Land degredation Flashcards

1
Q

Define land degradation

A

Land degradation describes a long-term decline in ecosystem function and productivity.

Land degradation is a bio-physical-chemical process driven by socioeconomic and political causes

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2
Q

What are the consequences of land degradation?

A
  • Decreased land productivity
  • Poverty, hunger, migration, worsened food insecurity + uncertainty
  • Reduced water quality and availability
  • Resource loss
  • Socioeconomic problems
  • Biodiversity loss + damage to ecosystems
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3
Q

Consequences of land degradation in terms of welfare

A
  • Clean and adequate water
  • Clean food and air
  • Encourages migration
  • Respiratory conditions by dust from wind erosion + other air pollutants
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4
Q

What are the three mechanisms that initiate land degredation?

A

Land degredation can be physical, chemical, or biological.

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5
Q

What is physical land degradation?

A

Decline in soil structure leading to crusting, compaction, erosion, desertification, anaerobism.

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6
Q

What is the result of chemical land degradation?

A

acidification, leaching, salinization, decrease in cation retention capacity, and fertility depletion, chemical toxicity

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7
Q

What is the result of biological land degradation?

A

Loss of soil carbon, loss of beneficial microbes, loss of microbial diversity and function

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8
Q

What are two main types of erosion?

A
  • Wind erosion

- Water erosion

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9
Q

Different forms of wind erosion based off particle size?

A

• 1 mm move by rolling (soil creep).
• 0.1 – 1 mm move by saltation, collision by
entrained particles.
• <0.1 mm detach into suspension.

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10
Q

What is saltation?

A
  • preferentially strips out quality aspects: soil carbon.

Saltation is the main process that suspends soil particles in the air - particles between 0.1 and
0.5mm in diameter are lifted by wind then fall back to the ground, so they hop or bounce across
the surface. Leads to breaking the boundary layer protecting lower layers from erosion.

When it doesn’t catch large particles and leads to the formation of a smooth/fine layer over the top: a crust that will break away+ allow beneath contents to erode if another particle lands on it and dislodges it.
=> chain reaction using v. fine clay, silts, and carbon
=> leaves larger, inert materials behind (sand) so reduces quality of the soil: will lack the ability to hold nutrients.

  • if one grain hits the surface, 3-4 will be liberated.
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11
Q

What is creep?

A

Particles greater than 0.5mm in diameter are usually too heavy to be lifted by wind. Creep is
when wind rolls these particles or they are moved along the surface by bombardment by other
moving particles.

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12
Q

What is suspension?

A

Small particles less than 0.1mm in diameter that have been ejected into the air by saltation
remain suspended as dust and are carried away from the erosion site by the wind. The majority
of particles greater than 0.02mm will settle back to the ground within 100 kilometres of the
erosion site, but finer particles can be carried long distances, as far as New Zealand.

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13
Q

What are the strategies to reduce wind erosion damage?

A

Cloddy Tillage or stubble retention should create soil roughness by leaving clods in the soil or by making ridges and furrows perpendicular to the prevailing wind direction. ….not effective in sandy soils due to lack of cohesiveness

Clay listing sandy soils is used in duplex because they do not produce durable surface clods. Listing ridges the soil and brings up firmer subsoil clay….perpendicular to the eroding wind, …need heavy duty cultivator.

Surface and crop residues can be retained after harvest, which generally coincides with the dry season, to provide soil cover and reduce wind erosion.

Strip cropping reduces the width of the field area where the soil is exposed to wind erosion. Alternating strips of crops and fallow or strips of clean cultivated crops …. not widely practiced.

Intercropping is widely used in many arid regions, and several systems have been developed. …i.e. pasture cropping.

Wind breaks interrupt wind flow and reduce wind velocity through presence of physical barriers.

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14
Q

What is the result of reducing fetch?

A

Reducing fetch means less distance over which wind can gain speed, so less capacity to strip soil away.

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15
Q

What are some wind erosion control options for cropping?

A
  • Strip cropping
  • Tree wind breaks/shelter belts: create eddying + pressure changes that reduce wind speed.
  • Ridging
  • Crop residues: about 50% of ground cover needed to control wind erosion. Ground cover prevents erosion.
  • Clay delving
  • Crop wind breaks
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16
Q

What’s the general pattern of a water erosion sequence?

A

Splash erosion leads to crust formation and reduced infiltration.

This causes sheet erosion. If conc. of water in depressions + increased flow velocity occurs, this leads to rill erosion. If run-off enters dispersive subsoil, tunneling will occur.

If roof collapse occurs in tunneling, or further conc. of flow and headwall development occurs in rill erosion, a gully will form.

17
Q

What is splash erosion?

A

Raindrop impact acts as soil bombardment which causes a crust to form.

  • First stage in erosion sequence.
  • Clogs up pores in soil that normally absorb rain water, forming crusts that are mostly impermeable, so puddles of unabsorbed water begin to form, flowing downhill in a thin sheet.
  • Carries away fine particles in run-off.
18
Q

What is rill erosion?

A

Rill erosion results from the concentration of surface water (sheet flow) into deeper, fasterflowing channels.

19
Q

Gullies vs rills?

A

Gullies are rills that are larger than 1 foot deep and 1 foot wide.

20
Q

What’s the problem with sodic/dispersive soils?

A

Erosion
• Gully erosion
• Tunnel erosion
• Dam collapse

Water Quality
• Extreme turbidity (never settles)
• Sediment deposits

Construction / Development
• Collapse of Fill
• Pipe & Cable Collapse
• Breaching Septic Trenches
• Dam Failure
21
Q

what are dispersive/sodic soils?

A
Dispersive Soils
• Appear to ‘dissolve’ in water.
• Responsible for tunnel erosion.
• Dispersive soils are usually sodic.
• Structurally unstable, require special consideration for development.
22
Q

How does sodicity lead to dispersiveness

A

Increased ion concentration on particle surface prevents formation of aggregates.

  • Normally clay platelets would stack together + clump.
  • More than 5% sodium leads to dispersive behaviour.
23
Q

Why is salinity a problem?

A

salinity is a problem because salt affects water and nutrient uptake by plants.

  • salt can be toxic to plants
  • remediation of salty land is hard
24
Q

Why is compaction a problem?

A

Compaction is a problem because it reduces infiltration and draining, making it harder for roots to penetrate.

Subsurface compaction restricts root
development: don’t get large fibrous nets but short bent roots.

25
Q

What are the properties of good soil structure?

A
• Porous clod faces.
• Many pore spaces and root
holes.
• A good range of aggregate sizes.
• Lots of fine fibrous white roots.
• large network of soil pores (high
porosity) 
• loose friable structure
• high permeability for rainfall
• good plant available moisture
range
• low soil strength
• Minimal surface ponding
26
Q

What are the causes of compaction?

A

Soil Moisture: The most important
factor ! Soil moisture affects both
the depth and severity of the
compaction.
Vehicle Weight: Increases the
depth of the compaction
Number of Passes: 90% of the
damage is done in the first pass
Tyre Pressure: Ground pressure is usually
1-2 PSI above the tyre pressure regardless of weight.
Tyre Width: Has minimal effect unless inflation pressure is reduced i.e.
Flotation tyres.
Soil Type: Compaction occurs more readily in soils with high Silts, fine
sands content, Low organic matter, high sodium ~ Sodic
soils

27
Q

How to avoid compaction?

A
HOW TO AVOID
• Avoid compression when susceptible
• Improve soil structure (SOM)
• Controlled traffic/ fixed bed cropping
• Cultivation strategies (eg deep ripping)
• Choice of machinery
28
Q

Why is soil organic matter important?

A
• Stabilises and holds soil
particles together
– reduced erosion
– improved structure
– Reduces susceptibility
to compaction
• Source of carbon and energy for soil biota
• Stores and supplies nutrients
• Binds pesticides
 SOM reduced by cultivation
• Increased by pasture, green manure crops,
addition of organic matter
• Effects of management
practices vary with
climate, soil type
29
Q

Relationship between soil carbon and nutrient holding capacity?

A

A 0.5% loss in organic matter may lead to 14% loss in nutrient holding capacity, 12% loss in water holding capacity.

30
Q

What causes acidification?

A

Acidification results from:
• Ammonium-based nitrogen fertilisers
• Leaching of nitrate nitrogen
• Continual removal of plant and animal produce and waste products
• Leaching of cations ie Calcium, Iron, Magnesium
• Sulphur fertilizers – ie ammonium sulphate, Potassium sulphate

31
Q

What does acidification cause?

A

Makes some nutrients less available and some toxins more available.
- Ca and P deficiency, Mn and Al toxicity

32
Q

why is degraded land an issue?

A

Degraded land bad bc
• costly to reclaim
• may no longer provide a range of ecosystem functions and services
• loss of the goods and potential environmental, social, economic and non-material benefits that are critical for society and development.