Biosphere - Soils Flashcards

1
Q

What is soil made of? + percentages

A

Minerals - 45%
Air and water - 50%
Organic matter - 5%

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2
Q

Leaching

A

Removal of soluble minerals, salts and humus,which are washed downwards through the soil and may accumulate in the subsoil.

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3
Q

Humification

A

Breakdown or decomposition of plant remains leading to the formation of different types of humus.

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4
Q

Illuviation

A

Introduction of material to a soil layer.

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5
Q

Eluviation

A

Removal of materials from a soil layer.

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6
Q

Soil horizon

A

A layer of soil parallel to the soil crust whose characteristics differ from the horizons above and below.

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7
Q

Soil profile

A

A vertical cross section of a soil, divided into a number of distinct layers, referred to as horizons.

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8
Q

Regolith

A

Fragments of rock

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9
Q

Capillary action

A

Process whereby water and minerals in a solution can be drawn upwards when the rate of evapotranspiration is greater than precipitation.

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10
Q

Parent material

A

Underlying geological material (bedrock) in which soil horizons for,.

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11
Q

anerobic conditions occur in…

A

gley soil

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12
Q

Intrazonal soils

A

Soils that do not reflect climactic or vegetation standard influence.

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13
Q

Azonal soil

A

Immature soils that lack the development of a B horizon

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14
Q

What are the 6 factors affecting soil formation

A
  1. Parent material
  2. Biotic factors
  3. Climate
  4. Man
  5. Relief
  6. Time
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15
Q

What is in the O horizon

A

Leaf litter and humus layer

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16
Q

What is in the A horizon

A

Mix of organic and parent material

17
Q

What is in the B horizon

A

Mix of mostly parent material with washed in organic matter

18
Q

Podzolisation

A

Leaching of material of iron, aluminium and humus from the surface layers to the lower layers. Causes A horizon to become grey colour and courser in texture. B horizon becomes darker and has a finer texture with an iron pan.

19
Q

Podzol

A

Surface - Coniferous vegetation
O horizon - Thin black humus
A horizon - Ash grey colour as minerals are eluviated into B horizon
B horizon - Dark brown - lighter brown
C horizon - Parent material
Distinct layers - not as much biotic activity bc cold + wet climate + acidic

20
Q

Gley

A

Surface - Grasses and shrubs
O horizon - Partial decomposition
A horizon - Black with acid humus
B horizon - Blue/ grey clayey mud. Waterlogged, slow decomposition. Angular rock fragments. Unstratified.
C horizon - Permafrost. Solid bedrock, generally shallow soil

21
Q

Brown earth

A

Surface - Deciduous vegetation (roots go straight down)
O horizon - Dark brown
A horizon - Light brown
Iron pan between
B horizon - Gradual leaching, iron and aluminium oxides deposited
C horizon - Parent material