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What is heat capacity? How is it related to changes in temperature?

Short Answer

Expert verified
Heat capacity is the amount of heat needed to raise the temperature of a substance's mass by one degree. It is related to temperature change through the formula \( Q = C \Delta T \), where \( Q \) is heat energy, \( C \) is heat capacity, and \( \Delta T \) is temperature change.

Step by step solution

01

Definition of Heat Capacity

Heat capacity is a physical property of a substance. It is defined as the amount of heat energy required to raise the temperature of a given mass of a substance by one degree Celsius (or one Kelvin). It is denoted as 'C' and commonly measured in units of joules per degree Celsius (J/°C) for a specific amount of substance.
02

Relation to Temperature Change

The heat capacity of a substance is directly related to temperature changes. It tells us how much heat energy is needed to change the temperature of the substance. The formula that connects heat, heat capacity, and temperature change is given by: \( Q = C \Delta T \), where \( Q \) is the heat energy added or removed, \( C \) is the heat capacity, and \( \Delta T \) is the change in temperature. When heat is added to a substance, the temperature increases, and when heat is removed, the temperature decreases.

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Key Concepts

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

Temperature Change
The concept of temperature change is central to understanding heat capacity and thermodynamics. As a start, think of temperature as a measure of the 'hotness' or 'coldness' of a substance, which is directly influenced by the amount of heat energy it contains. When heat energy is transferred to an object, its molecules begin to move more vigorously, and as a result, its temperature rises.

Conversely, when an object loses heat energy, the movement of its molecules slows down, leading to a reduction in temperature. This fundamental phenomenon is quantified by the change in temperature, symbolized as \( \Delta T \), which represents the difference between the final and initial temperatures.

For anyone struggling to grasp this, imagine a cup of coffee cooling over time; the temperature drop is a temperature change. It is an essential concept for many applications, including weather forecasting, designing heating and cooling systems, and understanding how insulating materials work.
Physical Property
Heat capacity is a distinctive physical property, which means it is an attribute that can be measured or observed without changing the substance's chemical identity. It is akin to properties like density, melting point, or color.

In the context of heat capacity, this property helps determine how a substance responds to the addition or removal of heat energy. To illustrate, water has a high heat capacity, meaning it takes a significant amount of heat energy to raise its temperature when compared to a substance like copper.

Understanding physical properties is invaluable in various scientific and engineering disciplines. For instance, knowing the heat capacity of materials is crucial when designing thermal systems like engines or refrigerators, as it determines how much energy will be needed to achieve or maintain a certain temperature.
Heat Energy
Heat energy, often simply called heat, refers to the energy transferred from one body or system to another as a result of a temperature difference. The transfer of heat can occur through various means such as conduction, convection, or radiation.

Considering heat capacity, we quantify heat energy in joules (J) and relate it to how much of this energy is required to change the temperature of a given mass by one degree. It's crucial to clarify that heat energy is not to be confused with temperature, as heat is the energy in transit, whereas temperature is the measure of heat energy possessed by a substance.

In practical scenarios, like heating a room or cooking food, controlling the transfer of heat energy is essential. Materials with different heat capacities will absorb and release heat at different rates, influencing efficiency and outcomes in everyday processes.

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Most popular questions from this chapter

What are the environmental problems associated with fossil-fuel use?

Explain the natural greenhouse effect.

From a molecular standpoint, explain how thermal energy is transferred from a hot object to a cold one.

Why are fossil fuels so named? Where do they come from?

The amount of \(\mathrm{CO}_{2}\) in the atmosphere is \(0.04 \%(0.04 \%\) \(=0.0004 \mathrm{~L} \mathrm{CO}_{2} / \mathrm{L}\) atmosphere). The world uses the equivalent of approximately \(4.0 \times 10^{12} \mathrm{~kg}\) of petroleum per year to meet its energy needs. Determine how long it would take to double the amount of \(\mathrm{CO}_{2}\) in the atmosphere due to the combustion of petroleum. Follow each of the steps outlined to accomplish this: a. We need to know how much \(\mathrm{CO}_{2}\) is produced by the combustion of \(4.0 \times 10^{12} \mathrm{~kg}\) of petroleum. Assume that this petroleum is in the form of octane and is combusted according to the following balanced reaction: $$ 2 \mathrm{C}_{8} \mathrm{H}_{18}(\mathrm{~L})+25 \mathrm{O}_{2}(\mathrm{~g}) \longrightarrow 16 \mathrm{CO}_{2}(\mathrm{~g})+18 \mathrm{H}_{2} \mathrm{O}(\mathrm{g}) $$ By assuming that \(\mathrm{O}_{2}\) is in excess, determine how many moles of \(\mathrm{CO}_{2}\) are produced by the combustion of \(4.0 \times 10^{12} \mathrm{~kg}\) of \(\mathrm{C}_{8} \mathrm{H}_{18}\). This will be the amount of \(\mathrm{CO}_{2}\) produced each year. b. By knowing that \(1 \mathrm{~mol}\) of gas occupies \(22.4 \mathrm{~L}\), determine the volume occupied by the number of moles of \(\mathrm{CO}_{2}\) gas that you just calculated. This will be the volume of \(\mathrm{CO}_{2}\) produced per year. c. The volume of \(\mathrm{CO}_{2}\) presently in our atmosphere is approximately \(1.5 \times 10^{18} \mathrm{~L}\). By assuming that all \(\mathrm{CO}_{2}\) produced by the combustion of petroleum stays in our atmosphere, how many years will it take to double the amount of \(\mathrm{CO}_{2}\) currently present in the atmosphere from just petroleum combustion?

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