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Weathering and Soil Formation

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Title: Weathering and Soil Formation


1
Weathering and Soil Formation
2
Weathering
  • The breaking down of rocks and other materials on
    the Earths surface is called weathering. A
    slow, continuous process, it affects all
    substances exposed to the atmosphere.

3
Types of Weathering
  • Rocks on the Earths surface are broken down by
    two types of weathering mechanical and chemical.

4
Mechanical Weathering
  • When the forces of weathering break rocks into
    smaller pieces but do not change the chemical
    makeup of the rocks, the process is called
    mechanical weathering. During mechanical
    weathering, rocks are broken into different
    shapes and smaller pieces. At the beginning the
    edges are jagged, as weathering continues, they
    become round.

5
Causes of Mechanical Weathering
  • There are several causes of mechanical
    weathering.
  • Temperature
  • Frost action
  • Organic activity
  • Gravity
  • abrasion

6
Temperature
  • Rocks can be broken apart by changes in
    temperature. As rocks are heat up in the sun
    during the day, the outside of the rock expands.
    The inside of the rocks remain cool and do not
    expand. When the air temperature drops at night,
    the outside of the rock cools and contracts.
    This continuing cycle causes particles to break
    off. This is called exfoliation.

7
Frost Action
  • Unlike most liquids, water expands when it
    freezes. The repeated freezing and melting of
    water, called frost action, is another cause of
    mechanical weathering. When water freezes in
    cracks in the rocks, it expands, making the crack
    larger.In time, this causes the rock to break
    into pieces.

8
Organic Activity
  • Plants and animals can cause mechanical
    weathering. The roots of plants sometimes
    loosens rock material. A plant growing in a
    crack can make the crack larger as the root
    spread out. This is known as root-pry. It is
    organic since this activity is caused by living
    things.

9
Gravity
  • Gravity is another agent of mechanical
    weathering. Sometimes gravity pulls loosened
    rocks down mountain cliffs in a landslide. A
    landslide is a large movement of loose rocks and
    soil. As the rocks fall, they collide with one
    another and break into smaller pieces. Falling
    rocks usually occur in areas where a road has
    been cut through, leaving cliffs on both sides.

10
Abrasion
  • Wind-blown sand causes mechanical weathering .
    Abrasion is the wearing away of rocks by solid
    particles carried by wind, water or other forces.
    In desert regions, the wind easily picks up and
    moves sand. The sharp edges of the sand
    particles scrape off pieces of exposed rocks.
    Running water also carries loose rocks which
    scrape against each other and break.

11
Chemical Weathering
  • When the chemical makeup of the rocks is changed
    it is called chemical weathering. During
    chemical weathering, changes occur in the mineral
    composition of rocks. Minerals can be added,
    removed or broken down (decomposed).Many
    substances react chemically with rocks to break
    them down.

12
Types of Chemical Weathering
  • There are several causes of chemical weathering.
  • Water
  • Oxidation
  • Carbonation
  • Sulfuric acid
  • Plant acids

13
Water
  • Most chemical weathering is caused by water and
    carbon dioxide. Water can dissolve most of the
    mineral that hold rocks together. Rocks that
    dissolve in water are said to be soluble. Water
    can form acids when it mixes with certain gases
    in the atmosphere to speed up the decomposition
    of rocks. Water can also combine with a mineral
    to form a new mineral.

14
Oxidation
  • Chemical weathering is also caused by oxidation.
    Oxidation is the process in which oxygen
    chemically combines with another substance. The
    result of oxidation is the formation of an
    entirely different substance. Iron in rocks
    combines with oxygen in the air to form iron
    oxide, or rust.

15
Carbonation
  • When carbon dioxide dissolves in water, a weak
    acid called carbonic acid is formed. When
    carbonic acid reacts chemically with other
    substance, the process of carbonation occurs. In
    nature, carbonic acid is formed when carbon
    dioxide in the air dissolves in rain. This acid
    rain falls to the ground and sinks into the soil.
    It decomposes feldspar and limestone.

16
Sulfuric Acid
  • The air in certain areas is polluted with sulfur
    oxides. Sulfur oxides are a byproduct of the
    burning of coal as a source of energy. These
    compounds dissolve in rainwater to form sulfuric
    acid. Rain that contains sulfuric acid is one
    type of acid rain. It is much stronger than
    carbonic acid. Sulfuric acid corrodes rocks,
    metals and other materials quickly.

17
Plant Acids
  • Plants produce weak acids that dissolve certain
    minerals in rocks. Mosses and lichens produce
    weak acids that dissolve some of the minerals in
    the rocks they grow on. Gradually the rocks
    break into smaller pieces. They are important in
    the formation of soil.

18
Rate of Weathering
  • The rate of weathering depends on several
    factors, including
  • The composition of the rock
  • The amount of time that the rock is exposed on
    the Earths surface
  • The amount of exposed surface on a rock

19
Composition of Rocks
  • Two different types of rocks in the same climate
    can weather differently, depending on the
    minerals that make up each rock type. If the
    minerals in a rock resist chemical weathering,
    the rock is called a stable rock. The stability
    of a rock can vary depending on the climate in
    which the rock is found. Limestone is stable in a
    dry climate but not in a wet climate.

20
Amount of Time of Exposure
  • The amount of time that rock is exposed on the
    Earths surface also affects its rate of
    weathering. A very old rock that has not been
    exposed to the forces of weathering can remain
    almost unchanged. If a newly formed rock is
    deposited on the Earths surface it will begin to
    weather right away.

21
The Amount of Exposed Surface
  • The amount of exposed surface area on a rock also
    affects its rate of weathering. As rocks are
    broken down into many small pieces, more rock
    surfaces are exposed and more weathering takes
    place. In rocks that contain many joints or
    cracks, various chemicals easily come into
    contact with the rock surfaces and break them
    down.

22
Soil Formation
  • The weathering of rocks on the Earths surface
    results in the formation of soil. Soil is formed
    when rocks are continuously broken down by
    weathering. As rocks weather, they break into
    smaller pieces. These pieces are broken down
    into even smaller pieces to form soil.

23
Importance of Soil
  • The formation of soil is extremely important to
    most living organisms. Plants depend on soil as
    source of food. Soil supplies plants with
    minerals and water needed for growth. Animals
    depend indirectly on soil since they eat plants
    and other animals that eat plants.

24
Residual Soil
  • Sometimes soil remains on top of its parent rock,
    or the rock from which it was formed. This is
    called residual soil. Residual soil has a
    composition similar to that of the parent rock it
    covers.

25
Transported Soil
  • Some soil is removed from the parent rock by
    water, wind, glaciers and waves.soil that is
    moved away from its place of origin is called
    transported soil. Transported soil can be very
    different in composition from the rock it covers.

26
Bedrock
  • The layer of rock beneath the soil is called
    bedrock.

27
Decay
  • Certain bacteria in the soil cause the decay of
    dead plants and animals. This decaying material
    is called humus. Humus is a dark-colored
    material that is important for the growth of
    plants. Some of the chemicals produced during
    the process of decay speed up the breakdown of
    rocks into soil.

28
Living Things
  • Living things such as moles, earthworms, ants and
    beetles help to break apart large pieces of soil
    as they burrow through the ground. The burrows
    allow water to move rapidly through the soil.
    The water speeds up the weathering of the
    underlying rock.

29
Soil Composition
  • Pieces of weathered rock and organic material, or
    humus, are the two main ingredients of soil.
    Organic materials is material that was once
    living or was formed by the activity of living
    organisms. Rock particles form more than 80 of
    soil. Air and water are also present in soil.

30
Minerals in Soil
  • Clay and quartz are the most abundant minerals in
    soil. Because they are stable, they exist in the
    greatest quantities. Potassium, phosphorus and
    the nitrogen compounds called nitrates are
    important chemicals in soil. They are vital to
    plant growth.

31
Pore Spaces
  • Air and water fill the spaces between soil
    particles. These are called pore spaces.
    Plants and animals use the water and air in these
    spaces, as well as the minerals dissolved in
    water. Pore spaces provide needed oxygen for
    healthy plant root growth.

32
Different Compositions of Soil
  • The composition of soil varies from place to
    place. The type of rock broken down by
    weathering determines the kinds of minerals in
    the soil. The type of weathering also affects
    the composition of soil. Mechanical weathering
    produces soil with a composition similar to the
    rock being weathered. Chemical weathering
    produces soil with a different composition.

33
Soil Texture
  • The type of weathering also affects soil texture.
    Texture refers to the size of the individual
    soil particles. Soil particles vary from very
    small to large. Both mechanical and chemical
    weathering first breaks rocks into gravel
    (2-64mm) and then in sand (less than 2mm) and
    finally into silt.

34
Soil Horizons
  • As soil forms, it develops separate soil layers
    called horizons. Each soil horizon is different.
    A cross section of the soil horizons is called
    soil profile. A soil profile shows the different
    layers of soil.

35
Mature Soil
  • Soil that has developed three layers is called
    mature soil. It takes thousands of years and the
    proper conditions for soil to develop three
    layers. The uppermost layer of mature soil is
    called the A horizon. The A horizon is a
    dark-colored soil layer in which much activity by
    living organisms takes place. Bacteria,
    earthworms and beetles help the decay.

36
A Horizon
  • The soil in the A horizon is called topsail.
    Topsail consists mostly of humus and other
    organic materials. Humus supplies minerals
    essential for plant growth. Humus is spongy and
    stores water. It also contains pore space for
    air and water. Topsoil is the most fertile part
    of the soil.

37
B Horizon
  • Water that soaks into the ground washes some
    minerals from the A horizon into the second layer
    of soil, or the B horizon. This process is
    called leaching.The B horizon is just below the A
    horizon. The B horizon is also made of clay and
    some humus. The soil in the B horizon is called
    subsoil. Subsoil is formed very slowly.

38
C Horizon
  • The third layer of soil is called the C horizon.
    The C horizon consists of partly weathered rock.
    The C horizon extends down to the top of the
    unweathered parent rock. The composition of the
    soil in the C horizon is similar to that of the
    parent rock.

39
Immature Soil
  • . In some places, the upper layers of soil are
    removed and the rocks below the soil are exposed.
    The weathering process then forms new soil from
    the exposed rocks. This recently formed soil is
    immature because there has not been enough time
    for all three soil layers to form. The soil in
    the northern regions where glacial erosion has
    taken place, is immature soil.

40
Formation of Soil
  • There are several factors that determine whether
    three layers of soil will form.
  • Time
  • Climate
  • Type of rock
  • Surface features of the region

41
Time
  • Time is one of the most important factors in soil
    formation. The longer a rock is exposed to the
    forces of weathering, the more it is broken down.
    Mature soil is formed if all three layers have
    had time to develop.

42
Climate
  • Climate is another important factor in the
    formation of soil. In areas with heavy rainfall
    and warm temperatures, weathering takes place
    more rapidly. Heavy rainfall may wash much of the
    topsoil away. Since Organisms are more plentiful
    these areas, the soil is quickly replaced. They
    speed up the chemical and mechanical weathering
    of rocks.

43
Type of Rock
  • The type of rock in an area also affects soil
    formation. Some rocks do not weather as rapidly
    as other do. Rocks that do not break down easily
    do not form soil rapidly. In some climates it
    takes along time for granite to break down. So
    soil formation from granite is slow. But
    sandstone breaks easily and forms soil quickly.

44
Surface Features of Region
  • The surface features of the region also determine
    the speed at which soil is formed. On very steep
    slopes, rainwater running off the land erodes the
    soil and exposes rock to weathering.

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