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  • Chemical Weathering: How Minerals are Removed from Soil and Rock
    The weathering process that results from the removal of minerals in soil and rock is chemical weathering.

    Here's why:

    * Chemical weathering involves changes in the chemical composition of the rock or soil. This can happen through:

    * Dissolution: Water can dissolve certain minerals, like limestone, and carry them away.

    * Oxidation: Iron in rocks can react with oxygen and water, forming rust (iron oxide) which weakens the rock.

    * Hydrolysis: Water molecules can break down mineral bonds, changing the composition of the rock.

    * Biological weathering: Organisms like bacteria and fungi can release acids that break down rocks.

    Physical weathering, on the other hand, involves breaking rocks down into smaller pieces without changing their chemical composition. Examples include:

    * Frost wedging: Water freezes in cracks, expands, and breaks the rock.

    * Abrasion: Rocks rub against each other, causing them to wear down.

    * Thermal expansion and contraction: Fluctuations in temperature cause rocks to expand and contract, creating stress that can lead to fracturing.

    Therefore, the removal of minerals is a clear indication of a chemical weathering process.

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