SOIL PROFILE Soil genetic horizons HORIZON soil layer
- Slides: 43
SOIL PROFILE
Soil genetic horizons -HORIZON: soil layer parallel to surface with characteristics produced by soilforming processes (based on qualitative judgement)
3 basic soil units (scale) Pedon: smallest volume called a soil Polypedon: soil body (2 or more pedons) in which soils are relatively uniform Soil Series: groups of like polypedons
profile: one side of pedon, showing all horizons; 2 -D
Master horizons O A E B C R
O horizon Organic material Oi slightly decomposed (litter) Oe intermediate decomposition Oa highly decomposed
A horizon § topmost mineral horizon (<12% O. M. ; if clayey: <18% O. M. ) accumulation of well-decomposed O. M. § Often bioturbated § § OR surface horizon disturbed by plowing (Ap)
E horizon § LOSS of § silicate clay, Fe & Al oxides, humus by eluviation § carbonates, gypsum by leaching § lighter color than A § coarser texture than B due to clay loss
LEACHING : removal of soluble minerals (Ca, Mg, Na) in solution ELUVIATION : loss (by water) of suspended materials (clay, humus, oxides) ”emigrating” ILLUVIATION : accumulation of suspended materials (clay, humus, oxides) and/or precipitated materials from solution (Ca, Mg, Na) “immigrating”
B horizon § ACCUMULATED (illuviated ) silicate clay, Fe & Al oxides, carbonates, gypsum, humus § distinguished from A : § stronger, redder, or darker color § OR different texture
C horizon § Mineral horizon (not bedrock) underlying A, E, B horizons § not affected by soil-forming processes § may be parent material
R horizon Consolidated rock
Solum = “true soil”: O, A, E, B
Transitional horizons Zone of transition between master horizons AB A B; A dominates BA A B; B dominates AC A C; A dominates EB E B; E dominates etc….
Mixed horizons One horizon scattered within another horizon B/A mixed A&B; B is matrix for A E/B E is matrix etc….
Numbers after letters Changes within master horizon for which there is no subhorizon designation e. g. , A 1 A 2 for color change within A
Numbers before letters: Lithologic discontinuities e. g. , soil has A, E, B horizon formed on one parent material and a second soil formed on another A E B (1)C 2 B 2 C Most recent soil Buried soil
Subhorizons Lowercase letters symbolizing divisions within master horizons or characteristics of master horizons
Alfisol from field trip; At electrical switching station
some terminology… Colloidal : submicroscopic humus and clay are colloidal Humus: ultimate stage of organic decay predominately protein, gums, lignin Sesquioxides: 1½ oxygens for each Fe, Al sesquioxides of Fe, Al: Fe 2 O 3 Al 2 O 3
- Soil horizons o a e b c r
- Soil horizons
- Soil horizons o a e b c r
- O a e b c r
- Soil horizons
- O a e b c r horizons
- Desert soil composition
- Genetic programming vs genetic algorithm
- Genetic programming vs genetic algorithm
- Genetic drift vs genetic flow
- Founder's effect
- What is the difference between genetic drift and gene flow
- Is topsoil renewable
- What is bedrock
- Food web soil profile
- Difference between silt and clay
- Soil health
- Regolith
- Soil horizon parent material
- Pie chart of soil components
- Shear strength of soil ppt
- Soil layers
- Chemical digestion
- Layer-by-layer assembly
- Secure socket layer and transport layer security
- Secure socket layer and transport layer security
- Layer 2 vs layer 3 bitstream
- Secure socket layer and transport layer security
- Layer 6 presentation layer
- Layer 2 e layer 3
- Pigmented layer and neural layer
- Secure socket layer and transport layer security
- Brown earth soil ireland
- Soil profile
- Regolith in soil profile
- Brown earth soil profile
- Soil profile
- Clay soil profile
- Gley soil higher geography
- Latosol soil
- Red latosols
- What is the
- Soil profile is a vertical cross section
- Weathering