3 - Biosphere Flashcards

1
Q

BROWN EARTH: HUMUS LAYER

A

Thick mull humus layer

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2
Q

BROWN EARTH: A HORIZON

A

dark brown enriched A horizon

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3
Q

BROWN EARTH: B HORIZON

A

Lighter brown B horizon

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4
Q

BROWN EARTH: C HORIZON

A

Weathered parent material

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5
Q

BROWN EARTH:VEGETATION COVER

A

Deciduous woodland with a layer of undergrowth and long tree roots

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6
Q

BROWN EARTH:SOIL BIOTA

A

Abundant soil biota

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7
Q

HOW DOES VEGETATION AFFECT BROWN EARTH FORMATION?

A

deciduous forests provide deep leaf litter and deep roots that recycle nutrients from deep into the soil.

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8
Q

HOW DOES SOIL BIOTA AFFECT BROWN EARTH FORMATION?

A

abundant soil biota leads to good mixing and aerating of thesoil resulting in poorly defined horizons.

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9
Q

HOW DOES TOPOGRAPHY AFFECT BROWN EARTH FORMATION?

A

Tend to be found on gentler slopes that allow the formation of thick soils.

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10
Q

HOW DOES CLIMATE AFFECT BROWN EARTH FORMATION?

A

precipitation slightly exceeds evaporation resulting in a small amount of downward leaching.

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11
Q

HOW DOES HUMIFICATION AFFECT BROWN EARTH FORMATION?

A

mild/ warmer climate rapidly breaks down organic matter into a mull humus providing a rich dark colour.

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12
Q

HOW DOES TRANSLOCATION AFFECT BROWN EARTH FORMATION?

A

B horizon is lighter in colour as limited leaching has taken place and an absence of nutrient rich humus.

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13
Q

PODZOL: HUMUS LAYER

A

Thin black mor humus

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14
Q

PODZOL: A HORIZON

A

Top stained darker by humus, ash grey eluviated layer

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15
Q

PODZOL: B HORIZON

A

reddish brown B horizon with iron pan

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16
Q

PODZOL: C HORIZON

A

Weathered parent material

17
Q

PODZOL: VEGETATION COVER

A

coniferous forest, heather moorland with thin undergrowth of mosses and lichens

18
Q

PODZOL: SOIL BIOTA

A

lack of soil biota

19
Q

HOW DOES VEGETATION AFFECT PODZOL FORMATION?

A

coniferous needles and cones produce an acidic mor humus whilst shallow roots limit absorption of deep leached minerals and nutrient recycling.

20
Q

HOW DOES SOIL BIOTA AFFECT PODZOL FORMATION?

A

limited soil biota leads to well defined horizons.

21
Q

HOW DOES TOPOGRAPHY AFFECT PODZOL FORMATION?

A

found on steeper slopes that encourages leach through the soil.

22
Q

HOW DOES HUMIFICATION AFFECT PODZOL FORMATION?

A

low temperatures cause a slow rate of decomposition.

23
Q

HOW DOES TRANSLOCATION AFFECT PODZOL FORMATION?

A

high precipitation leads to the leaching of aluminium and iron oxides. This creates an iron pan between the A/B horizons and may cause waterlogging.

24
Q

HOW DOES ELUVIATION AND ILLUVIATION AFFECT PODZOL FORMATION?

A

Eluviation leaves an ash grey A horizon. ​
Illuviation leads to a reddish brown B horizon

25
GLEY: HUMUS LAYER
Thin black mor humus
26
GLEY: A HORIZON
darker brown/grey A horizon (peat may form)
27
GLEY: B HORIZON
Blue/grey B horizon
28
GLEY: C HORIZON
Impermeable parent material
29
GLEY: VEGETATION COVER
shrubs, grasses and rushes with undergrowth of mosses and lichens
30
GLEY: SOIL BIOTA
Anaerobic conditions so little biota
31
HOW DOES VEGETATION AFFECT GLEY FORMATION?
limited vegetation produces a thin layer of acidic mor humus and shallow roots limit the recycling of minerals.
32
HOW DOES SOIL BIOTA AFFECT GLEY FORMATION?
low temperatures mean few organisms can survive which reduces mixing in the soil causing clearly defined layers. 
33
HOW DOES TOPOGRAPHY AFFECT GLEY FORMATION?
found on flatter ground that results in drainage problems.
34
HOW DOES WEATHERING AFFECT GLEY FORMATION?
freeze-thaw takes place causing large chunks of angular rock to be brought up to the A and B horizons.
35
HOW DOES HUMIFICATION AFFECT GLEY FORMATION?
low temperatures cause a slow rate of decomposition.
36
HOW DOES WATERLOGGING AFFECT GLEY FORMATION?
heavy precipitation and snow melt creates anaerobic conditions and a blue/grey colour due to gleying. If soils dries out in summer mottling occurs due to small oxygen pockets and the re-oxygenation of iron.