Soils: Composition & properties Flashcards

1
Q

Soil forming factors

A
climate, 
parent material, 
topography, 
biology, 
time
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2
Q

Soil water important for

A
  • soil fauna and flora
  • surface flora
  • maintaining good soil structure
  • influence on temperature
  • transport
  • medium for chemical reactions
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3
Q

Volume of solution depends on

A
  • total volume of pore space

- shape and size

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4
Q

Saturation point

A

all size pores full

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5
Q

Field capacity

A

pores 0.05mm and less are full

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6
Q

permanent wilting point

A

pores 0.001mm and less are full

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7
Q

Soil pores are created by:

A
  • wetting and drying of soil
  • freeze-thaw
  • roots
  • soil fauna
  • spaces between sand, silt and clay and organic matter particles
  • spaces within organic matter clay
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8
Q

Soil solution

A

contains all 18 essential nutrients for plant growth

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9
Q

Alkalinity and Acidity

A
  • chemical and biological reactions dependent on pH levels

- influence solubility and availability of some essential nutrients

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10
Q

Soil Air influences

A
  • soil organisms
  • biochemical activity and chemical reactions
  • soil structure and temperature
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11
Q

Water and air in soils is influenced by

A
  • pore size
  • pore shape
  • connectivity between pores
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12
Q

Leaching

A
  • water infiltration > evapotranspiration
  • physical movement of material down profile by water
  • often associated with frequent wetting and drying
  • movement of material in solution down profile
  • deposition in lower horizons
  • loss to groundwater
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13
Q

Salinity

A
  • accumulation of salts near surface
  • salts form groundwater, irrigation water or soil
  • irrigation raises ground water table and plants increase evapotranspiration
  • salts
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14
Q

Salts

A
  • toxic to plants
  • make water uptake difficult
  • make soil very alkaline
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15
Q

Sodicity

A
  • often associated with salinity but different process
  • if salts contain lots of sodium (Na)
  • Na replaces Ca in between clay lamellae (plates)
  • 2 Na for every 1 Ca
  • Na attracts much more water. water flows between eh lamellae
  • lamellae forced apart
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16
Q

Sodicity 2

A
  • soil weak and breaks down easily
  • pores filled
  • ‘concrete’ when dry ‘porridge’ when wet
  • poor rooting, aeration and drainage
  • crust at surface
17
Q

Gleying

A
  • permanently/temp waterlogged
  • produced gleyed soil
  • blue/grey when wet, mottled when dry
  • caused by reduction of iron oxides by bacteria to obtain oxygen
  • mottles caused by concentration of oxides and oxidation
18
Q

Soil Air

A
  • as soil dries out, pore space becomes occupied by soil air
  • soil air may be in contact with the atmosphere or isolated by water
  • soil organisms usually breath oxygen and produce carbon dioxide (roots)
  • soil carbon dioxide concentration can be 100 times greater than in atmosphere
19
Q

Soil Air 2

A
  • when soils become flooded, air gets trapped in the soil pores
  • this leads to large increases in the amount of CO2 in the soil
  • air can escape form flooded soil through diffusion, mass flow or bubbling
  • carbon dioxide dissolved in water produces carbonic acid, lowering the soil pH