Chapter 4: Terrestrial Environment Flashcards

0
Q

How do you calculate leaf area index?

A

Area of leaf over ground area

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1
Q

How much light reaches the forest floor?

A

1-5%

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2
Q

Pigment that allows plant to detect shading

There are increased amounts in shaded plants

A

Phytochrome

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3
Q

Why is soil important?

A

Medium for plant growth
Controls water levels
Decomposition and recycling
Important habitat

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4
Q

Unconsolidated mineral and organic maggot over unweathered rock

A

Soil

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5
Q

Destruction of rock material into smaller particles

A

Weathering

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6
Q

What are types of weathering?

A

Mechanical

Chemical

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7
Q

How is soil formed?

A
Parent material
Biotic factors
Climate
Topography
Time
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8
Q

Type of soil formation

Undifferentiated material from which soil develops

A

Parent material

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9
Q

Type of soil formation including the decomposition of organic matter and the ability of plant roots to hold soil in place

A

Biotic factors

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10
Q

Type of soil formation
Temperature, precipitation, and wind
Maximized at warm and wet conditions

A

Climate

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11
Q

Type of soil formation
Sloped causes more erosion
Soil affected by exposure to solar radiation and wind

A

Topography

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12
Q

Type of soil formation

Well devolved soil between 2,000 and 20,000

A

Time

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13
Q

Name the horizons from surface to deep

A
Organic
Topsoil
Subsoil
Rock fragments
Bedrock
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14
Q

To wash out (in soil horizons)

In the E horizon of the topsoil

A

Elluviation

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15
Q

To wash in; deposits (soil horizons)

In the subsoil

A

Illuviation

16
Q
Type of soil formation process
Humid environments
Heavy leaching of nutrients 
Characterized by iron oxides
Acidic soils
A

Laterization

17
Q
Type of soil formation
Water loss exceeds precipitation
Water taken up by plants 
Calcium carbonates build up
Deposition and build up of alkaline salts in subsoil 
B horizon looks white from calcium
A

Calcification

18
Q

Type of soil formation process
Dry climates and coastal regions from salt spray
Salt deposits near surface

A

Salinitization

19
Q

Type of soil formation
Coolly, moist climate
Acidic soil enhances leaching of cations (Fe & Al) from topsoil
Spodosols formed

A

Podzolization

20
Q
Type of soil formation process 
High rainfall or poor drainage 
Slow decomposition of organic matter
Accumulates in upper layers
Gleisol formed
A

Gleization

21
Q

More water than the pore space can hold and excess water drains freely from the soil

A

Saturated

22
Q

If water fills all of the pore spaces and is held there by capillary forces

A

Field capacity

23
Q

Water held between soil particles by capillary forces

A

Capillary water

24
Q

The amount of water retained by the soil between field capacity and wilting point

A

Available water capacity

25
Q

The total number of negatively charged sites, located on the edge of clay particles and soil organic matter
Negatively charges enable a soil to prevent leaching of positively charged nutrient cations

A

Cation exchange capacity

26
Q

What are the five soil formation processes?

A
Calcification
Laterization
Salinization
Podzolization
Gleization