Soil Properties - PowerPoint PPT Presentation

1 / 38
About This Presentation
Title:

Soil Properties

Description:

Soil Properties By: Johnny M. Jessup Agriculture Teacher/FFA Advisor What is Soil? Is the top layer of the Earth s surface suitable for the growth of plant life. – PowerPoint PPT presentation

Number of Views:77
Avg rating:3.0/5.0
Slides: 39
Provided by: loveffaWo
Category:
Tags: properties | soil

less

Transcript and Presenter's Notes

Title: Soil Properties


1
Soil Properties
  • By Johnny M. Jessup
  • Agriculture Teacher/FFA Advisor

2
What is Soil?
  • Is the top layer of the Earths surface suitable
    for the growth of plant life.

3
The Soil Profile
  • Soil Horizon
  • They are the layers of the different types of
    soil found at different depths in the soil
    profile.
  • Soil Profile
  • A vertical section through the soil extending
    into the unweathered parent materials and
    exposing all the horizons.

4
Master Horizons
  • Are the A, B and C horizons.
  • Typically found in most soils
  • They are a part of a system for naming soil
    horizons in which each layer is identified by a
    code O, A, E, B, C R.

5
The Horizons
  • The O Horizon
  • The organic layer made of wholly or partially
    decayed plant material and animal debris.
  • Normally found in a forest with fallen leaves,
    branches and other debris.

6
The Horizons
  • The A Horizon
  • Also called the topsoil.
  • The most fertile layer of soil.
  • Contains the most organic matter.
  • Usually the top or first layer.

7
The Horizons
  • The E Horizon
  • Also called the layer of eluviation.
  • This is the zone of the greatest leaching of
    clay, chemicals and organic matter.

8
The Horizons
  • The B Horizon
  • Also called the subsoil.
  • Called the zone of accumulation where chemicals
    leached out of the A horizon.
  • Reason why most subsoil has an increase
    in clay content.

9
The Horizons
  • The C Horizon
  • Called the parent material.
  • Lacks the properties of the A B horizon.
  • Less touched by soil forming processes.

10
The Horizons
  • R Horizon
  • Is the underlying bedrock such as.
  • Limestone
  • Sandstone
  • Granite

11
Soil Profiles
12
Soil Texture
  • Refers to the size of particles.
  • Three types are.
  • Sand (Large)
  • Silt (Medium)
  • Clay (Small)

13
Relative Size of Soil Particles
14
Soil Texture - Sandy
  • The largest of the soil particles.
  • Individual particles can be seen with
    the naked eye.
  • Low moisture-holding capacity.

15
Soil Texture - Loamy
  • About equal parts of.
  • Sand
  • Silt
  • Clay
  • Ideal texture for most non-container outside
    plants.

16
Soil Texture - Clayey
  • The smallest of the soil particles.
  • Clay particles stick to one another.
  • Has a high water-holding capacity.

17
Textural Classes
  • There are 12 textural classes.
  • Represented on the Soil Texture Triangle.
  • Textural class determined by the percentage of
    sand, silt, clay.

18
(No Transcript)
19
Soil Structure
  • Refers to the way soil particles cling together
    to form soil units or aggregates, while leaving
    pore space to.
  • Store air.
  • Store water.
  • Store nutrients.
  • Allow root
    penetration.

20
Types of Soil Structures
  • There are five types of soil structures.
  • They are
  • Single grain
  • Granular
  • Platy
  • Blocky
  • Prismatic

21
Soil Structure Single Grain
  • Associated with sandy soils.

22
Soil Structure - Granular
  • Is the best for most plants.
  • Particles cling together to form rounded
    aggregates.
  • It is commonly found in A horizons.
  • Peds are small usually between 1 to 10
    millimeters.

23
Soil Structure - Platy
  • Usually found in E horizons.
  • Large, thin peds.
  • Plate-like arranged in overlapping horizontal
    layers.

24
Soil Structure - Blocky
  • Particles cling together in angular aggregates.
  • Typical of soils with high clay content.
  • Typical of B horizons.
  • Peds are large about 5 to 50 millimeters.

25
Soil Structure - Massive
  • Soil has no visible structure.
  • Hard to break apart appears in very large clods.

26
Soil Structure
  • More important to producers who grow plants in
    natural soils because.
  • Producers of container grown plants add
    ingredients to make growing media desirable.

27
Soil Composition
  • About 50 of the soil should be solid particles.
  • 45 - Minerals
  • 5 - Organic Matter
  • About 50 of soil should be pore space.
  • 25 - Air/Pore Space
  • 25 - Water

28
Soil pH
  • pH has the most impact on the availability of
    nutrients in the soil/media.
  • pH Scale
  • Ranges from 0 to 15.
  • Indicates the level of acidity or alkalinity.
  • 7 is considered neutral.
  • Everything greater than 7 is considered alkaline
    (basic).
  • Everything less than 7 is considered acidic.

29
pH Scale
30
Ideal pH
  • The ideal pH of most ornamental plants
    lawn/turfgrasses is 5.5 to 7.0.

31
Ph Scale Review
  • What would be a pH of 7.0?
  • Neutral.
  • What would a Ph pf 3.5 be?
  • Acidic.
  • What would a pH of 9.0 be?
  • Alkaline.

32
Land Capability
  • Based on the physical, chemical, and
    topographical aspects of the land.

33
Land Capability Classes
  • Assigning a number to
    land.
  • Eight classes used.
  • I to VIII with I having the
    best arability.
  • Class I to IV can be cultivated.
  • V to VIII tend to have high slope or are low
    wet.

34
Land Capability Classes
  • Class I - Very good land.
  • Very few limitations.
  • Deep soil and nearly level.
  • Can be cropped every year as long as land is
    taken care of.
  • Class II - Good land
  • Has deep soil.
  • May require moderate attention to conservation
    practices.

35
Land Capability Classes
  • Class III - moderately good land.
  • Crops must be more carefully selected.
  • Often gently sloping hills.
  • Terraces and strip-cropping are more often used.
  • Class IV - fairly good land.
  • Lowest class cultivated.
  • On hills with more slope than class III.
  • Class V - Unsuited for cultivation.
  • Can be used for pasture crops and cattle grazing,
    hay crops or tree farming.
  • Often used for wildlife or recreation areas.

36
Land Capability Classes
  • Class VI - Not suited for row crops.
  • Too much slope.
  • Usually damaged by erosion with gullies.
  • Can be used for trees, wildlife habitat, and
    recreation.
  • Class VII - Highly unsuited for cultivation.
  • Has severe limitations.
  • Best used for planting trees.
  • Steeply sloping.
  • Large rock surfaces and boulders may be found.
  • Very little soil present.

37
Land Capability Classes
  • Class VIII Cannot be use for commercial plants.
  • Cannot be used for row crops or other crops.
  • Often lowland covered with water.
  • Soil maybe wet or high in clay.
  • Best suited for wildlife recreation.

38
Designed By
  • Johnny M. Jessup, FFA Advisor
  • Hobbton High School
Write a Comment
User Comments (0)
About PowerShow.com