L13 - Mineral and Organic Components of Soils Flashcards

1
Q

What determines mineral composition of soil?

A

Weathering (physical, chemical and biological)

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2
Q

Loamy soils

A

good drainage, sufficient water holding capacity, good for agriculture

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3
Q

Coarse sandy soils

A

heat up quickly, good drainage (leaching), low water holding capacity (WHC)

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4
Q

Clay soils

A

hold on to nutrients, poor drainage, waterlogged under wet conditions, solid under dry conditions

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5
Q

How do silicates form chains?

A

By sharing O atoms

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6
Q

Ortho-silicates

A

isolated

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7
Q

Ino-silicates

A

single/double chain

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8
Q

Phyllo-silicates

A

layered sheet

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9
Q

Tekto-silicate

A

3D framework

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10
Q

What climate are 2:1 clay particles typically found?

A

Temperate climates

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11
Q

What climate are oxides typically found?

A

Humid, tropical climates. Soils here are highly weathered and contain mainly kaolinite (1:1) and iron/aluminium oxides

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12
Q

What are clay minerals?

A

Layered silicates (phyllosilicates) formed by tetrahedrons and octahedrons. Connected by Si-O-Al/Si bridges

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13
Q

Elementary layer

A

succession of T and O (TOT) atoms in a clay mineral layer. Can be split by weathering

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14
Q

Basal spacing

A

distance from one basal layer to the next

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15
Q

How are nutrients held at exchange sites?

A

held in their cationic form by outer sphere complex formation. May easily be taken up by plant roots

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16
Q

What determines the bond strength between elementary layers?

A

By electrochemical charge. This influences sensitivity to weathering and physical characteristics such as swelling and shrinking

17
Q

Isomorphous substitution

A

exchange of ions with lower charge during clay mineral formation (compensation by adsorbing cations). Allows for permanent charge in 2:1 and 1:1 clay particles between elementary layers
E.g. tetrahedron Si4+ -> Al3+

18
Q

What are negative effects of shrinkage cracks in soil?

A

Water may bypass root zone and be transported straight to subsoil (B). This results in inefficient sprinkler irrigation, nutrient shortage in plants and groundwater pollution. Also destruction of buildings, pavements and pipes in heavy clay soils

19
Q

What are positive effects of shrinkage cracks in soil?

A

Drainage of heavy clay soils where (K) increases. Also naturally restores soil compaction

20
Q

Cation exchange capacity (CEC)

A

total number of cations a soil can hold, or total negative charge.

21
Q

Importance of CEC?

A

Important for availability of macro and micro nutrients, and soil remediation in case of heavy metal pollution

22
Q

What influences CEC?

A
  1. Equilibrium reaction
  2. Electrochemical charge
  3. pH - acidification can lead to Al toxicity and cation release. BS% increases with pH
23
Q

How can iron oxides retain nutrients?

A

By forming inner sphere complexes - such nutrients are not readily available to plants, and are stored in subsoil horizons

24
Q

How does organic matter influence soil fertility?

A

Source of nutrients, regulates pH and is the basis for soil fauna

25
Q

How does organic mater influence soil structure?

A

Allows for the formation of stable soil aggregates with mineral components, important for drainage and aeration, and reduces soil sensitivity to erosion

26
Q

Importance of organic matter in soil?

A

Fertility, structure, resistance to root penetration, increases WHC and CEC

27
Q

What is the primary source of organic matter?

A

Plant material. Composition depends on species, part, growth conditions and condition when cut off

28
Q

Mineralisation

A

transformation of organic molecules to inorganic molecules (including nutrients) by soil microbes.

29
Q

What determines the rate of mineralisation?

A

Composition of the organic matter, microbes present and the abiotic conditions (e.g. pH and moisture content)
Composition of the organic matter, microbes present and the abiotic conditions (e.g. pH and moisture content)

30
Q

Organisms involved in decomposition

A

Detritivores, Primary decomposer, Secondary decomposer