Chemical Characteristics of soil
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Questions and Answers

What is the term for the clustering together of soil particles to form larger structures?

  • Aggregates
  • Floccules
  • Flocculation (correct)
  • Pedogenesis
  • What type of charges do soil particles typically have?

  • Negative (correct)
  • Positive
  • Neutral
  • Variable
  • What is the purpose of cations in promoting flocculation?

  • They are repelled by the negative charge of soil particles
  • They neutralize the charge of soil particles
  • They are attracted to the negative charge of soil particles (correct)
  • They increase the negative charge of soil particles
  • What is the benefit of humus in terms of cation exchange capacity?

    <p>It has a higher CEC than clay</p> Signup and view all the answers

    What is the result of a cation with a +2 charge replacing two separate cations each with a +1 charge?

    <p>A release of minerals to the plant</p> Signup and view all the answers

    What happens to cations in the soil solution when plant roots absorb them?

    <p>They are replaced by other cations</p> Signup and view all the answers

    What is the term for the ability of the soil to adsorb cations onto its surface?

    <p>Cation Exchange Capacity</p> Signup and view all the answers

    What type of particles have a higher Cation Exchange Capacity?

    <p>Colloidal humus particles</p> Signup and view all the answers

    What is the effect of adding organic matter to a soil with poor CEC?

    <p>It increases the CEC</p> Signup and view all the answers

    What is the optimal pH range for soil?

    <p>5.5 - 7.5</p> Signup and view all the answers

    What is the effect of liming on soil pH?

    <p>It increases the pH</p> Signup and view all the answers

    What is the main purpose of liming?

    <p>To reduce 'acid leaching'</p> Signup and view all the answers

    Study Notes

    Flocculation

    • Flocculation is the clustering of soil particles to form larger structures called floccules, which improves soil structure.
    • Cations such as Ca2+ and Mg2+ promote flocculation by being attracted to the negative charges on soil particles.
    • Soil particles have a negative charge, with smaller particles having more negative charges.
    • Cations are adsorbed to the surface of soil particles, and polarized water holds soil particles together, trapping larger sand and silt in a floccule structure.
    • High humus content is more beneficial than high clay content because humus is more fertile, holds more water, has a higher Cation Exchange Capacity, encourages more earthworm activity, and has more negative charges, resulting in an increased rate of flocculation.

    Cation Exchange

    • Cation exchange is the ability of the soil to adsorb cations onto its surface and exchange them for other cations.
    • Cations are attracted to the negative charge of clay/humus particles and are adsorbed on the surface.
    • Cations can be released into soil water (soil solution) and be replaced by others, supplying minerals to plants.
    • A cation with a +2 charge (Ca2+) can replace two separate cations each with +1 charge (H+).
    • Cations are removed from soil solution by plant roots.
    • Colloidal humus particles have three times higher cation exchange capacity than colloidal clay particles.
    • Adding organic matter to a soil with poor CEC (like sand) will increase its CEC.
    • Main cations involved in cation exchange are Ca2+, Mg2+, Al3+, H+, and K+.
    • Note that nitrate (NO3-) cannot be held, and sandy soils have the lowest CEC.

    Soil pH

    • Soil pH is the acid-base scale, measuring the concentration of H+ ions in a solution.
    • Acidic soils have a pH of 0-6, neutral soils have a pH of 7, and basic soils have a pH of 8-14.
    • The concentration of acidic ions adsorbed onto the surface of the soil determines the acidity of the soil.
    • Acidic ions include H+ and Al3+, while alkaline/basic ions include Ca2+ and Mg2+.
    • Importance of Soil pH:
      • Lime increases Ca cations available for exchange (H, K, Al).
      • As pH increases, the amount of negative charges on soil colloids increases, leading to greater CEC.
      • Liming reduces ‘acid leaching’.

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    Description

    This quiz covers the process of flocculation, its effects on soil structure, and the role of cations such as Ca2+ and Mg2+ in promoting flocculation.

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