Physical Science (12th Edition), Standalone Book
12th Edition
ISBN: 9781260150544
Author: Bill W. Tillery
Publisher: McGraw Hill Education
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Chapter 17, Problem 11QFT
What is meant by the “texture" of an igneous rock? What does the texture of an igneous rock tell you about its cooling history?
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A cylinder with a piston contains 0.153 mol of
nitrogen at a pressure of 1.83×105 Pa and a
temperature of 290 K. The nitrogen may be
treated as an ideal gas. The gas is first compressed
isobarically to half its original volume. It then
expands adiabatically back to its original volume,
and finally it is heated isochorically to its original
pressure.
Part A
Compute the temperature at the beginning of the adiabatic expansion.
Express your answer in kelvins.
ΕΠΙ ΑΣΦ
T₁ =
?
K
Submit
Request Answer
Part B
Compute the temperature at the end of the adiabatic expansion.
Express your answer in kelvins.
Π ΑΣΦ
T₂ =
Submit
Request Answer
Part C
Compute the minimum pressure.
Express your answer in pascals.
ΕΠΙ ΑΣΦ
P =
Submit
Request Answer
?
?
K
Pa
Learning Goal:
To understand the meaning and the basic applications of
pV diagrams for an ideal gas.
As you know, the parameters of an ideal gas are
described by the equation
pV = nRT,
where p is the pressure of the gas, V is the volume of
the gas, n is the number of moles, R is the universal gas
constant, and T is the absolute temperature of the gas. It
follows that, for a portion of an ideal gas,
pV
= constant.
Τ
One can see that, if the amount of gas remains constant,
it is impossible to change just one parameter of the gas:
At least one more parameter would also change. For
instance, if the pressure of the gas is changed, we can
be sure that either the volume or the temperature of the
gas (or, maybe, both!) would also change.
To explore these changes, it is often convenient to draw a
graph showing one parameter as a function of the other.
Although there are many choices of axes, the most
common one is a plot of pressure as a function of
volume: a pV diagram.
In this problem, you…
Learning Goal:
To understand the meaning and the basic applications of
pV diagrams for an ideal gas.
As you know, the parameters of an ideal gas are
described by the equation
pV = nRT,
where p is the pressure of the gas, V is the volume of
the gas, n is the number of moles, R is the universal gas
constant, and T is the absolute temperature of the gas. It
follows that, for a portion of an ideal gas,
pV
= constant.
T
One can see that, if the amount of gas remains constant,
it is impossible to change just one parameter of the gas:
At least one more parameter would also change. For
instance, if the pressure of the gas is changed, we can
be sure that either the volume or the temperature of the
gas (or, maybe, both!) would also change.
To explore these changes, it is often convenient to draw a
graph showing one parameter as a function of the other.
Although there are many choices of axes, the most
common one is a plot of pressure as a function of
volume: a pV diagram.
In this problem, you…
Chapter 17 Solutions
Physical Science (12th Edition), Standalone Book
Ch. 17 - 1. A naturally occurring inorganic solid element...Ch. 17 - 2. A structural unit that is repeated in three...Ch. 17 - 3. Which element is the most abundant in Earth’s...Ch. 17 - 4. Minerals are classified as
a. silicates.
b....Ch. 17 - 5. The most abundant class of nonsilicates is...Ch. 17 - 6. Silicates are classified into two groups based...Ch. 17 - 7. The color of a mineral when it is finely...Ch. 17 - 8. The hardness of a mineral is rated using the
a....Ch. 17 - 9. The ratio of the mineral’s density to the...Ch. 17 -
10. Molten rock material from which minerals...
Ch. 17 -
11. An aggregation of one or more minerals that...Ch. 17 -
12. Rocks that are formed from molten minerals...Ch. 17 -
13. Igneous rock that slowly cooled deep below...Ch. 17 -
14. The rock that makes up the bulk of Earth’s...Ch. 17 -
15. The rock that makes up the ocean basins and...Ch. 17 -
16. Rocks that are formed from particles of other...Ch. 17 - 17. Accumulations of silt, sand, or other...Ch. 17 - 18. Limestone and dolomite are
a. sandstone.
b....Ch. 17 - 19. Heat and pressure change rocks into
a.igneous...Ch. 17 - 20. The relationship between rocks that are...Ch. 17 - 21. The thin layer that covers Earth’s surface is...Ch. 17 - 22. Based on its abundance in Earth's crust, most...Ch. 17 - 23. The most common rock in Earth's crust is
a....Ch. 17 - 24. An intrusive igneous rock will have which type...Ch. 17 - 25. Which igneous rock would have the greatest...Ch. 17 - 26. Which of the following formed from previously...Ch. 17 - 27. Sedimentary rocks are formed by the processes...Ch. 17 - 28. The greatest extent of metamorphic changes has...Ch. 17 - 29. Which type of rock probably existed first,...Ch. 17 - 30. Earth is unique because it has
a. CO2 in its...Ch. 17 - 31. The common structural feature of all silicates...Ch. 17 - 32. The one group that is not a subgroup of the...Ch. 17 - 33. The property that is not considered useful in...Ch. 17 - 34. The specific gravity of a mineral depends on...Ch. 17 - 35. Fluorite is a mineral that floats in liquid...Ch. 17 - 36. The group that is not a class of rocks is
a....Ch. 17 - 37. The classification of rocks is based on
a....Ch. 17 - 38. An example of a sedimentary rock is
a....Ch. 17 - 39. The term that does not describe a size of...Ch. 17 - 40. Dissolved rock materials form
a. chemical...Ch. 17 - 41. An example of a metamorphic rock is
a....Ch. 17 - 42. Extrusive igneous rocks are formed on Earth’s...Ch. 17 - 43. Foliation is found in
a. sedimentary rocks.
b....Ch. 17 - Prob. 1QFTCh. 17 - Prob. 2QFTCh. 17 - 3. Explain why each mineral has its own unique set...Ch. 17 - 4. Identify at least eight physical properties...Ch. 17 - 5. Explain how the identity of an unknown mineral...Ch. 17 - 6. What is a rock?
Ch. 17 - 7. Describe the concept of the rock cycle.
Ch. 17 - Prob. 8QFTCh. 17 - 9. Which major kind of rock, based on the way it...Ch. 17 -
10. What is the difference between magma and...Ch. 17 -
11. What is meant by the “texture" of an igneous...Ch. 17 -
12. What are the basic differences between...Ch. 17 -
13. Explain why a cooled and crystallized magma...Ch. 17 - Prob. 14QFTCh. 17 -
15. What are clastic sediments? How are they...Ch. 17 -
16. Briefly describe the rock-forming process...Ch. 17 - 17. What are metamorphic rocks? What limits the...Ch. 17 - 18. Describe what happens to the minerals as shale...Ch. 17 - Prob. 19QFTCh. 17 - 1. What are the significant similarities and...Ch. 17 - 2. Is ice a mineral? Describe reasons to support...Ch. 17 - 3. If ice is a mineral, is a glacier a rock?...Ch. 17 - Prob. 4FFACh. 17 - Prob. 1PEACh. 17 - Prob. 2PEACh. 17 - Prob. 3PEACh. 17 - Prob. 4PEACh. 17 - Prob. 5PEACh. 17 - Prob. 6PEACh. 17 - Prob. 7PEACh. 17 - Prob. 8PEACh. 17 - Prob. 9PEACh. 17 - Prob. 10PEACh. 17 - Prob. 11PEACh. 17 - Prob. 12PEACh. 17 - A granite countertop measuring 4.57 m long by 0.75...Ch. 17 - A limestone building stone measuring 40.0 cm long...Ch. 17 - Granite boulders with a minimum mass of 1.50...Ch. 17 - 1. A sample of the mineral sylvite measures 2.68...Ch. 17 - 2. A rectangular crystal of calcium plagioclase...Ch. 17 - 3. A spherical specimen of the mineral quartz...Ch. 17 - 4. Geologists separate nonferromagnesian silicates...Ch. 17 - 5. Compare the mineral halite (NaCl, hardness of...Ch. 17 - 6. Mica is a sheet silicate while quartz is a...Ch. 17 - 7. Magnesite is a magnesium ore mineral and has...Ch. 17 - 8. Magnetite and hematite are iron ore minerals....Ch. 17 - 9. An iron mine has an ore deposit estimated at...Ch. 17 - 10. An ore deposit consisting of chert and...Ch. 17 -
11. For a given igneous rock type, the proportion...Ch. 17 -
12. Based on Figure 17.13, what is the average...Ch. 17 -
13. A gabbro countertop measuring 4.70 m long by...Ch. 17 -
14. A sandstone building stone measuring 50.0 cm...Ch. 17 - Prob. 15PEB
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