Soil
The type of chemical weathering that breaks down rocks is acid.
Chemical weathering breaks down rocks
Physical weathering is breaking down of rocks by weather that does not change their chemical components. Chemical weathering is weathering that breaks rocks down by a chemical change.
The two types of weathering are mechanical weathering, which breaks rocks into smaller pieces through physical processes like freezing and thawing, and chemical weathering, which alters the composition of rocks through chemical reactions such as oxidation or dissolution. Mechanical weathering physically breaks down rocks, while chemical weathering changes their chemical composition.
weathering
Chemical weathering is the process that breaks down rocks by altering their chemical composition through reactions with substances like water, oxygen, and acids. This process can result in the transformation of minerals within the rock, leading to its decomposition and eventual disintegration.
The differences are that mechanical weathering breaks rocks into little pieces.. Chemical weathering not only breaks the rock but dissolves it.
This is an example of chemical weathering, as the acid rain is reacting chemically with the minerals in the rocks to break them down.
Carbon dioxide is related to chemical weathering as it combines with water to form carbonic acid, which can dissolve minerals in rocks over time. This chemical reaction gradually breaks down the rocks and contributes to the process of weathering.
Yes
Mechanical weathering involves physical processes that break down rocks into smaller pieces, such as freeze-thaw cycles or root growth. Chemical weathering involves chemical reactions that alter the composition of rocks, like oxidation or dissolution. Overall, mechanical weathering physically breaks down rocks, while chemical weathering changes their chemical makeup.
The two kinds of weathering are mechanical weathering, which breaks down rocks into smaller pieces without changing their chemical composition, and chemical weathering, which alters the chemical composition of rocks through processes like oxidation or dissolution.