Question

Water is a crucial agent of chemical weathering, primarily through processes like hydrolysis and carbonation. In hydrolysis, water reacts with minerals in rocks, leading to the breakdown of silicate minerals into clay minerals, releasing essential nutrients. Similarly, carbonation occurs when carbon dioxide dissolves in water to form carbonic acid, which can react with carbonate rocks like limestone, leading to the dissolution of minerals and the formation of features like caverns. Both processes illustrate how water facilitates chemical reactions that alter the composition and structure of rocks.

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GPT-4o mini
Water plays a vital role in chemical weathering through hydrolysis and carbonation. Hydrolysis breaks down silicate minerals into clay and releases nutrients, while carbonation involves carbonic acid dissolving carbonate rocks like limestone, forming caverns. These processes demonstrate how water alters the composition and structure of rocks.

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