Soil transportation, fate and exposure of chemicals Flashcards

1
Q

Characteristics of residual soil?

A
  • Underlying bedrock is the parent material.
  • Soil made in the same area and composition is similar with the bedrock.
  • It is usually less fertile and we have less information regarding it.
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2
Q

Characteristics of transported soil?

A
  • Parent material is different and depends on the source of rock.
  • Soil was transported so composition is different than the bedrock and is a mixture of various components.
  • It is usually more fertile and is more studied than the residual soil.
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3
Q

Main types of transported soil?

A

Gravity
Glaciers
Water
Wind

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4
Q

Examples under gravity transportation?

A

Colluvial deposits -> talus

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5
Q

Examples under glacier transportation?

A

Glacial deposits -> Eskers, drumlins

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6
Q

Examples under water transportation?

A

Fresh water:
streams -> alluvial deposits
lakes -> lacustrine deposits

Sea water:
marine deposits -> marine clay and marl

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7
Q

Examples under wind deposits?

A

Aeoline deposits -> loess and sand dunes

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8
Q

What happens to chemical when they enter the environment? (Many examples)

A

o Degrade chemically, photochemically or biologically
o Drift into the soil or to water body
o Be adsorbed to the soil or to the sediment
o Retail in solid material and accumulate in soil or organisms
o Vaporise to the atmosphere

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9
Q

The transformation of chemicals depend on what environmental conditions?

A

o Temperature, pH, sunlight intensity, microbial activity, etc.
o Air and water exchange, sorption/desorption, etc.

• Lipophilicity of chemicals – ability of chemical to dissolve in fats, oils, etc.

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10
Q

Properties of Chemicals? (3)

A

• Water Solubility:
- Tendency of chemical to transfer from water to air, soil, and organisms.

• Dissolving better in organic solvents than in water:

  • Tendency to move into organic phases (soluble in fat, etc.).
  • Lipophilic chemicals can be accumulated in an organism.

• Volatility:
- Tendency of chemical to vaporize with high vapor pressure and low water solubility.

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11
Q

What is sorption?

A

Stickiness of chemical with soil and
sediment, depends on the soil type and organic content.

Sticky soils such as clay has higher sorption
capacity.
o Absorption – soak up inside the
surface.
o Adsorption – hold molecules as a thin
film on the outside surface.
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12
Q

What is desportion?

A

Detachment of chemicals from

soil particles.

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13
Q

Small soil/sediment size particles do what?

A

They attract more chemicals. Small molecule size chemicals can easily accumulate in soil and organisms.

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14
Q

Water soluble chemicals can?

A

Travel through soil pores to ground and surface water

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15
Q

Particles age and temperature?

A

Aged and low temperature decrease release of chemical in water body through soil.

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16
Q

Organic matter of soil makes the soil retain?

A

More chemicals

17
Q

Environmental degradation and chemicals relate how?

A

Resistant chemicals to environmental degradation are typically harmful in nature.
Slow degradation leads to accumulation.

18
Q

What is abiotic degradation?

A

Abiotic Degradation - that of chemicals without microbes.

o Hydrolysis – breaking chemical bonds by addition of water.
o Oxidation – breaking chemical bonds by addition of oxygen.
o Oxidation helps in the process of photolysis.

19
Q

What is biotic degradation?

A

Biotic Degradation – that of chemicals with microbes.

o Leads to mineralization of chemicals to water, carbon dioxide, etc.

20
Q

What is mineralization?

A

Complete conversion of chemicals to their simplest
naturally occurring fragments.
Increasing microbial activity increases potential of chemical degradation.

21
Q

Finnish Context for Toxic Transportation in Soil?

A

Chemical and biological processes are slow due to cold.

Physical processes such as sorption, degradation, evaporation, bioaccumulation are slow due to cold.

Active organic layer is low in soil and amount of nutrient is low in soil.

Humic content (due to dissolved organic material) is high in water aiding sorption of chemicals.

22
Q

What are the water structures for soil interaction?

A
Littoral zone (producers like plants)
Limnetic zone (producers like algea)
Profundal zone (mixture of aerobic and anaerobic
producers such as green photosynthetic bacteria)
Benthic zone (with sulfur reducing bacteria)
23
Q

Presence of low nutrient content in the water can do what?

A

In case of low nutrient in the water, the microbes will grow in the surface (where there is carbon dioxide from atmosphere and light).

Same is the case of microbes based on the availability of oxygen (more on surface and less on deeper water)

24
Q

What is eutrophication?

A

Excess amount of nutrients in water body.

Major causes:
➢ Through organic matter (such as sewage waste)
➢ Through inorganic matter (such as nitrogen and phosphorous)

25
Q

How does the eutrophication starts?

A

Algae and cyanobacteria get energy
-> carbon from sunlight and carbon dioxide from the surface

Cyanobacteria also fixes atmosphere nitrogen adding up more nutrient in the water body system

Phosphorous is the required nutrient now – a small pollution can thus trigger eutrophication

26
Q

Water solubility, a chemical property what does it mean?

A

Determines the tendency for chemicals to move or

transfer from water to air, soil, and organisms.

27
Q

Chemicals that dissolve better in organic solvents than in water has?

A

Tendency to Move into Organic Phases (lipophilic = fatsoluble).
Lipophilic chemicals can be accumulated in an organism.

28
Q

What does bioaccumulation means?

A

Refers to the accumulation of substances, such as pesticides, or other chemicals in an organism.

29
Q

When does bioaccumulation occurs?

A

When an organism absorbs a substance at a rate greater than that at which the substance is lost.

30
Q

What is volatility?

A

Volatility is the tendency of a substance to vaporize = to get in the air.
It is directly related to a substance’s vapor pressure.

31
Q

The evaporation of a chemical from water depends on its volatility and its water solubility as well. However, If the substance is totally water soluble then?

A

It will not easily evaporate from water although it’s

vapor pressure is high.

32
Q

Soil sorption is highly dependent of?

A

Soil type and particularly soil organic content.

Generally, soils higher in clay and organic matter have a higher ‘sorption capacity´.

33
Q

Chemicals are usually attached to the smallest or largest particle size fraction?

A

Smallest!

34
Q

How does planarity affect sorption?

A

Planar compounds sorb more tightly and may reach more narrow spaces.
Planar compounds are more tightly bound and nonplanar compounds.

35
Q

Why is molecular size important?

A

Because the larger ones cannot bioaccumulate and thus cannot by pass the cell membrane easily.

36
Q

How does chemicals react if temperature is pretty low?

A

Decreases the fraction of chemicals that can be released to the water phase.
Evaporation is smaller.
Also bioaccumulation decreases.

37
Q

Why is chemical degradation important?

A

In ideal situation chemicals are degraded to nontoxic products such as carbon dioxide, water, and minerals
(mineralization).

38
Q

If the chemical is easily degradable, it may

A

not have significant impact on the environment.

39
Q

If the chemical degrades slowly,

A

it can spread broadly and accumulate in soil or in biological organisms.