Lab9AtmosphericRetentionCompletedCBuckland
pdf
keyboard_arrow_up
School
Sam Houston State University *
*We aren’t endorsed by this school
Course
1404
Subject
Astronomy
Date
Dec 6, 2023
Type
Pages
13
Uploaded by michelenrowe
Carissa Buckland
Your preview ends here
Eager to read complete document? Join bartleby learn and gain access to the full version
- Access to all documents
- Unlimited textbook solutions
- 24/7 expert homework help
Atmospheric Retention
9-5
PRE-LAB QUESTIONS
These questions must be answered before you show up to your lab class. You will not be able to start the lab exercise without the answers to these questions. A quiz based on these questions will be given at the beginning of the lab session. 1.
What is escape velocity?
Escape velocity is the lowest velocity a body must have in order to escape the
gravitational attraction of a planet, moon, star, or other celestial body.
2.
What is the escape velocity of Earth?
11.2 kilometers per second
3.
How is escape velocity related to the mass of a planet? to the radius of a planet?
Escape velocity depends on the mass and radius of a planet.
V
escape
=
√
2𝐺𝐺𝐺𝐺
𝑅𝑅
where G is Newton’s Gravitational Constant of 6.67x10
-11 Nm
2
/kg
2
, M is planetary mass, and R is planetary radius. 4.
What does the temperature of a gas represent?
The average kinetic energy of the particles in a gas is represented by the temperature.
5.
Do all particles in a gas move at the same speed? If not, what does the
distribution of speeds look like for a given temperature?
Not every molecule in a given gas moves at the same speed/temperature. Each gas
molecule has a slightly different kinetic energy. Because gases have the same
kinetic energy at the same temperature, lighter molecules will move faster, and
heavier molecules will move more slowly.
6.
What is the difference between the average speed, the most probable speed and
the rms speed of a gas particle?
Average speed is the average of all the magnitues of the individual moving gas
molecules.
Most probable speed is the speed that is being attained by the greatest amount of
moving gas molecules.
Rms speed is the square root of all the mean squared speed of all moving gas
particles. V
rms
=
√
3𝑘𝑘𝑘𝑘
𝑚𝑚
where T is temperature, m is mass of gas, and k is kinetic
energy.
7.
How do their values compare?
Probable speed is greater than average speed which is great than rms speed.
V
p
>
V
avg >
V
rms
8.
What fraction of particles will have a speed less than the average speed?
More than half of the particles
9.
How does the speed distribution of gas particles vary with temperature?
If the temperature increases, the speed distribution increases. If temperature decreases,
the speed distribution decreases.
Atmospheric Retention
9-6
10.
How does the speed distribution of gas particles vary with mass of the gas
particles?
The speed of distribution is directly proportional to the mass of the gas particles.
The greater the mass of the gas particles, the greater the value will be for the
speed distribution.
11.
Which planets have atmospheres?
Venus, Earth, Mars, Saturn, Jupiter, Uranus, and Neptune all have atmospheres.
Mercury is the only planet with no atmosphere.
12.
Which major moons have atmospheres?
Saturn’s Titan, Neptune’s Triton, and Jupiter’s Io are major moons that have
atmospheres.
Your preview ends here
Eager to read complete document? Join bartleby learn and gain access to the full version
- Access to all documents
- Unlimited textbook solutions
- 24/7 expert homework help
4.3
21.7
2.5
0.3
35.4
2651
2373
:11
Atmospheric Retention
9-9 The relationship between T (temperature) and the most probable velocity for escape is that as temperature is decreased, the most probable velocity decreases. As temperature increases, the most probable velocity increases as well. 3.
If the simulator allowed the temperature to be reduced to 0 K, what would you guess would be the most probable velocity at this temperature? Why?
I would wager to guess that at 0ºK, the most probable velocity would be zero, as well, because no energy would be emitted at that temperature. Return the temperature to 300 K. Use the gas panel to add Ammonia and Carbon Dioxide to the chamber.
4.
Complete the table using the draggable cursor to measure the most probable velocity at a temperature of 300 K and recording the atomic mass for each gas. Write a short description of the relationship between mass and Vmp
As mass increases, the width of the Maxwell distribution decreases and the most probable velocity decreases. in the chamber properties panel. You should still have an evenly balanced mixture of hydrogen, ammonia,
H
2 1500 17 549 44 333
Your preview ends here
Eager to read complete document? Join bartleby learn and gain access to the full version
- Access to all documents
- Unlimited textbook solutions
- 24/7 expert homework help
Atmospheric Retention
9-10 1
500
1500
H
2
is very quickly lost since it only has a mass of 2u and its most probable velocity is greater than the escape velocity, NH
3
is slowly lost since it is a medium mass gas (18u) and
a significant fraction of its velocity distribution is greater than 1500 mis, CO
2
is unaffected since its most probable
Hydrogen is lost very quickly due to its low mass, the ammonia is lost at a rate that is about half as quick as the hydrogen because of its medium mass, and the carbon dioxide is lost at a much slower rate. Both hydrogen and ammonia are completely lost before the carbon dioxide is even half-way depleted. Reducing the escape velocity allows for all three gases to escape the chamber at a relatively simultaneous rate. Carbon dioxide is moderately slower than ammonia and hydrogen, but is lost nonetheless. Only hydrogen is lost from the chamber, leaving both the ammonia and carbon dioxide present. Neither ammonia nor carbon dioxide are able to escape due to their most probable velocities being lower than 1500 m/s. Again, only hydrogen is lost from the chamber, leaving both the ammonia and carbon dioxide. Neither remaining gas can escape due to their most probable velocities being lower than 1000 m/s. Hyrdogen is rapidily lost, ammonia is slowly depleted, leaving carbon dioxide to slowly exit the chamber. Higher temperatures combined with lowered escape velocities resulted in a greater loss of gases at a higher rate. Lower temperatures and lowered escape velocities resulted in the standard loss of the low mass hydrogen gas, but much slower losses of the larger mass molecules. Gas is most likely to escape the chamber when temperatures are high and escape velocities are low. I Run I T (K) l
V
esc
Atmospheric Retention
9-11 GAS RETENTION PLOT
This simulator presents an interactive plot summarizing the interplay between escape velocities of large bodies in our solar system and the Maxwell distribution for common gases. The plot has velocity on the y-axis and temperature on the x-axis. Two types of plotting are possible: •
A point on the graph represents a large body with that particular escape velocity and outer atmosphere temperature. An active (red) point can be dragged or controlled with sliders. Realize that the escape velocity of a body depends on both the density (or mass) and the radius of an object. •
A line on the graph represents 10 times the average velocity (10 v
avg
) for a particular gas and its variation with temperature. This region is shaded with a unique color for each gas. o
If a body has an escape velocity v
esc
over 10 v
avg
of a gas, it will certainly retain that gas over time intervals on the order of the age of our solar system. o
If v
esc
is roughly 5 to 9 times v
avg
, the gas will be partially retained and the color fades into white over this parameter range. o
If v
esc
< 5 v
avg
, the gas will escape into space quickly. Begin experimenting with all boxes unchecked in both the gases and plot options. 7.
Plot the retention curves for the gases hydrogen, helium, ammonia, nitrogen, carbon dioxide, and xenon. Explain the appearance of these curves on the retention plot. The retention plots are very similar in appearance, with the speed (km/s) of the gases rising with an increase in temperature (K). Hydrogen has the lowest retention curve, meaning it escapes quickly from an atmosphere. Nitrogen and ammonia have very similar curves. Carbon dioxide has a higher retention curve than the three aforementioned gases. Xenon has the highest retention curve and also the highest mass of the gases. Check show gas giants in the plot options panel. 8.
Discuss the capability of our solar system's gas giants to retain particular gases among those shown. Gas giants are able to retain particular gases because of the high escape velocities that these planets have, and their speeds are greater than 10 x v
avg
.
Atmospheric Retention
9-12 9.
Drag the active point to the location (comparable with the escape speed and temperature) of Mercury. The gases hydrogen, helium, methane, ammonia, nitrogen, and carbon dioxide were common in the early solar system. Which of these gases would Mercury be able to retain? Mercury would be able to retain none of these gases because it falls below the retention curve of all of the aforementioned gases and has an extremely low escape velocity. 10.
Most nitrogen atoms have a mass of 14u (hence 28u for N2), but a small percentage of nitrogen atoms have an extra neutron and thus an atomic mass of 15u. (We refer to atoms of the same element but with different masses as isotopes of that element.) Recently, scientists studying isotope data from the Cassini spacecraft have noticed that the ratio of 15u nitrogen to 14u nitrogen is much larger than it is here on earth. Assuming that Titan and the earth originally had the same isotope ratios, explain why the ratios might be different today. The average velocity of a gas molecule is directly proportional to its temperature; that is, the higher the temperature, the higher the velocity; on the other hand, the average speed is inversely proportional to the molecule's atomic weight. Because Titan is much colder than Earth, gases move at a slower speed than they do here. If the planet's escape velocity is less than the average velocity of the gas, the gas will quickly escape from the atmosphere. Since Earth’s escape velocity is higher than Titan’s, both gases will be retained on Earth and lost on Titan, resulting in the different ratios of today. 11.
Other observations by the Cassini probe have confirmed that Titan has a thick atmosphere of nitrogen and methane with a density of about 10 times that of the Earth's atmosphere. Is this finding completely consistent with Titan's position on the atmospheric retention plot? Explain. (Make sure that show icy bodies and moons is checked as well as the gases methane and nitrogen.) According to the retention plot, Titan has a temperature of 90K with an escape velocity of 2.6 km/s. Titan would have a moderate escape velocity, meaning it would be able to retain nitrogen and methane. Titan’s thick atmosphere is consistent with its position on the atmospheric retention plot. Titan’s low temperatures and ice trap the gases in its atmosphere.
Your preview ends here
Eager to read complete document? Join bartleby learn and gain access to the full version
- Access to all documents
- Unlimited textbook solutions
- 24/7 expert homework help
Atmospheric Retention
9-13 POST-LAB QUESTIONS
1.
Earth and the Moon are located roughly the same distance away from the Sun, yet Earth has a permanent atmosphere while the Moon does not. Explain why.
The gravity of Earth is greater than that of the Moon. The Moon’s low surface gravity is unable to retain its atmosphere.
2.
Mercury and Mars have similar surface gravities, yet Mars has a permanent atmosphere while Mercury does not. Explain why. Mercury’s thin atmosphere is constantly blown away by the extreme temperature of the Sun and solar winds. 3.
Earth's primary atmosphere consisted of hydrogen and helium, yet today it is now mostly nitrogen with some oxygen. Why did Earth's atmospheric composition change over time? Planetary surface changes, temperature changes, and the introduction of photosynthetic plant life changed Earth’s atmospheric composition. 4.
Both Venus and Mars have atmospheres that are predominantly carbon dioxide while Earth only has trace amounts, even though it is gravitationally strong enough to hold on to it. How do we account for this difference? Earth’s large bodies of liquid water account for the difference in carbon dioxide concentrations.