/*! This file is auto-generated */ .wp-block-button__link{color:#fff;background-color:#32373c;border-radius:9999px;box-shadow:none;text-decoration:none;padding:calc(.667em + 2px) calc(1.333em + 2px);font-size:1.125em}.wp-block-file__button{background:#32373c;color:#fff;text-decoration:none} Problem 13 A U.S. penny has a diameter of \... [FREE SOLUTION] | 91Ó°ÊÓ

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A U.S. penny has a diameter of \(1.9000 \mathrm{~cm}\) at \(20.0^{\circ} \mathrm{C}\). The coin is made of a metal alloy (mostly zinc) for which the coefficient of linear expansion is \(2.6 \times 10^{-5} \mathrm{~K}^{-1}\). What would its diameter be on a hot day in Death Valley \(\left(48.0^{\circ} \mathrm{C}\right) ?\) On a cold night in the mountains of Greenland \(\left(-53^{\circ} \mathrm{C}\right) ?\)

Short Answer

Expert verified
The diameter of the penny in the Death Valley would be about 1.9014032 cm, and in the mountains of Greenland, it would be about 1.8964118 cm.

Step by step solution

01

Identify given dimensions

The initial diameter of the penny is given as \( L_{0} = 1.9 \, cm \). The coefficient of thermal expansion \( \alpha = 2.6 \times 10^{-5} 1/K \). The initial temperature is \( 20.0^{\circ}C \).
02

Calculate the new diameter at Death Valley

The change in temperature, \( \Delta T \), is the final temperature minus the initial temperature, \( \Delta T = T_{f} - T_{i} \). The final temperature at Death Valley is \( 48.0^{\circ}C \), hence the change in temperature is \( \Delta T = 48.0 - 20.0 = 28.0^{\circ}C \). Plug these values into the formula for change in dimension: \( \Delta L = L_{0} \alpha \Delta T = 1.9cm * 2.6 \times 10^{-5} 1/K * 28.0 K = 0.0014032 cm \). The new diameter is then \( L_{0} + \Delta L = 1.9000 cm + 0.0014032 cm = 1.9014032 cm \).
03

Calculate the new diameter in the mountains of Greenland

The final temperature in the mountains of Greenland is \( -53.0^{\circ}C \), so the change in temperature is \( \Delta T = -53.0 - 20.0 = -73.0^{\circ}C \). Plug these values into the formula for change in dimension: \( \Delta L = L_{0} \alpha \Delta T = 1.9 cm * 2.6 \times 10^{-5} 1/K * -73.0 K = -0.0035882 cm \). The new diameter is then \( L_{0} + \Delta L = 1.9000 cm - 0.0035882 cm = 1.8964118 cm \)

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Key Concepts

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

Linear Expansion Coefficient
The linear expansion coefficient is a crucial concept in understanding how materials respond to temperature changes. This small value, often represented by the symbol \( \alpha \), indicates how much a material will expand or contract for each degree change in temperature.

In our exercise, the penny's metal alloy has a linear expansion coefficient of \( 2.6 \times 10^{-5} \, \mathrm{K}^{-1} \). This number tells us that for every degree Kelvin (or Celsius, since the scale increment is the same), one meter of this material will expand by \( 2.6 \times 10^{-5} \) meters.
  • A higher linear expansion coefficient means the material expands more with temperature.
  • A lower coefficient indicates lesser expansion or contraction with temperature changes.
Having a solid grasp on this concept helps predict the dimensional changes of materials such as metals or any other substance when subjected to different thermal environments.
Understanding the linear expansion coefficient is essential in engineering and construction, where precise measurements are critical.
Temperature Change
Temperature change, denoted by \( \Delta T \), plays a significant role in the material's dimensional change.

In thermal expansion problems like ours, you would calculate \( \Delta T \) simply by subtracting the initial temperature from the final temperature.
For instance:
  • In Death Valley, the temperature change is \( 48.0^{\circ}\mathrm{C} - 20.0^{\circ}\mathrm{C} = 28.0^{\circ}\mathrm{C} \).
  • In the mountains of Greenland, it’s \( -53.0^{\circ}\mathrm{C} - 20.0^{\circ}\mathrm{C} = -73.0^{\circ}\mathrm{C} \).
Knowing \( \Delta T \) is crucial because it directly influences how much a material will expand or contract.
The larger the temperature change, the more pronounced the effect on the object's dimensions.
Accurately measuring and understanding these temperature differences is vital for predicting how objects behave in various thermal conditions.
Dimension Change Calculation
The dimension change calculation is where the principles of thermal expansion come to life.

To find the change in an object’s dimensions due to temperature variation, you utilize the formula:
\[ \Delta L = L_0 \alpha \Delta T \]
Where:
  • \( \Delta L \) is the change in length (in this case, the change in diameter).
  • \( L_0 \) is the original length or diameter of the object.
  • \( \alpha \) is the linear expansion coefficient.
  • \( \Delta T \) is the temperature change.
For example, in Death Valley, we calculated the new diameter with:
\( \Delta L = 1.9 \mathrm{cm} \times 2.6 \times 10^{-5} \, \mathrm{K}^{-1} \times 28.0^{\circ} \mathrm{C} = 0.0014032 \mathrm{cm} \).
  • Add \( \Delta L \) to the original diameter to get the new diameter.
  • Similarly, apply this formula to calculate the diameter in Greenland.
Such calculations are immensely useful in predicting and understanding how temperature variations affect the practical use of materials across different climates.
Thermal Physics
Thermal physics is a broad field that encompasses how energy, in the form of heat, affects matter.

It includes studying how objects expand when heated and contract when cooled, as well as various other heat-related phenomena.
Thermal expansion is just one aspect of this field and is particularly significant in areas where thermal stress or measurement precision is critical.
  • Understanding thermal physics helps in designing structures that can withstand temperature changes.
  • It is crucial for manufacturing processes, where metal precision is important.
  • It also aids in everyday objects, like ensuring that a bridge doesn't buckle or shrink excessively with seasonal changes.
By learning about concepts like thermal expansion, we can create more durable designs and predict how everyday materials behave under temperature variations.

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Most popular questions from this chapter

One suggested treatment for a person who has suffered a stroke is immersion in an ice-water bath at \(0^{\circ} \mathrm{C}\) to lower the body temperature, which prevents damage to the brain. In one set of tests, patients were cooled until their internal temperature reached \(32.0^{\circ} \mathrm{C}\). To treat a \(70.0 \mathrm{~kg}\) patient, what is the minimum amount of ice (at \(0^{\circ} \mathrm{C}\) ) you need in the bath so that its temperature remains at \(0^{\circ} \mathrm{C} ?\) The specific heat of the human body is \(3480 \mathrm{~J} / \mathrm{kg} \cdot \mathrm{C}^{\circ},\) and recall that normal body temperature is \(37.0^{\circ} \mathrm{C}\).

Consider a poor lost soul walking at \(5 \mathrm{~km} / \mathrm{h}\) on a hot day in the desert, wearing only a bathing suit. This person's skin temperature tends to rise due to four mechanisms: (i) energy is generated by metabolic reactions in the body at a rate of \(280 \mathrm{~W},\) and almost all of this energy is converted to heat that flows to the skin; (ii) heat is delivered to the skin by convection from the outside air at a rate equal to \(k^{\prime} A_{\mathrm{skin}}\left(T_{\mathrm{air}}-T_{\mathrm{skin}}\right),\) where \(k^{\prime}\) is \(54 \mathrm{~J} / \mathrm{h} \cdot \mathrm{C}^{\circ} \cdot \mathrm{m}^{2},\) the exposed skin area \(A_{\text {skin }}\) is \(1.5 \mathrm{~m}^{2},\) the air temperature \(T_{\text {air }}\) is \(47^{\circ} \mathrm{C},\) and the skin temperature \(T_{\text {skin }}\) is \(36^{\circ} \mathrm{C} ;\) (iii) the skin absorbs radiant energy from the sun at a rate of \(1400 \mathrm{~W} / \mathrm{m}^{2} ;\) (iv) the skin absorbs radiant energy from the environment, which has temperature \(47^{\circ} \mathrm{C}\). (a) Calculate the net rate (in watts) at which the person's skin is heated by all four of these mechanisms. Assume that the emissivity of the skin is \(e=1\) and that the skin temperature is initially \(36^{\circ} \mathrm{C}\). Which mechanism is the most important? (b) At what rate (inL/h) must perspiration evaporate from this person's skin to maintain a constant skin temperature? (The heat of vaporization of water at \(36^{\circ} \mathrm{C}\) is \(2.42 \times 10^{6} \mathrm{~J} / \mathrm{kg} .\) ) (c) Suppose the person is protected by light-colored clothing \((e \approx 0)\) and only \(0.45 \mathrm{~m}^{2}\) of skin is exposed. What rate of perspiration is required now? Discuss the usefulness of the traditional clothing worn by desert peoples.

While running, a \(70 \mathrm{~kg}\) student generates thermal energy at a rate of \(1200 \mathrm{~W}\). For the runner to maintain a constant body temperature of \(37^{\circ} \mathrm{C},\) this energy must be removed by perspiration or other mechanisms. If these mechanisms failed and the energy could not flow out of the student's body, for what amount of time could a student run before irreversible body damage occurred? (Note: Protein structures in the body are irreversibly damaged if body temperature rises to \(44^{\circ} \mathrm{C}\) or higher. The specific heat of a typical human body is \(3480 \mathrm{~J} / \mathrm{kg} \cdot \mathrm{K},\) slightly less than that of water. The difference is due to the presence of protein, fat, and minerals, which have lower specific heats.)

At very low temperatures the molar heat capacity of rock salt varies with temperature according to Debye's \(T^{3}\) law: $$ C=k \frac{T^{3}}{\theta^{3}} $$ where \(k=1940 \mathrm{~J} / \mathrm{mol} \cdot \mathrm{K}\) and \(\theta=281 \mathrm{~K}\). (a) How much heat is required to raise the temperature of \(1.50 \mathrm{~mol}\) of rock salt from \(10.0 \mathrm{~K}\) to \(40.0 \mathrm{~K} ?\) (Hint: Use Eq. (17.18) in the form \(d Q=n C d T\) and integrate.) (b) What is the average molar heat capacity in this range? (c) What is the true molar heat capacity at \(40.0 \mathrm{~K} ?\)

A \(\mathrm 500.0 \mathrm{~g}\) chunk of an unknown metal, which has been in boiling water for several minutes, is quickly dropped into an insulating Styrofoam beaker containing \(1.00 \mathrm{~kg}\) of water at room temperature \(\left(20.0^{\circ} \mathrm{C}\right) .\) After waiting and gently stirring for 5.00 minutes, you observe that the water's temperature has reached a constant value of \(22.0^{\circ} \mathrm{C}\). (a) Assuming that the Styrofoam absorbs a negligibly small amount of heat and that no heat was lost to the surroundings, what is the specific heat of the metal? (b) Which is more useful for storing thermal energy: this metal or an equal weight of water? Explain. (c) If the heat absorbed by the Styrofoam actually is not negligible, how would the specific heat you calculated in part (a) be in error? Would it be too large, too small, or still correct? Explain.

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