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    Arrange the following clay minerals with their increasing order of permanent negative charge (moles sites kg−1): (A) Smectite (B) Illite (C) Kaolinite
    Question



    Arrange the following clay minerals with their increasing order of permanent negative charge (moles sites kg−1): (A) Smectite (B) Illite (C) Kaolinite
    Choose the correct answer from the options given below:

    A.

    (A), (C), (B)

    B.

    (B), (C), (A)

    C.

    (C), (B), (A)

    D.

    (A), (B), (C)

    Correct option is C


    1. Explanation of Permanent Negative Charge:
    · Clay minerals possess a permanent negative charge due to isomorphous substitution, where higher-valence cations are replaced by lower-valence cations within the clay structure.
    · The magnitude of the negative charge depends on the clay mineral's structure and chemical composition.
    2. Analysis of the Given Minerals:
    · Kaolinite:
    · Least negatively charged due to its 1:1 layer structure (one silica tetrahedral sheet and one aluminum octahedral sheet).
    · Minimal isomorphous substitution.
    · Permanent negative charge: low.
    · Illite:
    · Intermediate negative charge due to its 2:1 layer structure (two tetrahedral and one octahedral sheet).
    · Moderate isomorphous substitution in tetrahedral sheets.
    · Permanent negative charge: moderate.
    · Smectite:
    · Highest negative charge due to significant isomorphous substitution in its 2:1 layer structure.
    · It has a large surface area and high cation exchange capacity (CEC).
    · Permanent negative charge: high.
    3. Order of Increasing Permanent Negative Charge:
    · Kaolinite (C) < Illite (B) < Smectite (A).
    Thus, the correct answer is (3) (C), (B), (A)
    Information Booster: 1. Cation Exchange Capacity (CEC):
    · Indicates the ability of clay minerals to hold and exchange cations.
    · Order: Smectite > Illite > Kaolinite.
    2. Structural Differences in Clays:
    · Kaolinite: 1:1 structure; low surface area and minimal negative charge.
    · Illite: 2:1 structure with moderate charge and binding strength.
    · Smectite: 2:1 structure with high negative charge and swelling capacity.
    3. Applications of Clay Minerals:
    · Kaolinite: Used in ceramics, paper, and cosmetics due to its low plasticity and low charge.
    · Illite: Common in soil fertility studies for its moderate CEC.
    · Smectite: Applied in drilling muds, liners for landfills, and water treatment due to its high adsorption capacity.
    Additional Knowledge: · Importance of Negative Charge in Clays:
    · Influences soil fertility by retaining nutrients like potassium and calcium.
    · Affects water retention and soil structure.
    · Role in Agriculture:
    · Soils rich in smectite are fertile but prone to swelling and shrinkage.
    · Kaolinitic soils are less fertile but more stable structurally.

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