Physical Changes: Condensation
Interactive passage with audio narration, comprehension questions, and printable PDF.
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About this printable Physical Changes: Condensation science reading passage, NGSS-aligned (Grades 5-8)
Sample passage and quiz from Physical Changes: Condensation
Reading passage and comprehension quiz preview
Why Condensation Is a Physical Change

Condensation is a physical process where a substance changes from a gas to a liquid. This change is important in many natural and everyday systems, such as the formation of dew on grass or water droplets on a cold drink. When water vapor in the air cools down, it turns into liquid water. This transformation is part of the water cycle, which moves water through the environment and affects weather and climate. Understanding condensation helps explain how clouds form, how rain develops, and why mirrors fog up after a hot shower.
How Condensation Happens: The Particle Perspective
On a microscopic level, all matter is made of particles that are always moving. In a gas, like water vapor, these particles move quickly and are far apart. When the gas cools, the particles lose energy and begin to slow down. As they move slower, the particles come closer together and form a liquid. This process releases energy into the surroundings, often as heat. For example, when humid air touches a cold surface, like the outside of a chilled glass, the water vapor cools and condenses, forming visible droplets. The rate of condensation increases when the temperature of the surface is much colder than the air, which is why more droplets appear on very cold drinks.
Real-World Examples and Applications
Condensation is responsible for many familiar phenomena. Dew forms on grass in the early morning when the air cools overnight, causing water vapor to condense on surfaces. Fog appears when warm, moist air meets cooler air or ground, making tiny droplets of water suspended in the air. After a hot shower, the bathroom mirror fogs up because water vapor hits the cold glass and condenses. In the atmosphere, clouds form when air rises, cools, and water vapor condenses around tiny particles like dust. Condensation is also essential in technology, such as air conditioners and refrigerators, which use it to remove heat and cool spaces efficiently.
Condensation and the Water Cycle
The role of condensation goes beyond everyday life. It is a critical part of the water cycle. Water evaporates from oceans, lakes, and rivers into the atmosphere as vapor. When this vapor rises and cools, condensation turns it back into liquid water, which can become clouds and eventually precipitation like rain or snow. This cycle ensures that fresh water is distributed across the planet, supporting all life. Scientists study condensation to better predict weather patterns and understand climate systems. The energy released during condensation also plays a role in storm development and atmospheric movement.
Condensation shows how changes in energy and particle motion can lead to important physical changes. It connects the behavior of molecules to large-scale natural processes, demonstrating the interactions between matter and energy in our world.
Interesting Fact:
A single cumulus cloud can contain more than 500,000 kilograms (over 1 million pounds) of condensed water droplets created by condensation in the atmosphere!
Comprehension quiz (10 questions)
1. What is condensation?
2. Which of the following is an example of condensation?
3. Why do water droplets form on the outside of a cold drink?
4. What happens to the energy of particles during condensation?
5. What does the term 'precipitation' mean in the context of the water cycle?
6. In the passage, what does the word 'particles' mean?
7. How does condensation relate to cloud formation?
8. Why is condensation important in air conditioners and refrigerators?
9. Condensation only happens at high temperatures. (True/False)
10. The energy released during condensation can help form storms. (True/False)
Perfect for the way you teach
- Build comprehension skills
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- Improve fluency
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