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Plants obtain from soil:
- Physical support
- Air
- Water
- Temperature regulation
- Protection
- Nutrient elements (17 essential elements)
Root respiration
- Produce CO2
- Release O2
(ventilation in soil pores)
Macronutrients (8)
- Calcium (Ca)
- Magnesium (Mg)
- Nitrogen (N)
- Potassium (K)
- Phosphorous (P)
- Carbon (C)
- Hydrogen (H)
- Oxygen (O)
- Sulfur (S)
Micronutrients (8)
- Copper (Cu)
- Iron (Fe)
- Manganese (Mn)
- Nickel (Ni)
- Zinc (Zn)
- Boron (B)
- Chlorine (Cl)
- Molybdenum (M)
Humus
organic component of soil
pedosphere
soil environment/interface
lithosphere
rock environment
regolith
a layer of unconsolidated debris overlying hard, unweathered rock
(ABC horizons; C horizons contain bulk rock material - above bedrock)
Sparolite
underlying rock has weathered in place to the degree that is loose enough to be dug
Soil Profile
a vertical section exposing a set of soil horizons
O Horizon
organic material layer at the soil surface
A Horizon
also called top soil, is the layer nearest the surface and is dominated by mineral particles and accumulated organic matter
Plow layer
formed by plowing and cultivating a soil to homogenize and modifies the upper 12 to 25 cm
E Horizon
usually just below the A horizon, intensely weathered and leached horizon that hasn't accumulated organic matter
B Horizon
also called subsoil;
- contain less organic material
- varying amounts of silicate clays, iron and aluminum oxides, gypsum, or calcium carbonate
- plant roots and microorganisms often extend below
C Horizon
are the least weathered part of the soil profile
Major components of a typical, moist soil
- 20-30% Air
- 20-30% Water
^pore space^
- 40-60% Minerals
- 1-5% Organic Matter
^Soil Solids^
% by volume
Three Mineral properties
- Sand (2-0.05mm)
- Silt (0.05-0.002mm)
- Clay (<0.002mm)
- Colloidal properties of clay (<0.001mm)
Soil Texture
12 soil textures
- Clay
- Sandy Clay
- Sandy Clay Loam
- Clay Loam
- Sand Loam
- Loamy Sand
- Sand
- Loam
- Silty Clay Loam
- Silty Clay
- Silt Loam
- Silt
Soil
Dynamic natural body having properties due to the combined effects of climate and biota as modified by relief acting on parent material over time.
5 things that affect soil
Active:
-climate
-biota
Passive:
-parent material
-time
Modifying:
-relief (topography)
Organic matter
- binds mineral particles into a granular soil structure that is responsible for loose, easily managed, productive soil
- increase the amount of water a soil can hold
- major source of P, S, N for plants
Humus
- black or brown in color
- a collection of very complex organic matter
- is the colloidal fraction of soil organic matter
- g for g, holds nutrients and
water < clay
- increase soil's capacity to promote plant growth
Soil gases
CO2 > O2
Diffusion
a measure of air movement due to differences in partial pressure of individual gases
Hydroscopic water
water which is held so tightly to silicate surfaces that it cannot move as a liquid
Typical structure description:
grade, size, type
hue
redness or yellowness
value
lightness or darkness
chroma
intensity of brightness