Chapter 4: Terrestrial Environment Flashcards

(27 cards)

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

16
Q
Type of soil formation process
Humid environments
Heavy leaching of nutrients 
Characterized by iron oxides
Acidic soils
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
21
Q

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

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
The amount of water retained by the soil between field capacity and wilting point
Available water capacity
25
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
Cation exchange capacity
26
What are the five soil formation processes?
``` Calcification Laterization Salinization Podzolization Gleization ```