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Physical Properties of Soil

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Layers are cemented by a special type of clay common to the tropics ... Has chemicals cement soil particles together. Soil Colors. Dark Brown to Black ... – PowerPoint PPT presentation

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Title: Physical Properties of Soil


1
Chapter 3
  • Physical Properties of Soil

2
Soil Texture
  • What is Soil Texture?
  • It is the proportion of three sizes of soil
    particles.
  • Which are
  • Sand (Large)
  • Silt (Medium)
  • Clay (Small)

3
Soil Texture
  • Effects of Particle Size?
  • Soil particle size affects two important soil
    features
  • They are internal surface area
  • The numbers and size of the pore spaces

4
Soil Texture
  • What is the internal surface area ?
  • It is the area of soil that the total surface
    are of the particles in the soil.
  • So the smaller the soil particles the greater the
    internal surface area will be.

5
Soil Texture
  • Pore size and number
  • this depends on the particle size.
  • So there are more pores that are found between
    the larger particles.
  • See page 34 for example.

6
Soil Texture
  • What is a Soil Separates?
  • They are categories that scientist have divided
    up into three groups
  • The three groups are
  • Sand
  • Silt
  • Clay

7
Soil Texture
  • What is Sand?
  • It is the largest and is further divided into
    four subcategories.
  • They are
  • Very coarse sand
  • Coarse sand
  • Medium sand
  • Fine Sand

8
Soil Texture
  • Sand
  • it is the larges soil separate and is composed
    mainly of weathered grains of quartz.
  • Sand is also gritty to the touch.
  • Sand grains will not stick to each other.

9
Soil Texture
  • Sand
  • What will sand do to the soil?
  • It will improve the soil by improving the water
    infiltration and aeration

10
Soil Texture
  • Silt
  • is the medium sized soil separated.
  • Silt particles are silky or powdery to the touch
  • Silt grains will not stick to one another just
    like sand grains.
  • Silt is the best soil as it has the ability to
    hold large amounts of water in a form plants can
    use.

11
Soil Texture
  • Clay
  • is the smallest size soil separate.
  • It is composed of tiny crystals
  • Clay is formed by chemical reactions between
    weathered minerals to form tiny particle of new
    minerals.
  • Clay will hold more plant nutrients than any
    other separate.
  • Clay grains will stick to one another.

12
Soil Texture
  • There are 12 textural classes which can be seen
    in the next slide.

13
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14
Soil Texture
  • Pass out picture of triangle and lets see if we
    can classify some soils.

15
Soil Texture
  • 1.
  • 40 sand 22 clay and 38 silt
  • What is the soil classified as?

16
Soil Texture
  • 2.
  • 90 sand 10 clay and 25 silt
  • What is it?

17
Soil Texture
  • 3.
  • 30 sand 50 clay and 15 silt
  • What is it?

18
Soil Texture
  • 4.
  • 10 sand 80 clay and 30 silt.
  • What is it?

19
Soil Texture
  • Lets go and texture some of the kits that we
    have.
  • See if you can make a ribbon and with which one?
  • Which one feels grittiest?
  • Which one feel powdery?

20
Soil Density and Permeability
  • What is Particle Density?
  • it is the density of solid particles only.

21
Soil Density and Permeability
  • What is Bulk Density?
  • It is the mass of a volume of undisturbed oven
    dry soil
  • BD Weight dry soil
  • ___________ __G__
  • Volume dry soil cm3

22
Soil Density and Permeability
  • Example BD
  • The core is 500 cubic cm that weighs 650 grams
  • What is the answer?

23
Soil Density and Permeability
  • Answer
  • BD 650g
  • ______ 1.3 g/cm3
  • 500 cm3

24
Soil Density and Permeability
  • Soil Porosity
  • Total pore space is measured of the soil volume
    that holds air and water.
  • SPwet weight(g) dry weight (g)
  • _____________________ x100
  • soil volume (cm3)

25
Soil Density and Permeability
  • Example
  • The soil core before had a volume of 500 cubic
    centimeters and weighed 650 grams when dry.
    When wet the same core weighed 900 grams.
  • Calculate Porosity.

26
Soil Density and Permeability
  • Answer
  • 900-650
  • _________x100 50
  • 500

27
Soil Density and Permeability
  • What is Permeability?
  • is the ease of which air, water, and roots move
    through the soil

28
Soil Density and Permeability
  • What is Hydraulic Conductivity?
  • Is the measure of the rate of water movement
    through the soil

29
Soil Structures
  • What is Soil Aggregates?
  • It is aggregates that occur naturally in the
    soil are called peds. While clumps of soil
    caused by tillage are called clods

30
Types of Soil Structures
  • Before we discuss these turn to pg 43.
  • There are four types of soil structures.
  • They are
  • Granular structure
  • Platy structure
  • Blocky structure
  • Prismatic structure

31
Types of Soil Structures
  • What is Granular structure?
  • It is commonly found in A horizons
  • Peds are small usually between 1to 10
    millimeters

32
Types of Soil Structures
  • What is Platy Structures?
  • Usually found in E horizons
  • Peds are large but tin, platelike and arranged
    in overlapping horizontal layers.

33
Types of Soil Structures
  • What is Blocky Structures?
  • This is the typical of my B horizons
  • Peds are large about 5 to 50 millimeters

34
Types of Soil Structures
  • What is Prismatic structure?
  • found in Horizon B
  • Peds are large range from 10- 100 millimeters in
    size

35
Soil Tilth
  • What is Soil Tilth?
  • is a general term for the physical conditions of
    a tilled soil.

36
Soil Tilth
  • What is compaction?
  • It is the result when pressure is applied to
    the soil surface.

37
Soil Tilth
  • Now you will read pages 45-50 and will take notes
    over these pages

38
Soil Pans
  • What is a pan?
  • It is any layer of hardened soil.
  • There are four types of pans
  • Clay pan
  • Fragipans
  • Plinthite
  • Caliche and duripans

39
Soil Pans
  • Claypans
  • Has a very high clay content in the subsoil
    layer. This layer is very dense

40
Soil Pans
  • Fragipans
  • results from clay accumulation
  • Clay will bind soil particles into hard brittle
    layer

41
Soil Pans
  • Plinthite
  • Layers are cemented by a special type of clay
    common to the tropics
  • These soils are very poor for Agriculture uses.

42
Soil Pans
  • Caliche and Duripans
  • Has chemicals cement soil particles together

43
Soil Colors
  • Dark Brown to Black
  • dark colors result from organic matter or dark
    parent material.

44
Soil Colors
  • White to Light Gray
  • color indicates that chemicals that color soil
    have leached out
  • May also be a result of a large amount of lime in
    one place for the white appearance.

45
Soil Colors
  • Light brown, Yellow to Red
  • These are the colors of oxidized iron minerals,
    chemically similar to rust
  • Red indicates good drainage

46
Soil Colors
  • Bluish Gray
  • this is the color of less oxidized iron and
    indicates a lack of oxygen in the soil
  • So this is an indication of poor drainage

47
Soil Colors
  • Mottled Colors
  • Will show different colors often spots of rust,
    yellow, and gray.

48
Soil Colors
  • Hue-
  • is the color such as red and yellow
  • Value-
  • Is the lightness or darkness of the hue 0-10 and
    0 being the darkest and 10 the lightest
  • Chroma- is the purity of the dominant color and
    is also number

49
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