Soil Flashcards
Fulvic acids
organic acids found in soils derived from organic matter decomposition
- smaller than humic acids, soluble in water, more OH and COO- groups
- strong chelating agents, determine soil acidity
4 functions of soil
plant growth medium
water storage, supply, and purification
modifier of the atmosphere
habitat for organisms (decomposers)
Soil water
mediates organic and inorganic components with microbes
- site of redox, acid-base reactions
Clay
<2um
- site of chemical reactions in soil
Sand
20-200um
Silt
2-20 um
Loam
mixture of silt, sand, and clay
- high nutrients, moisture, and humus
Formation of soil
CLORPT
Climate
Topography (Relief)
Organisms
Parent Material
Time
Colloids
clay particles, mixture that has particles between 1-1000um, evenly distributed
Koalinite
hexagonal sheets, clay mineral
cation exchange capacity
capacity for soil to exchange nutrients with plants
- important for farming
- determined by amount of clay and/or humus present
(meq/100g dry soil)
humic acids
larger, fewer COOHs, soluble in bases (not water) because they become deprotonated
liming
adding CaCO3 to soils to partially neutralize soil acids
Kow
octanol-water partition coefficient
- high Kow = deposit in sediments rather than water and bioaccumulate
- hydrophobic (and/or very large) organic substances
chelation
“binding” of heavy metals onto folic acids