Ch. 5 Roots Part 3 Flashcards
Describe 3 soil components from largest to smallest
sand –> silt –> clay in soil
Describe soil pH
Extreme pH can kill mycorrhizae
* Acidity inhibits growth of nitrogen-fixing bacteria
* Counteract by adding calcium or magnesium compounds
o Example: liming
Affects nutrient availability
Alkalinity causes some mineral to become less available
* Example: copper, iron, manganese
Counteracted by sulfur
* Converted to sulfuric acid by bacteria
Counteracted by adding nitrogenous fertilizers
Describe the human relevance of roots
o Roots Human Relevance
Food
* Carrots, beets, turnips, sweet potatoes
Spices
* Sassafras, licorice
Dyes
Drugs
* Aconite, ipecac, gentian
Insecticide
* Rotenone
Soil
Formed through interaction of climate, parent material, topography, vegetation, living organism, and time
Solid portion of soil consists of minerals and organic matter
Pore spaces: fill with air or water, between solid particles
Describe soil climate
- Varies around globe, effects weathering of rocks
- Desert: little weathering by rain, soil poorly developed
- Moderate rainfall: well-developed soils
- High rainfall: excessive water flow through soil leaches out important materials
Describe interactions between soil living organisms and organic composition
- Organisms, roots, and other plant parts
- Bacteria and fungi decompose material from dead materials (plants, animals, etc.)
- Roots produce carbon dioxide, combines with water to form acid and increases mineral dissolve rate
Humus in soil
small animals alter soil through activity and waste
Humus
partially decomposed organic matter, gives soil dark color
o Holds minerals and water like sponge
o Plants have less limitations, better environment
Topography for soil
- Steep areas: soil may erode (wind, water, ice)
- Flat, poorly drained areas: pools/ponds disappear, negative soil development
- Ideal topography: permits drainage without erosion!
Soil Texture and mineral composition
relative proportion of sand, silt, and clay in soil
o Sand: many small particles bound together chemically
o Silt: particles too small to be seen without microscope
o Clay: only seen with electron microscope
Field capacity
water remaining in soil after water drains way by gravity
* Determined by soil texture, structure, organic content of soil
Permanent wilting point
rate of water absorption insufficient for plant needs
Available water
soil water between field capacity and the permanent wilting point