Chemical weathering is influenced by water, oxygen, and carbon dioxide, which play crucial roles in breaking down minerals in rocks.
Water, carbon dioxide, and oxygen are important agents of chemical weathering. Different types of rocks weather at different rates, with more resistant rocks lasting longer. Chemical weathering results from chemical changes to minerals exposed to surface conditions, with factors like water, oxygen, and carbon dioxide playing crucial roles. The presence of water is vital in facilitating chemical reactions that break down minerals in rocks through processes like hydrolysis and dissolution.
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