Chemical Weathering (2024)

Chemical Weathering (1)

If you’ve ever seen a rusty building, a statue that looks like it’s rotting, or the green copper roof of the Parliament buildings in Ottawa, you’ve seen chemical weathering in action. In this experiment, discover the effect of size on weathering reactions.

What you need

  • Vinegar
  • Sidewalk chalk (make sure it says calcium carbonate on the label)
  • Two glass cups or jars
  • Pencil and paper

Make it

  1. Take two pieces of equal-sized chalk and place one inside one of the jars.
  2. Break the other piece up into many smaller pieces, and place the pieces inside the other jar.
  3. Fill the jars with approximately the same amount of vinegar. It should be enough to completely cover all of the chalk, but with some room left at the top.

Test it

Watch the two jars for about two minutes and record your observations. What do you notice is different between them? Why do you think that it happened?

Explain it

Sidewalk chalk contains a compound called calcium carbonate (CaCO3), which reacts with vinegar (acetic acid, CH3COOH) to form the gas carbon dioxide (CO2). Some of the mass of the chalk is lost to form this gas, making it smaller.

You will have noticed that the reaction with the broken-up chalk happens much quicker than the solid piece of chalk, as seen by how quickly the bubbles are produced. This is because the reaction needs to have vinegar and chalk molecules colliding together to complete. When the chalk is broken up, more surface area is created on the small pieces for the reaction to occur.

Observe it

Although it is a slower process in nature, this same reaction happens to limestone — acidic rain reacts with it, producing carbon dioxide. This process is called chemical weathering. As shown in this experiment, when the limestone is in smaller pieces, it will be weathered away more quickly, even with the same mass. Take a look at some statues in your town or city; can you tell which ones are older?

Go further

In nature, usually when something needs their surface to perform something (like a reaction) often, the structure is small. This is because smaller objects have more surface area in comparison to their volume.

This can be shown mathematically. Imagine you have three cubes: one with the dimensions 1x1x1, one that’s 2x2x2 and one that’s 3x3x3. First, calculate the volume (length3), and then calculate the surface area (length2 x 6) for each cube. Then, take a look at how fast both the surface area and the volume are growing from one cube to the next. You’ll notice that volume grows more quickly than surface area, so the ratio between them gets smaller.

This phenomenon allows things like cells to be as efficient as they are; their small size allows them to transport more food over their surface, while not wasting energy on a big interior!

Chemical Weathering (2)

Chemical Weathering (3)

Chemical Weathering (2024)

FAQs

What is the definition of chemical weathering? ›

Chemical weathering involves the interaction of rock with mineral solutions (chemicals) to change the composition of rocks. In this process, water interacts with minerals to create various chemical reactions and transform the rocks.

Where are chemical weathering examples? ›

Chemical weathering occurs when water dissolves minerals in rocks, resulting in new compounds. This is also known as hydrolysis. An example would be when water comes in the proximity of granite. Feldspar crystals present inside the rock react chemically, forming clay minerals.

Which process is an example of chemical weathering? ›

Chemical Weathering is an erosional process in which rocks and other materials are broken down by chemical reactions (predominantly by water and chemicals dissolved within it). This process occurs when water comes into contact with rocks and dissolves the minerals that make up that rock into individual elements.

What are the products of chemical weathering? ›

The clay gradually gets eroded away, then the rock breaks apart leaving lots of grains of quartz. In other words, quartz, clay minerals, and dissolved ions are the most common products of weathering.

What is chemical weathering for kids? ›

What is chemical weathering for kids? Chemical weathering slowly decomposes or decays rocks and minerals. It is caused by rain water reacting with the mineral grains in rocks, to form new minerals and soluble salts.

What is chemical erosion? ›

Erosion is the process where rocks are broken down by natural forces such as wind or water. There are two main types of erosion: chemical and physical. Chemical erosion occurs when a rock's chemical composition changes, such as when iron rusts or when limestone dissolves due to carbonation.

Is the best example of chemical weathering? ›

Rusting iron because of oxidation is the best example of chemical weathering. Oxidation occurs where there is ready access to the atmosphere and oxygenated waters.

What is an example of chemical weathering 4th grade? ›

Chemical weathering can cause minerals to decompose and even dissolve. Examples of chemical weathering include how acid rain can change the appearance of a statue and the way salty ocean water wears away cliffs.

Which example will have the most chemical weathering and why? ›

Chemical weathering is highest in areas that are warm and wet. One of the main ways that chemical weathering occurs is when water gets into the rocks and reacts with the minerals inside the rock, softening them and causing the rock to break down. In areas of high rainfall, this will occur more often.

Is ice wedging chemical weathering? ›

Ice wedging is a form of mechanical weathering or physical weathering in which cracks in rock or other surfaces fill with water, freeze and expand, causing the cracks to enlarge and eventually break.

Is ice breaking a rock chemical weathering? ›

Mechanical weathering breaks rocks into smaller pieces without changing their composition. Ice wedging and abrasion are two important processes of mechanical weathering. Chemical weathering breaks down rocks by forming new minerals that are stable at the Earth's surface.

What is an example of weathering in real life? ›

Examples of physical weathering include potholes in roadways, tree roots breaking apart sidewalks, salt causing honeycomb appearance in rocky shores, and river currents breaking down and rounding pebbles.

Which is not an example of something that can cause chemical weathering? ›

The correct answer is Thermal expansion. Thermal expansion is NOT a chemical weathering process. Thermal expansion, which typically excludes phase transitions, is the tendency of matter to change its shape, area, volume, and density in response to a change in temperature.

What are the 5 processes of chemical weathering? ›

The Important processes of chemical weathering are solution, carbonation, hydration, oxidation and reduction. These processes act on the rocks to decompose, dissolve or reduce them to a fine clastic state through chemical reactions by oxygen, surface and/or soil water and other acids.

What is an example of chemical weathering hydration? ›

Hydration is a form of chemical weathering in which the chemical bonds of the mineral are changed as it interacts with water. One instance of hydration occurs as the mineral anhydrite reacts with groundwater. The water transforms anhydrite into gypsum, one of the most common minerals on Earth.

What is the definition of biological weathering? ›

Biological weathering occurs when plants break up rocks with roots or root exudates. The process is slow, but may strongly influence landscape formation.

What is chemical weathering in a sentence? ›

The acidic action of some organisms such as lichens that live on rocks can cause chemical weathering. In arid and semi-arid lands, the scarcity of water generally slows the effects of chemical weathering.

What is the definition of chemical weathering quizlet? ›

Chemical Weathering. the process that breaks down rock through chemical changes.

What does physical weathering mean? ›

Physical weathering, also called mechanical weathering, is a process that causes the disintegration of rocks, mineral, and soils without chemical change. The primary process in physical weathering is abrasion (the process by which clasts and other particles are reduced in size).

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