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7.2 NOTES What is chemical weathering? Objective: Explain how Earth’s surface is worn away by chemical weathering In chemical weathering, substances in water cause substances in rocks to dissolve. This action weakens the rock’s structure over time. Chemical changes occur when minerals in rocks are broken down into other substances. They also occur when minerals are added or removed from rocks. Chemical weathering is usually caused by reactions with oxygen, water, or acids. OxidationOxidation occurs when oxygen combines with another substance, forming oxides. Rust is an iron oxide. Rocks such as pyrite and magnetite have minerals that contain iron. When exposed to the air, the iron undergoes oxidation, and the rocks weaken and crumble. WaterMost chemical weathering is caused by water. Hydrolysis is a chemical reaction that occurs when minerals with little water content react with water. When feldspar combines chemically with water, it changes into clay. When heated or dried even a little, the minerals formed by hydrolysis may fall apart. AcidsCarbon Dioxide can dissolve in rain to form weak carbonic acid. When this acid comes in contact with certain minerals, carbonation occurs. The mineral calcite is changed by carbonation. Two rocks that are made of calcite are limestone and marble. Buildings made of these materials are often weathered by carbonation. Some green plants produce weak acids that wear away at rock surfaces. Decaying organisms also produce acids. The internal structure of materials that come in contact with these mosses or decayed organisms will weaken over time.