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Nuts & Volts

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ties can drop to only a few meters and<br />

the dirt will sandblast astronaut’s<br />

visors. So to safely launch a balloon<br />

during a dust storm, astronauts will<br />

have to fill the balloon inside of a<br />

structure, like a shed. After they finish<br />

filling the balloon, they’ll carry it<br />

outside and release it. This is the same<br />

way the National Weather Service fills<br />

and launches their radiosondes.<br />

The Mars Pathfinder, which<br />

landed on Mars in July 1997, carried a<br />

set of wind socks on its ASI/MET<br />

mast. Pathfinder’s windsock data<br />

indicated that the Martian winds are<br />

at their strongest from morning to<br />

noon and weakest in the late<br />

afternoon and early evening.<br />

So it appears astronauts can fill<br />

and launch weather balloons on Mars.<br />

It will be easier if they wait until after<br />

noon local time to fill the balloon. But<br />

if they want to launch during a dust<br />

storm, they’ll need to use a filling shed.<br />

THE COMPOSITION<br />

OF THE MARTIAN<br />

ATMOSPHERE<br />

Let’s assume our astronauts want<br />

to launch a four pound (1,816 grams)<br />

payload and 6.6 pound (3,000 grams)<br />

weather balloon. Mars has a surface<br />

gravity that’s 38% of Earth’s gravity.<br />

Therefore, on Mars, the payload will<br />

only weigh 1.5 pounds and the balloon<br />

2.5 pounds. For our weather balloon to<br />

launch this payload, it must contain<br />

enough helium to displace at least four<br />

pounds of Martian atmosphere (the<br />

weight of the payload and balloon).<br />

Because gravity affects the weight<br />

of air and the payload alike, we won’t<br />

calculate weights on Mars, but just<br />

use mass. So in this case, the balloon<br />

must displace an atmospheric mass<br />

of at least 4,812 grams before the<br />

balloon can begin lifting the payload.<br />

An Avogadro’s number of gas molecules<br />

at standard temperature and<br />

pressure (STP) occupies a volume of<br />

22.4 liters and has a mass that is equal<br />

to the gas’ atomic weight. Did you get<br />

all of that I guess I should explain a<br />

few things about that sentence.<br />

Avogadro’s number is 6.022 x 10 23<br />

and it’s the number of molecules in one<br />

mole of any chemical. One mole of a<br />

chemical is an amount of that chemical<br />

that has a weight in grams that’s equal<br />

to its atomic mass. So one mole of<br />

hydrogen gas weighs two grams, occupies<br />

a volume of 22.4 liters at STP, and<br />

contains 6.022 x 10 23 molecules<br />

(remember that hydrogen gas is diatomic,<br />

or contains two hydrogen atoms).<br />

Standard temperature and pressure<br />

is a temperature of 0 degrees C<br />

(or 273 Kelvins) and a pressure of one<br />

atmosphere (1,013 mb). A Kelvin is<br />

equal to a degree Celsius. The only<br />

difference between them is that the<br />

Kelvin temperature scale begins at<br />

-273 degrees Celsius, or the temperature<br />

of absolute zero, while the<br />

Celsius scale begins at the freezing<br />

point of pure water. The Kelvin temperature<br />

scale doesn’t use the word<br />

“degrees” like Fahrenheit or Celsius.<br />

So please say the temperature is 273<br />

Kelvins and not 273 degrees Kelvin.<br />

The Martian atmosphere is 95%<br />

CO 2 , 3% N 2 , and 2% is trace gases.<br />

We’ll treat the Martian atmosphere as<br />

if it were pure carbon dioxide since<br />

the nitrogen and other trace gases<br />

only affect the density of the Martian<br />

atmosphere by a small amount. Since<br />

the chemical formula of carbon dioxide<br />

is CO 2 , its atomic mass is equal to<br />

the atomic mass of one carbon atom<br />

plus two oxygen atoms. By ignoring<br />

isotopes, I calculate the mass of a carbon<br />

dioxide molecule to be (1 x 12) +<br />

(2 x 16), or 44 atomic mass units.<br />

So an atmosphere of pure carbon<br />

dioxide has a mass of 44 grams per<br />

22.4 liters at STP. Helium has a mass<br />

of four grams per 22.4 liters at STP, so<br />

22.4 liters of helium will displace 40<br />

grams of carbon dioxide at STP.<br />

However, the air temperature at the<br />

Martian surface is -14 degrees C (259<br />

K) and the pressure is seven millibars.<br />

So we must adjust the density of the<br />

carbon dioxide atmosphere on Mars.<br />

You probably learned in your high<br />

school chemistry class that decreasing<br />

the temperature of a fixed amount<br />

of gas causes it to contract in volume<br />

and that decreasing the air pressure<br />

acting on it causes it to expand in volume.<br />

The equation used to calculate<br />

the volume of a gas outside of STP is:<br />

V f = V i X (T f /273) X (1013/P f )<br />

where<br />

V f is the final volume<br />

V i is the initial volume<br />

T f is the final temperature<br />

P f is the final pressure<br />

NEAR SPACE<br />

Weather Balloon, $55. Tank of Helium, $100. Photograph of the Earth from Near Space, PRICELESS.<br />

March 2006 91

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