Ch. 5 Roots Part 3 Flashcards

1
Q

Describe 3 soil components from largest to smallest

A

sand –> silt –> clay in soil

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2
Q

Describe soil pH

A

 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

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3
Q

Describe the human relevance of roots

A

o Roots Human Relevance
 Food
* Carrots, beets, turnips, sweet potatoes
 Spices
* Sassafras, licorice
 Dyes
 Drugs
* Aconite, ipecac, gentian
 Insecticide
* Rotenone

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4
Q

Soil

A

 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

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5
Q

Describe soil climate

A
  • 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
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6
Q

Describe interactions between soil living organisms and organic composition

A
  • 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

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7
Q

Humus

A

partially decomposed organic matter, gives soil dark color
o Holds minerals and water like sponge
o Plants have less limitations, better environment

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8
Q

Topography for soil

A
  • Steep areas: soil may erode (wind, water, ice)
  • Flat, poorly drained areas: pools/ponds disappear, negative soil development
  • Ideal topography: permits drainage without erosion!
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9
Q

Soil Texture and mineral composition

A

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

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10
Q

Field capacity

A

water remaining in soil after water drains way by gravity
* Determined by soil texture, structure, organic content of soil

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11
Q

Permanent wilting point

A

rate of water absorption insufficient for plant needs

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12
Q

Available water

A

soil water between field capacity and the permanent wilting point

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