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30 Cards in this Set
- Front
- Back
Conversion of nutrients from organic to mineral (inorganic) form |
Mineralization |
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Vertical movement of water due to gravitational forces |
Percolation |
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Water so tightly held by the charges in the soil that is is unavailable to plants |
Hygroscopic water |
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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 |
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Nitrogen fixing bacteria that has a mutualistic relationship with Fabaceae |
Rhizobia |
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When new leaves are green and old leaves are yellow |
Nitrogen deficiency |
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When nutrients get tied up in organic form |
Immobilization |
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Nitrogen's form when available to plants |
Nitrate |
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Ability for a soil to resist pH change or nutrient loss during leaching |
Buffering capacity |
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Part of the chlorophyll molecule |
Nitrogen, magnesium |
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Nitrogen fixing bacteria that has a relationship with alder |
Frankia |
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Small charged particles in soil water |
Colloids |
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New leaves have interveinal chlorosis, old leaves are fine |
Iron deficiency |
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Water movement in micropores of soil |
Capillary action |
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Fine textured soils layered over coarse |
Perched water table |
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Nitrogen lost to the atmosphere |
Denitrification |
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Nitrogen |
Protein (amino acids), mobile, promotes growth, deficiency: yellowing of older and all leaves, part of chlorophyll molecule |
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What are the primary macronutrients? |
Nitrogen, phosphorous, potassium (NPK) |
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What are the secondary macronutrients? |
Calcium, Magnesium, Sulphur |
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What is the unavailable form of nitrogen? |
Nitrites (NO2-) |
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Phosphorous |
Essential for growth, in every living cell, root development and flowering, can tie up iron, deficiency: leaves reddening |
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How do micro organisms help soil? |
Nutrient cycling (carbon, nitrogen cycle), food chain, soil structure |
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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 |
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What are decomposers called? |
Saprophytes |
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Compost: Carbon:nitrogen ratio too high... |
C:N too high —> bacteria doesn't have enough nitrogen, composting slows down, compost will be cold |
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Composting: C:N too low |
C:N too low —> excess nitrogen will be lost to atmosphere as ammonia gas, pile will stink like ammonia |
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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 |
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Composting: moisture too high |
(60% too high). Pile becomes anaerobic, decomposition is slow, nutrients are leached from soil, smelly |
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Compost: oxygen too high |
Materials may combust, dry out if not irrigated |
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Compost: oxygen too low |
Will decompose, but take a very long time |