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Lab 3 Marsorbit 2

1) Kepler used Tycho Brahe's astronomical data to determine that planets orbit the sun in ellipses, not circles as previously thought. 2) By observing Mars from Earth every 623 days, when Mars is in the same position in its orbit, Kepler was able to triangulate Mars' position and construct its elliptical orbit around the sun. 3) Applying Kepler's laws, the student constructed an elliptical orbit for Mars that demonstrated its eccentricity and that a line from the sun sweeps out equal areas in equal time intervals, as Mars orbits the sun.

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0% found this document useful (0 votes)
58 views4 pages

Lab 3 Marsorbit 2

1) Kepler used Tycho Brahe's astronomical data to determine that planets orbit the sun in ellipses, not circles as previously thought. 2) By observing Mars from Earth every 623 days, when Mars is in the same position in its orbit, Kepler was able to triangulate Mars' position and construct its elliptical orbit around the sun. 3) Applying Kepler's laws, the student constructed an elliptical orbit for Mars that demonstrated its eccentricity and that a line from the sun sweeps out equal areas in equal time intervals, as Mars orbits the sun.

Uploaded by

Zachary Blasczyk
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© © All Rights Reserved
We take content rights seriously. If you suspect this is your content, claim it here.
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Name

______________________________
Hour ___________
Back Ground: Back in 1609, Johannes Kepler did not have a computerized
planetarium that he could use to visualize the solar system at hatever instant he chose!
"hat he did have as an enormous #uantity o$ data inherited $rom %ycho Brahe, an
o&servational astronomer so care$ul and meticulous that his data can still &e used today
to locate astronomical o&'ects! %ycho had hoped that Kepler ould &e a&le to use his
data to prove mathematically the correctness o$ his on (eocentric cosmolo(y )a
complicated variation o$ *tolemy+s model,! "hat happened instead as that Kepler ent
here the data took him, and it asn+t in %ycho+s direction!
Kepler+s -irst .a states that planets or&it the sun, and the or&its are ellipses! "e
are (oin( to take a very small portion o$ data similar to hat as availa&le to Kepler, and
determine the or&it o$ /ars usin( the
method that he used!
Kepler as a&le to determine the
or&ital period o$ /ars )ith respect to the
stars,! He determined that /ars or&ited
the 0un once every appro1imately 623
days! %his is important since this tells us
that /ars ill &e at the same location in its
or&it every 623 days! "hy is this
important4 %ycho+s accurate data $or /ars
in the sky only provided direction &ut not
its distance! But one can trian(ulate the
position i$ one o&serves /ars in the same
position )623 days apart,!
Objectives:
5pply (eometric methods o$
trian(ulation
6se o&servational data to construct the
or&it o$
the planet /ars
7emonstrate Kepler+s -irst .a o$
*lanetary
/otion
.a&el and de8ne the properties o$ an
ellipse 5pply the properties o$ ellipses to
the or&it to
determine the eccentricity e o$ /ars+
or&it 9alculate the percent error in your
e1perimental
value o$ e
Procedure:
1) :et the lon(itudes $or mars o&served
positions
Fram
e
Date Longitude
A
/ar! ;1,19<1
B
-e&! =, 19<<
C
5pril ;0,
19<<
D
/ar! 2, 19<=
E
/ay ;6,
19<=
F
5pril 1;,
19<3
G
0ept! 16,
19<9

5u(! >, 19>1


!
Nov! ;;,
19>1
"
?ct! 11,
19><
#
Jan! ;1,
19>>
L
7ec! 9, 19>=
$
/ar! 19,
19>6
%
-e&! <, 19>2
O
5pril >, 19>2
P
-e&! ;1,
19=0
/ars ?r&it .a&
$rom the %ransparencies! @ound to the nearest
hal$A de(ree, and enter them in ta&le 1!
&) %ape $our sheets o$ paper to(ether at their ed(es to make one lar(e s#uare )or i$
availa&le (ra& one
lar(e s#uare sheet,! -ind the center and la&el it ith a dot to represent the sun!
') 9onstruct the or&it o$ the BarthC 0tart &y assumin( that the Barth+s or&it is circular(
use a compass to
dra a circle D a radius o$ 10cm to represent the or&it o$ earth around the sun!
)) Be(in on the ri(ht horizontal end o$ your circle and la&el that position 0E! /ark the
other $our points
o$ the a1is+ )these represent the e#uino1es and solstices, ith 90E, 120E, and ;30E
respectively (oin(
counter clockise!
*) *lot the si1teen Barth positions &y usin( their dates! 0ince there are almost the
same num&er o$ days
as there are de(rees, make one day one de(ree! Fou ill need to 8(ure out ho
many days there are
&eteen certain dates! )@emem&er -e&! G ;2 days! 5pr!, June, 0ept!, Nov! are all
<0 days! Jan!, /ar!,
/ay, July, 5u(!, ?ct!, 7ec! are all <1days!,
Bach data pair represents an o&servation o$ /ars, taken $rom here on Barth! Hn
each case, the o&servations are separated in time &y e1actly 623 days, or the
len(th o$ one /artian year! %hus, each pair o$ o&servations puts /ars in the same
place on its or&it relative to the sun! Hoever, that does not put it in the same
place relative to the Barth! %his is &ecause the Barth is also movin( ith respect to
the sun, and a$ter 623 days, the Barth is de8nitely not &ack in the same place it
started!
0o, to 8nd here /ars is ith respect to the
sun, e need to kno here the Barth is ith
respect to the sun, and then here /ars is ith
respect to the Barth! %he 8(ure illustrates thisC
%he heliocentric lon(itude o$ Barth is the
position o$ the Barth relative to the sun, and
the (eocentric lon(itude o$ /ars is the position
o$ /ars relative to the Barth!
+) -rom each pair o$ Barth positions there ill
&e
one /ars position! 5lays measure $rom
the east
)0E,! %he point o$ intersection o$ the to
lines
ill &e the position o$ /ars!
,) %o 8nd the areas that /ars seeps out &eteen positions, you need to 8nd the
avera(e radius o$ the
positions! %hen use that in the $olloin( $ormula to (et the amount o$ area per day
the or&it seeps
outC I J r
;
<60
Conc-usion .uestions:
1) 7oes your plot a(ree ith Kepler+s conclusion that the or&it is an ellipse4
&) "hat is the avera(e sunAtoA/ars distance in astronomical units )56,4
') 5s seen $rom the sun, hat is the direction )lon(itude, o$ /ars+ nearest and
$arthest positions4
)) 7urin( hat month is the Barth closest to the or&it o$ /ars4 "hat ould &e the
minimum separation &eteen the Barth and /ars4
*) "hat is the eccentricity o$ the or&it o$ /ars4
+) 7oes your plot o$ /ars+ or&it a(ree ith Kepler+s la o$ areas, hich states that a
line dran $rom the sun to the planet seeps out areas proportional to the time
intervals4 -rom tour or&it, you see that /ars as at point B+ on -e&ruary =, 19<<,
and point 9+ on 5pril ;0, 19<<! %here are ei(ht such pairs o$ dates in your data!
%he time intervals are diKerent $or each pair!
,) Ho much )&y hat percenta(e, do they vary4
/) "hat is the uncertainty in your area measurements4
0) Hs the uncertainty the same $or lar(e areas as small4
11) 7o your results &ear out Kepler+s la o$ areas4
ints 2or 3uestions:
1!
a, "hen determinin( the ma'or a1is, hich is the (reatest distance across the or&it,
the sun ill &e
at one o$ the $oci! %he second $oci is symetrically placed on the a1is! 9onstruct
the ellipse usin(
a piece o$ strin( e#ual to the len(th o$ the ma'or a1is!
&, 5lso anser #uestions 1 &y
determinin(
i$ *-
1
L *-
;
G constant! %ry this $or
to
diKerent points on the plot and
determine
the M diKerence!
;! @ememe&er that 156 on your plot is
10cm!
also @
ave
G aD;!
<! 0E is to the ri(ht!
>! :ive minimum separations in 56!
=! eGcDa
6A10!
a! %hese deal ith the .a o$ 5reas! 7etermine the areaDday values $or three
se(ments o$ the
plot $or #uestion 6 )See PPT).
&! M variation G .ar(est N smallest O
100M
5v(!
c! -or #uestion 10, (ive a 'usti8cation
$or
your anser!

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