Upload
lundy
View
490
Download
71
Embed Size (px)
DESCRIPTION
Soil Taxonomy- Properties of Soil. Plant & Soil Science. Property #1: Soil has Horizons (layers). Property #2: Soil has Color…. Property #3: pH Levels. Soil Property #4 - Organic Content. Desert soils have low organic content. Grasslands have high organic content. - PowerPoint PPT Presentation
Citation preview
Soil Taxonomy- Properties of Soil
Plant & Soil Science
Property #1: Soil has Horizons (layers)
Property #2: Soil has Color…
Property #3: pH Levels
Soil Property #4 - Organic Content Desert soils have low
organic content. Grasslands have high
organic content.
The exact type of vegetation is also important because it also affects pH.
Pine needles add acid to the soil.
Grasses conserve calcium and magnesium (bases).
Most crops like a neutral pH.
Order
Soil Taxonomy- 12 Soil Orders
Soils are classified into into six categories based on diagnostic characteristics
The last (largest) category will place the soils into one of the 12 Soil Orders.
Soil Taxonomy
1) Orders (12)2) Suborders (54)3) Great Groups (211)4) Subgroups (1,100+)5) Family (7,000+)6) Series (a lot!)
Fine-loamy mixed, superactive, mesic Aquic Argiudolls(This is the name of a specific soil in Soil Taxonomy)
This is the name of oneOf the 12 large categories
Mollisol - oll
Oder - root of order
Orders
Highest and most general of the soil classification system (similar to the phylum in plant taxonomy)
Based on conditions under which the soil developed
Fine-loamy mixed, superactive, mesic Aquic Argiudolls
Orderoll = Mollisols
Suborders
Grouped by similarities in soil formation such as wetter/dryer soil, colder/warmer soil, etc.
Fine-loamy mixed, superactive, mesic Aquic Argiudolls
SubOrder
Order
Ud = Udic Moisture
Great Groups (not required to know)
Based on differences between soil horizons
Fine-loamy mixed, superactive, mesic Aquic Argiudolls
GreatGroup
SubOrder
Order
Argi = Clay accumulation
Sub Groups (not required to know)
Describes a profile characteristic, wetness, sand, etc.
GreatGroup
Fine-loamy mixed, superactive, mesic Aquic Argiudolls
SubGroup
SubOrder
Order
Aquic = wet soil
Family (not required to know)
Based on soil properties that affect management and root penetration, such as texture, temperature, and depth
GreatGroup
Fine-loamy, mixed, superactive, mesic Aquic Argiudolls
FamilySubGroup
SubOrder
OrderTexture, clay minerals, CEC, temp,
Series (not required to know)
Named from the town or landscape feature near where the soil was first recognized (Eleva= Eleva, WI or Gale for Galesville, WI .)
GreatGroup
Fine-loamy mixed, superactive, mesic Aquic Argiudolls
FamilySubGroup
SubOrder
Order
Soil Orders – Upper Midwest
12 Soil Orders - Each Order has a diagnostic epipedon and subsurface horizons – which could be “none”.
WEB SITE for soil orders = www.mines.uidaho.edu/pses/teach_res
Entisol Inceptisol Andisols Spodosols Mollisols Alfisols Ultisols Oxisols Aridisols Vertisols Histosols Gelisols
The 12 Soil Orders
Orders with unique parent materials:
Andisols (and)
Volcanic ash soils.
Histosols (ist)
Organic soils.
Vertisols (ert)
High shrink/swell clay soils.
Orders formed in unique environments.
Aridisols (id)
Arid climates. CaCO3 accumulation
in subsoil.
Gelisols (el)
Colder climates. Permafrost layer
within 2 m of surface.
Oxisols (ox)
Tropics and subtropics.
Intensely weathered.
Orders by age.
Entisols (ent)
‘Baby’ soil. Little to no
morphological development.
Inceptisols (ept)
‘Toddler’ soils. Weakly developed
sub-surface horizons.
Ultisols (ult)
Older soils. “Ultimately
weathered”. Strongly leached. Sub-surface clay
accumulation. < 35% base sat. in
sub-soil.
Orders developed under unique vegetative ecosystems.
Alfisols (alf)
Forest soils. Usually an A-E-B
type horizon development.
The A horizon is usually less than 25 cm.
Mollisols (oll)
Grasslands soil. Thick, dark A
horizon. High % base
saturation.
Spodosols (od)
Acid forest soils. Usually sandy. Thick, bright white E
horizon. Sub-surface layer of
accumulated metal-humus complex (Bhs and Bs horizons).
Summary:
3 orders with unique parent materials (Andisols, Histisols, Vertisols).
3 orders with unique environments (Aridisols, Gelisols, Oxisols).
3 orders by age of development (Entisols, Inceptisols, Ultisols).
3 orders by unique vegetative influence (Alfisols, Mollisols, Spodosols).
Resources
http://soils.usda.gov/technical/soil_orders/ http://www.soils4teachers.org/lessons-and-ac
tivities http://www.cals.uidaho.edu/soilorders/orders.
htm