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  • Weathering Processes: Formation of New Substances Explained
    Weathering processes can lead to the formation of various new substances, depending on the type of weathering and the parent material. Here's a breakdown:

    1. Physical Weathering:

    * Physical weathering primarily breaks down rocks into smaller pieces without changing their chemical composition. However, it can create new surfaces that are more susceptible to chemical weathering.

    * Examples:

    * Frost wedging: Water seeps into cracks, freezes, expands, and widens the cracks.

    * Thermal expansion and contraction: Rocks expand when heated and contract when cooled, leading to fracturing.

    * Abrasion: Rocks collide with each other, causing wear and tear.

    * Root wedging: Growing plant roots exert pressure on rocks, causing them to break.

    2. Chemical Weathering:

    * Chemical weathering alters the chemical composition of rocks, leading to the formation of new minerals and substances.

    * Examples:

    * Hydrolysis: Water reacts with minerals in rocks, causing them to break down.

    * Oxidation: Oxygen reacts with minerals, especially iron, forming iron oxides (like rust).

    * Carbonation: Carbon dioxide dissolves in water, forming carbonic acid, which reacts with carbonate minerals like limestone, dissolving them.

    * Biological Weathering: Plants and animals can release acids that break down rocks.

    * Acid Rain: Sulphuric acid and nitric acid in acid rain react with rocks, especially limestone and marble, causing them to dissolve.

    New Substances Formed:

    * Clay minerals: Formed by the hydrolysis of feldspar and other minerals.

    * Iron oxides: Formed by the oxidation of iron-containing minerals.

    * Carbonates: Dissolved by carbonic acid, but can also be formed by the reaction of calcite with organic acids.

    * Gypsum: Formed by the reaction of water with calcium sulfate.

    * Sulphates: Formed by the reaction of water with sulfides.

    Important Note:

    * The specific substances formed through weathering depend on the original composition of the rock and the specific weathering processes involved.

    * The products of weathering can then be transported and deposited elsewhere, contributing to soil formation, sedimentary rock formation, and other geological processes.

    Let me know if you want more detail on any specific weathering process or the substances it forms!

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