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CHEMICAL
WEATHERING
   Decomposition of rock in situ resulting
    from chemical change

   Water (rain, fog, moisture, ocean etc) is
    the key medium for chemical weathering.

   Common in warm humid climate (high
    temperature & high rainfall)

   Weathered rocks by this process have a
    dull pitted appearance
1.   Oxidation

2.   Hydration

3.   Hydrolysis

4.   Carbonation

5.   Solution
   Oxygen dissolved in
    water reacts with mineral
    iron in the rock

   The rock is converted to
    iron oxide

   Always seen as reddish-
    brown crust

   This conversion
    weakened the mineral
    bonding and
    consequently the whole
   Involves in the expansion of minerals
    resulting from the absorption of water

   E.g. Clay minerals are capable of absorbing
    large quantities of water into their crystal
    structure

   When this happen, they exerts stresses
    within the rock which may eventually cause it
    to break apart
   Involves a chemical reaction

   between hydrogen ions in water with certain
    minerals in the rock

   E.g. Weakly acidic rainwater causes
    feldspar to be converted into white powdery
    clay (kaolin) which breaks down easily
Hydrolysis
Kaolinite mine
   Is a form of solution weathering

   Common in rocks composed of calcium
    carbonate such as limestone and chalk

   Rainwater mixed with carbon dioxide form
    carbonic acid

   The acid water change the calcium
    carbonate to soluble calcium bicarbonate
    which is then easily washed away
   Simply the
    dissolving
    minerals in water

   E.g Halite (rock
    salt) dissolve in
    water

   Quartz dissolves
    at an extremely
    slow rate
Spheroidical Weathering
   A type of chemical
    weathering

   Creates rounded boulders
    and domed monolith

   Typically granitic in
    composition

   Rock forms at great
    temperatures and pressures
BIOLOGICAL
WEATHERING
   Caused by the action living organisms

   Can lead to physical break down of rock
    (Biophysical)

   Also chemical attack (Biochemical weathering)
1.   By plant roots
2.   By animals such as rodents
     and earthworms
3.   By human activities
   By plant roots:

       When roots
        penetrate
        into
        cracks, they
        will usually
        break rocks
        apart
   By animals:

       Help to widen and
        loosen the joints in
        rocks and expose
        underlying rocks to
        weathering
        processes as they
        burrow through the
        ground
   By human activities:

       Clearing of land for
        cultivation

       Construction and
        mining activities

       This activities break
        up rocks and expose
        them to the
        weathering
   Organic acids from
    dead plants and root
    can help to decompose
    rock

   Chelation is the effect
    of organic acid on rock

   Waste and organic
    acids from dead
    animals help to
    weather rocks
    chemically
   Human activities:

       Industrialisation
        can cause pollution
        such emission of
        sulphur dioxide
        which can produce acid rain

       Accelerate the chemical weathering process of
        hydrolysis, carbonation and solution

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Chemical and biological weathering lesson 5

  • 2.
  • 3. Decomposition of rock in situ resulting from chemical change  Water (rain, fog, moisture, ocean etc) is the key medium for chemical weathering.  Common in warm humid climate (high temperature & high rainfall)  Weathered rocks by this process have a dull pitted appearance
  • 4. 1. Oxidation 2. Hydration 3. Hydrolysis 4. Carbonation 5. Solution
  • 5. Oxygen dissolved in water reacts with mineral iron in the rock  The rock is converted to iron oxide  Always seen as reddish- brown crust  This conversion weakened the mineral bonding and consequently the whole
  • 6.
  • 7.
  • 8.
  • 9. Involves in the expansion of minerals resulting from the absorption of water  E.g. Clay minerals are capable of absorbing large quantities of water into their crystal structure  When this happen, they exerts stresses within the rock which may eventually cause it to break apart
  • 10.
  • 11. Involves a chemical reaction  between hydrogen ions in water with certain minerals in the rock  E.g. Weakly acidic rainwater causes feldspar to be converted into white powdery clay (kaolin) which breaks down easily
  • 14. Is a form of solution weathering  Common in rocks composed of calcium carbonate such as limestone and chalk  Rainwater mixed with carbon dioxide form carbonic acid  The acid water change the calcium carbonate to soluble calcium bicarbonate which is then easily washed away
  • 15.
  • 16.
  • 17. Simply the dissolving minerals in water  E.g Halite (rock salt) dissolve in water  Quartz dissolves at an extremely slow rate
  • 18.
  • 19.
  • 20.
  • 21.
  • 22. Spheroidical Weathering  A type of chemical weathering  Creates rounded boulders and domed monolith  Typically granitic in composition  Rock forms at great temperatures and pressures
  • 23.
  • 24.
  • 25.
  • 27. Caused by the action living organisms  Can lead to physical break down of rock (Biophysical)  Also chemical attack (Biochemical weathering)
  • 28. 1. By plant roots 2. By animals such as rodents and earthworms 3. By human activities
  • 29. By plant roots:  When roots penetrate into cracks, they will usually break rocks apart
  • 30.
  • 31. By animals:  Help to widen and loosen the joints in rocks and expose underlying rocks to weathering processes as they burrow through the ground
  • 32. By human activities:  Clearing of land for cultivation  Construction and mining activities  This activities break up rocks and expose them to the weathering
  • 33. Organic acids from dead plants and root can help to decompose rock  Chelation is the effect of organic acid on rock  Waste and organic acids from dead animals help to weather rocks chemically
  • 34. Human activities:  Industrialisation can cause pollution such emission of sulphur dioxide which can produce acid rain  Accelerate the chemical weathering process of hydrolysis, carbonation and solution