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An ideal gas, at initial temperature \(T_{1}\) and initial volume \(2.0\) \(\mathrm{m}^{3}\), is expanded adiabatically to a volume of \(4.0 \mathrm{~m}^{3}\), then expanded isothermally to a volume of \(10 \mathrm{~m}^{3}\), and then compressed adiabatically back to \(T_{1}\). What is its final volume?

Short Answer

Expert verified
The final volume is 2.0 m鲁.

Step by step solution

01

Understand the process sequence

The problem involves a sequence of transformations of an ideal gas. First, there is an adiabatic expansion from a volume of 2.0 m鲁 to 4.0 m鲁. Next, there is an isothermal expansion to a volume of 10.0 m鲁. Finally, the gas is adiabatically compressed back to its initial temperature, with the task being to find the final volume.
02

Apply adiabatic process formula

For an adiabatic process of an ideal gas, the relation between volume and temperature is given by \( TV^{\gamma - 1} = \text{constant} \), where \( \gamma = \frac{C_p}{C_v} \) . During the first adiabatic expansion from 2.0 m鲁 to 4.0 m鲁, the initial and final temperatures are related but not needed to solve the problem since the second adiabatic process will restore the gas to its initial temperature.
03

Examine the isothermal expansion

During an isothermal process, the temperature remains constant. The volume change from 4.0 m鲁 to 10.0 m鲁 occurs at this constant temperature, but it does not affect the adiabatic relations of initial and final states.
04

Apply adiabatic process on compression

In the final adiabatic compression, the gas returns to its initial temperature \( T_1 \). Use the adiabatic process formula again: since it returns to \( T_1 \), we have \( T_1 V_1^{\gamma - 1} = T_1 V_f^{\gamma - 1} \), simplifying to \( V_1^{\gamma - 1} = V_f^{\gamma - 1} \). Thus, the final volume \( V_f = 2.0 \text{ m}^3 \).

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Key Concepts

These are the key concepts you need to understand to accurately answer the question.

Ideal Gas Law
The Ideal Gas Law is a fundamental principle in thermodynamics that describes the behavior of an ideal gas - a theoretical gas composed of many randomly moving particles that perfectly follow Newton's laws of motion. The law is typically expressed as \( PV = nRT \), where:
  • \( P \) represents the pressure of the gas
  • \( V \) is the volume occupied by the gas
  • \( n \) is the number of moles of the gas
  • \( R \) is the universal gas constant, approximately \( 8.314 \) J路mol鈦宦孤稫鈦宦
  • \( T \) is the absolute temperature of the gas, measured in Kelvin
This formula allows us to predict how a gas will respond to changes in its environment, such as alterations in temperature or pressure. It is important to note that this law assumes ideal conditions where gases do not interact except through elastic collisions.
The Ideal Gas Law serves as a good approximation for many gases under a range of conditions although it does not perfectly describe real gases due to potential forces between molecules or varying molecular volume.
Isothermal Process
An isothermal process is a thermodynamic transformation that occurs at a constant temperature. During such transformations, the system exchanges heat with its surroundings to maintain the temperature, altering the pressure and volume unlike in other processes where temperature changes as well. For an ideal gas in an isothermal process, Boyle's Law applies which states that the product of pressure and volume is constant: \( PV = ext{constant} \).
Consider a gas expanding isothermally. As the gas expands and its volume increases, the pressure must decrease in order to satisfy the relation \( PV = ext{constant} \). This means that the pressure and volume are inversely related when temperature remains fixed.
  • The energy transferred as heat is equal to work done by or on the system since internal energy doesn't change (assuming ideal conditions).
In our exercise above, the gas undergoes an isothermal expansion from a volume of \(4.0\, ext{m}^3\) to \(10.0\, ext{m}^3\), where heat flow between the system and its environment is crucial to maintaining constant temperature.
Thermodynamics
Thermodynamics is the branch of physics that deals with heat, work, and temperature, and their relation to energy and physical properties of matter. It is founded on four laws that describe these relationships:
  • ***Zeroth Law***: If two systems are indistinguishable from a third system, they are also indistinguishable from each other in terms of temperature.
  • ***First Law***: Energy can be transformed from one form to another, but cannot be created or destroyed (conservation of energy).
  • ***Second Law***: Entropy of an isolated system always increases over time.
  • ***Third Law***: As temperature approaches absolute zero, the entropy of a system approaches a constant minimum.
Thermodynamics principles are used extensively when analyzing processes like those outlined in the exercise. The principles help understand how internal energy changes, how heat transfers, and how work is done, providing insight into whether certain processes are feasible or which pathway might be the most efficient. Well-versed understanding of these principles is essential for model predictions and analyzing physical systems, be they engineering processes, biological phenomena or natural occurrences.

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Most popular questions from this chapter

Suppose \(4.00\) mol of an ideal diatomic gas, with molecular rotation but not oscillation, experienced a temperature increase of \(60.0 \mathrm{~K}\) under constant-pressure conditions. What are (a) the energy transferred as heat \(Q,(\mathrm{~b})\) the change \(\Delta E_{\mathrm{int}}\) in internal energy of the gas, (c) the work \(W\) done by the gas, and (d) the change \(\Delta K\) in the total translational kinetic energy of the gas?

The normal airflow over the Rocky Mountains is west to east. The air loses much of its moisture content and is chilled as it climbs the western side of the mountains. When it descends on the eastern side, the increase in pressure toward lower altitudes causes the temperature to increase. The flow, then called a chinook wind, can rapidly raise the air temperature at the base of the mountains. Assume that the air pressure \(p\) depends on altitude \(y\) according to \(p=p_{0} \exp (-a y)\), where \(p_{0}=\) \(1.00 \mathrm{~atm}\) and \(a=1.16 \times 10^{-4} \mathrm{~m}^{-1}\). Also assume that the ratio of the molar specific heats is \(\gamma=\frac{4}{3}\). A parcel of air with an initial temperature of \(-5.00^{\circ} \mathrm{C}\) descends adiabatically from \(y_{1}=4267 \mathrm{~m}\) to \(y=1567 \mathrm{~m}\). What is its temperature at the end of the descent?

When \(1.0 \mathrm{~mol}\) of oxygen \(\left(\mathrm{O}_{2}\right)\) gas is heated at constant pressure starting at \(0^{\circ} \mathrm{C}\), how much energy must be added to the gas as heat to double its volume? (The molecules rotate but do not oscillate.)

During a compression at a constant pressure of \(250 \mathrm{~Pa}\), the volume of an ideal gas decreases from \(0.80 \mathrm{~m}^{3}\) to \(0.20 \mathrm{~m}^{3}\). The initial temperature is \(360 \mathrm{~K}\), and the gas loses \(210 \mathrm{~J}\) as heat. What are (a) the change in the internal energy of the gas and (b) the final temperature of the gas?

An ideal monatomic gas initially has a temperature of \(330 \mathrm{~K}\) and a pressure of \(6.00 \mathrm{~atm}\). It is to expand from volume \(500 \mathrm{~cm}^{3}\) to volume \(1500 \mathrm{~cm}^{3}\). If the expansion is isothermal, what are (a) the final pressure and (b) the work done by the gas? If, instead, the expansion is adiabatic, what are (c) the final pressure and (d) the work done by the gas?

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