5.1 Introduction to soil systems Flashcards

1
Q

soil storages

A

organic matter, organisms, nutrients, minerals, air, water

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

soil transfers

A
  • Biological mixing: Organisms like earthworms move soil particles and organic matter.
  • Leaching: Water-soluble substances move downward through the soil profile.
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

soil profile order

A

O, A, E, B, C

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

O horizon

A

Organic: the topmost layer, consisting of organic matter like leaf litter and decomposing organisms.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

A horizon

A

Also known as topsoil, rich in organic matter and minerals.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

E horizon

A

eluvial or leached horizon
- leaching removes matieral from the horizon

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

B horizon

A

Subsoil, where materials leached from upper layers accumulate.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

C horizon

A

Partially weathered parent material.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

soil profile definition

A

a vertical section through a soil, from the surface down to the parent material, revealing the soil layers or horizons.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

inputs of soil

A

inputs: organic (i.e. leaf litter) and parent material (inorganic matter), precipitation, energy

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

outputs of soil

A
  • uptake by plants
  • soil erosion
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

transformations of soil

A
  • decomposition
  • weathering
  • nutrient cycling
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

soil structure

A

the shape of the particles. it has an effect on primary productivity

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

soil texture

A

the size of a soil particle

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

sand particle size

A

less than 0.2mm in diameter

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

silt particle size

A

less than 0.02mm

17
Q

clay particle size

A

less than 0.002mm

18
Q

clay characteristics

A
  • Small particles (<0.002mm)
  • Poor drainage
  • Small air spaces
  • High water-holding capacity
  • High nutrient content
19
Q

sand characteristics

A
  • Large particles (0.05-2mm)
  • High drainage
  • Large air spaces
  • Low water-holding capacity
  • Low nutrient content
20
Q

field capacity

A

the max amount of water that a soil can hold

21
Q

loam soil

A
  • best soil for cultivation
  • Mixture of sand, silt, and clay
  • Balanced drainage
  • Good water-holding capacity
  • Adequate air spaces
  • Moderate to high nutrient content
22
Q

soil functions for humans

A
  • medium for plant growth (most food for humans is grown in soil)
  • soils contain an important store of relatively accessible freshwater (approx. 0.005% of global freshwater)
  • soils filter materials added to the soil thereby maintaining water quality
  • some recycling of nutrients takes place in soil → breakdown of dead organic matter
  • provide raw materials in the form of peat, clays, sands, gravels, and minerals
23
Q

is fertile soil renewable or non-renewable?

A

non renewable because it takes so long to develop and because of the current rate of resource use compared to the length of time required for resources to be replaced

24
Q

soil forming processes involve

A
  • gains and losses of material to and from the profile
  • movement of water between the horizons
  • chemical transformations within each horizon
25
Q

what kind of systems are soils

A

open system in a steady state equilibrium

26
Q

contrast in soils of tropical vs cold climates

A

tropical (Borneo):
- extremely deep due to the warm, wet year-round climate

cold (Iceland):
- thin or non-existent due to the lack of chemical weathering

27
Q

soil conditions that restrict root growth

A
  • absence of cracks
  • shortage of oxygen due to waterlogging
  • dryness
  • temperatures that are too high or too low

chemical conditions:
- high aluminium concentration, usually associated with low pH
- low nutrient supply
- phytotoxic chemicals in anaerobic soil

28
Q

advantages of triangular graphs

A
  • a large number of data can be shown on one graph
  • groupings are easily recognizable
  • dominant characteristics can be shown
  • classifications can be drawn up
29
Q

primary productivity of different soils

A
  • sandy soil: low primary productivity due to poor water holding capacity and low nutrient status
  • clay soil: quite low primary productivity due to poor aeration and poor water infiltration
  • loam soil: high primary productivity due to medium infiltration rate, water holding capacity, nutrient status, aeration, and ease of working
30
Q

primary productivity of soil depends on :

A
  • mineral content
  • drainage
  • water holding capacity
  • air spaces
  • biota
  • potential to hold organic matter
31
Q

Soil is an example of …

A

non-renewable natural capital

32
Q

ratio air, water, etc .

A
33
Q

system definition

A

an assemblage of parts, working together, forming a functional whole

34
Q

a soil horizon

A

distinct layer within the soil profile