Chapter 12: Problem 21
Is the melting of ice endothermic or exothermic? What is the sign of \(\Delta H\) for the melting of ice? For the freezing of water?
Short Answer
Expert verified
The melting of ice is endothermic with a positive \(\Delta H\). The freezing of water is exothermic with a negative \(\Delta H\).
Step by step solution
01
Understanding Endothermic and Exothermic Processes
First, recall the definitions of endothermic and exothermic processes. An endothermic process is one that absorbs energy from the surroundings, usually as heat. Conversely, an exothermic process releases energy to the surroundings.
02
Determining the Nature of the Melting of Ice
Determine whether energy is absorbed or released during the melting of ice. Melting ice requires energy to overcome the molecular forces holding the solid together, which means heat is absorbed from the surroundings. Therefore, melting is an endothermic process.
03
Identifying the Sign of \(\Delta H\) for Melting
Since melting is endothermic, the change in enthalpy (\(\Delta H\)) is positive because the system absorbs heat from the surroundings.
04
Assessing the Nature and \(\Delta H\) Sign for Freezing
Freezing is the opposite of melting. During freezing, energy is released to the surroundings as the water molecules form a solid structure. Hence, freezing is exothermic and the sign of \(\Delta H\) is negative.
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Key Concepts
These are the key concepts you need to understand to accurately answer the question.
Enthalpy Change
The term 'enthalpy change' describes the amount of heat released or absorbed by a system at constant pressure. It's represented by the symbol \( \Delta H \). This concept is a fundamental piece of the puzzle in thermal dynamics and helps us understand the energy transfers during physical processes and chemical reactions.
When energy is absorbed in a system, we observe a positive enthalpy change (\(\Delta H > 0\)). This is indicative of an endothermic process, where the system gains heat from its surroundings, potentially leading to an increase in temperature if the heat isn’t used in performing work or causing a phase change.
In contrast, when a process is exothermic, energy is released into the surroundings resulting in a negative enthalpy change (\(\Delta H < 0\)). This can decrease the temperature of the surroundings if the heat is not absorbed by other means.
An easy way to remember this is to think of the sign of \(\Delta H\) as an indicator of where the heat is 'going'. Positive \(\Delta H\) means heat goes 'into' the system, while negative \(\Delta H\) means heat 'exits' the system.
When energy is absorbed in a system, we observe a positive enthalpy change (\(\Delta H > 0\)). This is indicative of an endothermic process, where the system gains heat from its surroundings, potentially leading to an increase in temperature if the heat isn’t used in performing work or causing a phase change.
In contrast, when a process is exothermic, energy is released into the surroundings resulting in a negative enthalpy change (\(\Delta H < 0\)). This can decrease the temperature of the surroundings if the heat is not absorbed by other means.
An easy way to remember this is to think of the sign of \(\Delta H\) as an indicator of where the heat is 'going'. Positive \(\Delta H\) means heat goes 'into' the system, while negative \(\Delta H\) means heat 'exits' the system.
Melting and Freezing of Ice
Understanding the processes of melting and freezing is crucial in grasping how energy transfer works in physical states. Let's take ice as an example. Melting, the transition from solid to liquid, requires that ice absorbs heat from its environment. This heat disrupts the crystalline structure, allowing the molecules to move freely and the solid to become a liquid.
The absorption of heat during this process makes the melting of ice an endothermic process. In other words, the enthalpy change for melting ice is positive (\(\Delta H > 0\)). We can infer that if we wanted to reverse the process—turn water back into ice—we would need to remove heat from the water.
Freezing, therefore, is exothermic – it gives off heat. As water freezes and turns into ice, the molecules slow down and arrange into a more ordered structure, releasing energy in the process. Thus, the enthalpy change for freezing is negative (\(\Delta H < 0\)). Understanding melting and freezing through the lens of enthalpy changes reveals a beautiful symmetry in the laws of thermodynamics.
The absorption of heat during this process makes the melting of ice an endothermic process. In other words, the enthalpy change for melting ice is positive (\(\Delta H > 0\)). We can infer that if we wanted to reverse the process—turn water back into ice—we would need to remove heat from the water.
Freezing, therefore, is exothermic – it gives off heat. As water freezes and turns into ice, the molecules slow down and arrange into a more ordered structure, releasing energy in the process. Thus, the enthalpy change for freezing is negative (\(\Delta H < 0\)). Understanding melting and freezing through the lens of enthalpy changes reveals a beautiful symmetry in the laws of thermodynamics.
Thermochemistry
Thermochemistry is the branch of chemistry that deals with the heat involved during chemical reactions and physical transformations, like phase changes. It's essential in explaining how energy is stored, transferred, and converted from one form to another.
In the context of our ice example, thermochemistry would explore how the melting and freezing relate to heat absorption or release. It also expands our understanding of enthalpy change as it applies to chemical reactions. For instance, when analyzing a chemical reaction, one might use a calorimeter to measure the heat change, which corresponds to the reaction's enthalpy change.
In the classroom or lab, this field allows students to perform experiments that quantify the energy involved in different processes. They learn about concepts like specific heat capacity, conservation of energy, and Hess's Law, which are crucial for solving thermochemical equations. By scrutinizing these reactions and processes, such as the melting of ice, students appreciate the interplay between energy and matter. This knowledge has practical applications in various industries, including materials science, environmental science, and energy production.
In the context of our ice example, thermochemistry would explore how the melting and freezing relate to heat absorption or release. It also expands our understanding of enthalpy change as it applies to chemical reactions. For instance, when analyzing a chemical reaction, one might use a calorimeter to measure the heat change, which corresponds to the reaction's enthalpy change.
In the classroom or lab, this field allows students to perform experiments that quantify the energy involved in different processes. They learn about concepts like specific heat capacity, conservation of energy, and Hess's Law, which are crucial for solving thermochemical equations. By scrutinizing these reactions and processes, such as the melting of ice, students appreciate the interplay between energy and matter. This knowledge has practical applications in various industries, including materials science, environmental science, and energy production.