Soil Temperature Flashcards

1
Q

Why is soil temperature so important

A
  • optimum for root growth and germination
  • freeze / thaw action alters soil structure
  • chemical and biological rates are low in could soils; availability of nutrients; decomposition
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2
Q

Definition of temperature

A

Measure of kinetic energy of individual

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3
Q

Definition of heat

A

Represents transfer of energy from one body to another, due to the difference in temperature

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4
Q

How does heat transfer

A

Conduction ( through molecular collisions)

Convection ( byass movement of molecules)

Radiation ( by electromagnetic waves )

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5
Q

Couriers law of hear conduction

A

G = thermal conductivity * temperature gradient

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6
Q

Definition of thermal conductivity

A

Heat flow in response to a temperature gradient

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7
Q

What is the thermal conductivity

A

As water content increases –> air content decreases –> transfer resistance lowered –> lambda increases

Leaf mulch has low lambda

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8
Q

Heat conduction of soil and air

A

Water is good conductor

Air is a poor conductor

  • dry soil is a good insulator
  • heat conduction is slow –> changes in subsoil temperature lag behind surface temperature
  • temperature changes less in subsoil
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9
Q

Definition of specific heat of soils

A

Amount of energy required to raise the temperature of a substance by 1 degree dlon a unit mass basis

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10
Q

Specific heat of soil and air

A

Water has high heat capacity
Air has low heat capacity

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11
Q

Heat capacity of water and air

A

Water has high heat capacity

Air has low heat capacity

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12
Q

Definition of heat of vaporization

A

Evaporation of water from the soil surface required a large amount of energy

Energy comes from soil radiation and surrounding soil -> has the potential cool the soil

Low temperature of wet soil in the day in the spring / summer –> due to evaporation and specific heat ( in spring -> wet would are 3 to 6 degrees cooler than dry soils )

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13
Q

How does soil temperature vary with depth?

A
  • surface layer temperature varies according to air temperature –> usually warmer than air
  • subsoil temperature lags behind changes in the surface temperature -+> warmer in winter and cooler in summer than surface –> not affected directly by solar radiation
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14
Q

List 2 to 3 different ways you can control soil temperature

A

Organic mulch buffers extremes in temperatures
- in hot weather –> keep surface soil cooler
- in cold weather –> moderate rapid temperature decrease

Organic mulch and plant residues
- conservation tillage –> leave residue at surface –> cooler soils in July / Aug
- low temperature in May / June –> may decrease germination
- decrease evaporation of water

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15
Q

Describe how plastic mulch work

A

Increase soil temperature –> good in spring; root growth may decrease in summer

  • use for water management and weed control
  • gardens, high value crops –> can extend the growing season and hasten growth
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16
Q

Describe moisture control for soil temperature control

A

Wet would in spring are 3 to 6 degrees cooler than dry soils
- control methods:
-install drainage system
- ridge the soil