Earth Science Unit 1.4: Weathering and Soils - PowerPoint PPT Presentation

1 / 25
About This Presentation
Title:

Earth Science Unit 1.4: Weathering and Soils

Description:

Earth Science Unit 1.4: Weathering and Soils The Rock Cycle Weathering The breakdown of rock near the surface due to surface processes, such as: Chemical Alteration ... – PowerPoint PPT presentation

Number of Views:87
Avg rating:3.0/5.0
Slides: 26
Provided by: Giac1
Category:

less

Transcript and Presenter's Notes

Title: Earth Science Unit 1.4: Weathering and Soils


1
Earth Science Unit 1.4Weathering and Soils
2
The Rock Cycle
3
WeatheringThe breakdown of rock near the surface
due to surface processes, such as
  • Chemical Alteration
  • Solution leaching of water
  • Biological action
  • Hydration
  • Mechanical
  • Impact
  • Wedging Frost, Plant Roots, Salt Crystal
    Growth, Expansion of Hydrated Minerals

4
Weathering Rates
5
Differential Weathering and Erosion
6
Differential Weathering and Erosion
7
Mass-WastingMovement of Large Amounts of
Material Downhill under Gravity
  • Creep
  • Mudflows
  • Slump
  • Rockfalls
  • Avalanches

8
Surface Area and Weathering
9
Spheroidal Weathering
10
Spheroidal Weathering and Exfoliation
11
Spheroidal Weathering
12
Joints and Spheroidal Weathering
13
What Determines Soil Type
  • Climate
  • Vegetation
  • Drainage
  • Time
  • Parent Material
  • Residual - Transported
  • Least Important Factor for Mature Soils

14
Soil Formation Processes
  • Leaching from Surface
  • K, Mg, Na
  • Ca
  • Si
  • Al, Fe
  • Accumulation beneath Surface
  • Al, Fe in Humid Climates
  • Ca in Arid Climates

15
Soil Horizons and Profiles
  • Soil Horizons
  • Layers in Soil
  • Not Deposited, but Zones of Chemical Action
  • Soil Profile
  • Suite of Layers at a Given Locality

16
Principal Soil Horizons
  • O - Organic (Humus) Often Absent
  • A Leaching (Clay Removed)
  • E - Bleached Zone - Only in Certain Soils
  • B Accumulation
  • Absent in Young Soils
  • Distinct in Old Soils
  • Al, Fe, Clay (Moist)
  • Si, Ca (Arid)
  • C - Parent Material (bedrock)

17
Soil Classification
  • This may be the most difficult classification
    problem in science because of the many factors
    involved.
  • Varied Bases for Classification
  • Parent Material
  • Special Constituent Materials
  • Maturity
  • Structure
  • Climate Vegetation
  • Multiple Objectives
  • Scientific
  • Genesis Evolution
  • Agricultural
  • Fertility
  • Most Effective Use
  • Engineering
  • Slope Stability
  • Expansion and Shrinkage
  • Stability of Excavations

18
"The 7th Approximation"
  • U.S. Soil Conservation Service
  • 12 Soil Orders

19
"The 7th Approximation"
Degree of Weathering and B Horizon Development Degree of Weathering and B Horizon Development Degree of Weathering and B Horizon Development Degree of Weathering and B Horizon Development Degree of Weathering and B Horizon Development Degree of Weathering and B Horizon Development
Little Slight Slight Moderate Large Extreme
Entisols Aridisols Aridisols
Inceptisols Inceptisols Alfisols
Spodosols Ultisols
Mollisols Oxisols
Soils Defined by Special Constituent Materials Soils Defined by Special Constituent Materials Soils Defined by Special Constituent Materials Soils Defined by Special Constituent Materials Soils Defined by Special Constituent Materials Soils Defined by Special Constituent Materials
Andisols Andisols Volcanic Ash Volcanic Ash Volcanic Ash Volcanic Ash
Histosols Histosols Peat, Organic Matter Peat, Organic Matter Peat, Organic Matter Peat, Organic Matter
Vertisols Vertisols Self-Mixing Clay Soils Self-Mixing Clay Soils Self-Mixing Clay Soils Self-Mixing Clay Soils
Gelisols Gelisols Soils on Permafrost Soils on Permafrost Soils on Permafrost Soils on Permafrost
20
Soils of the U.S.
21
Typical Soil Profile (Spodosol)
22
Aridisol, Kuwait
23
UltisolsAlabamaTennessee
24
Oxisol, California (a Paleosol)
25
Paleosol, Scotland
Write a Comment
User Comments (0)
About PowerShow.com