.html"&gt;here,&lt;span&gt; &lt;/span&gt;&lt;/a&gt;and&lt;span&gt; &lt;/span&gt;&lt;a href="https://www.nasa.gov/centers/johnson/rocketpark/saturn_v_third_stage.html"&gt;here.&lt;/a&gt;) Wernher von Braun led the Saturn V team, serving as chief architect for the rocket.&lt;/p&gt;
&lt;p&gt;Perhaps the Saturn V’s greatest claim to fame is the Apollo Program, specifically Apollo 11. Several manned and unmanned missions that tested the rocket preceded the Apollo 11 launch. Apollo 11 was the United States’ ultimate victory in the space race with the Soviet Union; the spacecraft successfully landed on the moon, and its crew members were the first men in history to set foot on Earth’s rocky satellite.&lt;/p&gt;
&lt;p&gt;A Saturn V rocket also put Skylab into orbit in 1973. A total of 15 Saturn Vs were built, but only 13 of those were used.&lt;/p&gt;</text>
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                <text>The Saturn C-1 space vehicle system is being developed by government agencies at industrial firms under the direction of the National Aeronotics and Space Division</text>
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                <text>1965-10-01</text>
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          <element elementId="49">
            <name>Subject</name>
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                <text>Saturn project</text>
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                <text>Diagram</text>
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                <text>Launch vehicles</text>
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                <text>Instruction Manuals</text>
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          <element elementId="48">
            <name>Source</name>
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                <text>Saturn V Collection</text>
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              <elementText elementTextId="158954">
                <text>Box 28, Folder 14</text>
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                <text>University of Alabama in Huntsville Archives, Special Collections, and Digital Initiatives, Huntsville, Alabama</text>
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                <text>en</text>
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            <name>Rights</name>
            <description>Information about rights held in and over the resource</description>
            <elementTextContainer>
              <elementText elementTextId="158957">
                <text>This material may be protected under U. S. Copyright Law (Title 17, U.S. Code) which governs the making of photocopies or reproductions of copyrighted materials. You may use the digitized material for private study, scholarship, or research. Though the University of Alabama in Huntsville Archives and Special Collections has physical ownership of the material in its collections, in some cases we may not own the copyright to the material. It is the patron's obligation to determine and satisfy copyright restrictions when publishing or otherwise distributing materials found in our collections.</text>
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                <text>http://libarchstor.uah.edu:8081/repositories/2/archival_objects/17956</text>
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                  <text>Saturn V Collection</text>
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                  <text>&lt;a href="http://libarchstor.uah.edu:8081/repositories/2/resources/60" target="_blank" rel="noreferrer noopener"&gt;View the Saturn V Collection finding aid in ArchivesSpace&lt;/a&gt;</text>
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                  <text>Saturn V Collection</text>
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                  <text>&lt;p&gt;The Saturn V was a three-stage launch vehicle and the rocket that put man on the moon. (Detailed information about the Saturn V's three stages may be found&lt;span&gt; &lt;/span&gt;&lt;a href="https://www.nasa.gov/centers/johnson/rocketpark/saturn_v_first_stage.html"&gt;here,&lt;span&gt; &lt;/span&gt;&lt;/a&gt;&lt;a href="https://www.nasa.gov/centers/johnson/rocketpark/saturn_v_second_stage.html"&gt;here,&lt;span&gt; &lt;/span&gt;&lt;/a&gt;and&lt;span&gt; &lt;/span&gt;&lt;a href="https://www.nasa.gov/centers/johnson/rocketpark/saturn_v_third_stage.html"&gt;here.&lt;/a&gt;) Wernher von Braun led the Saturn V team, serving as chief architect for the rocket.&lt;/p&gt;
&lt;p&gt;Perhaps the Saturn V’s greatest claim to fame is the Apollo Program, specifically Apollo 11. Several manned and unmanned missions that tested the rocket preceded the Apollo 11 launch. Apollo 11 was the United States’ ultimate victory in the space race with the Soviet Union; the spacecraft successfully landed on the moon, and its crew members were the first men in history to set foot on Earth’s rocky satellite.&lt;/p&gt;
&lt;p&gt;A Saturn V rocket also put Skylab into orbit in 1973. A total of 15 Saturn Vs were built, but only 13 of those were used.&lt;/p&gt;</text>
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                <text>"Saturn history documentation: subject index."</text>
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            <name>Description</name>
            <description>An account of the resource</description>
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                <text>This document explains the handwritten numbers on each document.;  On spine is the title "Saturn history subject categories."</text>
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            <name>Temporal Coverage</name>
            <description>Temporal characteristics of the resource.</description>
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            <name>Subject</name>
            <description>The topic of the resource</description>
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                <text>Saturn project</text>
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                <text>History</text>
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                <text>Text</text>
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                <text>Indexs</text>
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            <name>Source</name>
            <description>A related resource from which the described resource is derived</description>
            <elementTextContainer>
              <elementText elementTextId="159004">
                <text>Saturn V Collection</text>
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              <elementText elementTextId="210313">
                <text>University of Alabama in Huntsville Archives, Special Collections, and Digital Initiatives, Huntsville, Alabama</text>
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            <name>Language</name>
            <description>A language of the resource</description>
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                <text>en</text>
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            <name>Rights</name>
            <description>Information about rights held in and over the resource</description>
            <elementTextContainer>
              <elementText elementTextId="159007">
                <text>This material may be protected under U. S. Copyright Law (Title 17, U.S. Code) which governs the making of photocopies or reproductions of copyrighted materials. You may use the digitized material for private study, scholarship, or research. Though the University of Alabama in Huntsville Archives and Special Collections has physical ownership of the material in its collections, in some cases we may not own the copyright to the material. It is the patron's obligation to determine and satisfy copyright restrictions when publishing or otherwise distributing materials found in our collections.</text>
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