The Dynamics of Soil: Formation, Properties, and Influences

 
Introduction to Soils
 
Kristen Manies (US Geological Survey)
Lee Pruett (Notre Dame High School)
Jennifer Harden (US Geological Survey)
 
What is soil?
 
 
 
Often defined one of several
ways:
   
Utilitarian
   
Ecological
   
Pedologic
 
Utilitarian
 
defined by the properties important to
agriculture, engineering, etc. (soil material)
 
Ecological
 
medium capable of supporting plants both
physically and through the transfer of water
and nutrients (soil medium)
 
Pedologic
 
Formation of 
soil by processes 
such as
weathering, organic matter accumulation ,and
leaching (soil as a system)
 
 
Processes that Form Soils and
Influence Soil Properties
 
The movement of water down through the
soil profile (leaching)
Organic matter accumulation (sequesters
carbon)
Mineral weathering
Mineral formation
Many Others
 
 
Services by the Soil System
 
Food
Fiber
Filtration of gas & water
Water storage
Carbon Storage
 
Threats to Soils Include:
 
 
Erosion
Contamination
Sealing
Compaction
Loss of biodiversity
Salinization
Floods and Landslides
 
Soils are dynamic,
they change over time
 
As soils age, they form distinct
soil
 horizons 
and a soil
 profile
 
topsoil
 
subsoil
 
parent material
 
Ultimately, soils are influenced by their environment
 
If you add time, then you get the soil
forming factors:  
CLORPT
 
Cl
imate
O
rganisms
R
elief
P
arent material
T
ime
 
The Role of Climate
 
The balance between moisture and temperature is
particularly important to the development of soils.
 
MOISTURE
how much
when
 
TEMPERATURE
season length
range of highs/lows
 
Houston, TX
 
Houston soil
 
Gainsville, AL
 
Bama soil
 
(Casa Grande soil
From Arizona)
 
(Orovada soil
from Nevada)
 
In summary
 
Dark topsoil:
lots of plant
material
 
Red subsoil:
weathering
and oxidation
 
Complex subsoil:
Lots of time to
differentiate horizons
 
Soil profiles reflect the conditions
under which they formed.
 
Extension slides
 
The Role of 
P
arent Material
 
(Arizona)
 
Material from which soil forms:
bedrock
colluviam (sediments transported via gravity to the base of a slope)
alluvium (loose, eroded soil)
loess (windblown material)
 
Parent material influences
mineral composition
 and
particle size
 of soil.
 
Smaller, finer particles
(like clay)
hold water and
nutrients,
including carbon
 
Coarser particles
don’t hold water or nutrients,
 but they promote oxidation
 
Particle size
 
(Arizona)
 
Linking 
topsoil
 to 
P
arent material
Light brown
 
 
Darker brown
 
 
Linking 
subsoil
 to 
P
arent material
Oxidized, red and
yellow
 
 
Reduced, green
and grey
 
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Soil, the foundation of life on Earth, is a complex system influenced by various factors such as utilitarian, ecological, and pedologic processes. This introduction covers the definition of soil, its importance in agriculture and ecosystems, the formation processes, services provided by soils, threats they face, their dynamic nature over time, and how they are shaped by environmental factors.

  • Soil Dynamics
  • Soil Formation
  • Ecological Systems
  • Environmental Influences
  • Soil Services

Uploaded on May 16, 2024 | 1 Views


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  1. Introduction to Soils Kristen Manies (US Geological Survey) Lee Pruett (Notre Dame High School) Jennifer Harden (US Geological Survey)

  2. What is soil? Often defined one of several ways: Utilitarian Ecological Pedologic

  3. Utilitarian defined by the properties important to agriculture, engineering, etc. (soil material)

  4. Ecological medium capable of supporting plants both physically and through the transfer of water and nutrients (soil medium)

  5. Pedologic Formation of soil by processes such as weathering, organic matter accumulation ,and leaching (soil as a system)

  6. Processes that Form Soils and Influence Soil Properties The movement of water down through the soil profile (leaching) Organic matter accumulation (sequesters carbon) Mineral weathering Mineral formation Many Others

  7. Services by the Soil System Food Fiber Filtration of gas & water Water storage Carbon Storage

  8. Threats to Soils Include: Erosion Contamination Sealing Compaction Loss of biodiversity Salinization Floods and Landslides

  9. Soils are dynamic, they change over time Time Parent material Young soil Mature soil Old soil

  10. As soils age, they form distinct soil horizons and a soil profile topsoil subsoil parent material

  11. Ultimately, soils are influenced by their environment Relief Climate Organisms Humans Bacteria Parent material Fungi Vegetation

  12. If you add time, then you get the soil forming factors: CLORPT Climate Organisms Relief Parent material Time

  13. The Role of Climate The balance between moisture and temperature is particularly important to the development of soils. MOISTURE how much when TEMPERATURE season length range of highs/lows

  14. Houston, TX 90 8 Temperature 80 7 Rainfall 70 6 Precipitation (in.) Temperature ( F) 60 5 50 4 40 3 Period of high rainfall also has high temperature 30 2 20 1 10 0 0

  15. High rainfall during warm temperatures Water used by plants Lots of plant growth Darker topsoil Houston soil

  16. Gainsville, AL 90 7 80 6 70 Precipitation (in.) Temperature ( F) 5 60 4 50 40 3 30 2 Period of high rainfall during lower temperatures Temperature 20 1 Rainfall 10 0 0

  17. High rainfall during cooler temperatures Few plants to use water Excess water leaches through the soil Red/orange subsoil Bama soil

  18. Low rainfall Little vegetation Little water reaches subsoil Low plant growth Salts accumulate Thin, light colored topsoil White subsoil (Orovada soil from Nevada) (Casa Grande soil From Arizona)

  19. In summary Soil profiles reflect the conditions under which they formed. Dark topsoil: lots of plant material Red subsoil: weathering and oxidation Complex subsoil: Lots of time to differentiate horizons

  20. Extension slides

  21. The Role of Parent Material Material from which soil forms: bedrock colluviam (sediments transported via gravity to the base of a slope) alluvium (loose, eroded soil) loess (windblown material) Parent material influences mineral composition and particle size of soil. (Arizona)

  22. Particle size Smaller, finer particles (like clay) hold water and nutrients, including carbon Coarser particles don t hold water or nutrients, but they promote oxidation (Arizona)

  23. Linking topsoil to Parent material Coarse Fine Organic matter stays in the soil Organic matter more readily decomposed Darker brown Light brown

  24. Linking subsoil to Parent material Coarse Fine Weathering products remain in subsoil as salts Water allows weathering and chemical transport Oxidized, red and Reduced, green and grey yellow

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