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30 Cards in this Set

  • Front
  • Back

Conversion of nutrients from organic to mineral (inorganic) form

Mineralization

Vertical movement of water due to gravitational forces

Percolation

Water so tightly held by the charges in the soil that is is unavailable to plants

Hygroscopic water

Fine textured soils will have a

High buffering capacity - more surface area for more cation exchange capacity, more sites allows for less effect by things like leaching

Nitrogen fixing bacteria that has a mutualistic relationship with Fabaceae

Rhizobia

When new leaves are green and old leaves are yellow

Nitrogen deficiency

When nutrients get tied up in organic form

Immobilization

Nitrogen's form when available to plants

Nitrate

Ability for a soil to resist pH change or nutrient loss during leaching

Buffering capacity

Part of the chlorophyll molecule

Nitrogen, magnesium

Nitrogen fixing bacteria that has a relationship with alder

Frankia

Small charged particles in soil water

Colloids

New leaves have interveinal chlorosis, old leaves are fine

Iron deficiency

Water movement in micropores of soil

Capillary action

Fine textured soils layered over coarse

Perched water table

Nitrogen lost to the atmosphere

Denitrification

Nitrogen

Protein (amino acids), mobile, promotes growth, deficiency: yellowing of older and all leaves, part of chlorophyll molecule

What are the primary macronutrients?

Nitrogen, phosphorous, potassium (NPK)

What are the secondary macronutrients?

Calcium, Magnesium, Sulphur

What is the unavailable form of nitrogen?

Nitrites (NO2-)

Phosphorous

Essential for growth, in every living cell, root development and flowering, can tie up iron, deficiency: leaves reddening

How do micro organisms help soil?

Nutrient cycling (carbon, nitrogen cycle), food chain, soil structure

Two types of (bacteria) parasites: pathogens and mutualists. Give an example of each

Pathogen: negatively affects host, example: powdery mildew, rust, black spot


Mutualistic: mycorrhizal fungi

What are decomposers called?

Saprophytes

Compost: Carbon:nitrogen ratio too high...

C:N too high —> bacteria doesn't have enough nitrogen, composting slows down, compost will be cold

Composting: C:N too low

C:N too low —> excess nitrogen will be lost to atmosphere as ammonia gas, pile will stink like ammonia

Compost: moisture levels too low

(35-40% is too low). Bacteria decomposition will stop at 15%, well functioning pile will dry out due to evaporation

Composting: moisture too high

(60% too high). Pile becomes anaerobic, decomposition is slow, nutrients are leached from soil, smelly

Compost: oxygen too high

Materials may combust, dry out if not irrigated

Compost: oxygen too low

Will decompose, but take a very long time