Contaminant transport in soil Flashcards

1
Q

What is a soil?

A

a natural body comprised of soilds, liquids and gases that occur on the land surface. Characterized bo on of the following:
- horizon or layers that are distinguishable from the initial material as a result of addition, losses, transfere and transformation of energy and matter

  • the ability to support rooted plants in a natural environment
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2
Q

What are the main constituents of soil?

A
  • liquid and gas phases (pore volume) (ca 50%)
  • solid phase: inorganic (mineral) matter (ca 45%)
  • solid phase: organic matter (ca 5%)
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3
Q

Whant is a sand?

A
  • mainly quartz
  • has uniform dimensions
  • can be represented as spherical
  • not necessarilt smooth, can have jagged surfaces
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4
Q

What is a silt?

A
  • particles size intermediate between and and clay
  • higher surface area then of sand
  • coated with clay
  • some simular physioco-chemical properties to clay
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5
Q

What is a clay?

A
  • particle size <0,002 mm
  • secondary mineral derived from weathering of primare minerals
  • plate like a needle in shape
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6
Q

What type of building blocks are the layers in a clay made of?

A
  • tetraheda
  • octaheda
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7
Q

what is the charge of a clay mineral and what does it depend on?

A
  • always negative charge
  • permanent surface charge that is pH dependent

OBS! could have a positive charge at very low pH

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8
Q

What is adsorption?

A

a process of accumulation of gas or liquid solute on the surface of a solid, forming a molecular or atomic layer

  • clays, metal oxides and organic matter provides surface for adsorption because of:
    - large specifc surface area
    - large change per surface unit
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9
Q

What is a diffuse double layer?

A
  • no complexes between ions and charged surfaces
  • neutralization of the surface charge
  • ions and molekules can easily be exchanged for other ions and molecules present in the pore water
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10
Q

What is ion exchange?

A

one ion is exchanged for onother ion at the surface of a solid particle

  • cation exchange: Ca2+ –> K+
    CEC: the amount of cations a soil can hold
  • anion axchange: H2PO4- –> NO3-
    AEC: the amount of anions a soil can hold
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11
Q

What is CEC?

A

cation exchange capacity

ex: if CEC=8 meq/100g –> 8 mmol K+ eller 4 mmol Ca2+

OBS! sand dose not contribute to CEC!

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12
Q

What is AEC?

A

anions exchange capacity

  • AEC increases as soil pH decreases
  • most contaminents are however positive charged
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13
Q

What is soil organic matter?

A
  • forms from plants and animal tissues through decomposistion by microorganisms, air and water
  • new compounds, humus, are formed through humification
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14
Q

What is humus?

A

composed of:
- fulvic acids: light yellow to yellow brown, most soluble

  • humic acids: dark brown to grey black
  • humin: black. NOT soluble, contains more carbon
  • Carbon, hydrogen, oxygen and nitrogen
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15
Q

How does the pH effect the cation adsorption?

A

the higher the pH is, the more negative charge –> more CEC

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16
Q

How is gas present in soil?

A
  • free phase
  • dissolved in soil solution
  • absorbed by solid matter

depends on:
- soil porosity (more pores –> more air)
- O2/CO2 penetration
- biochemical processes and reactions

17
Q

what is the aeration zone?

A

the zone where you have exchange between soil and atmosphere

  • above the saturated zone
18
Q

What does hygroscopic water mean?

A

the water molecules are tightly bound to the surfaces of particles by electrostatic force
- looses mobility
- increased density
- altered physical properties

19
Q

What is capillary water?

A

remaines in the pores through surface tension forces
–> the smaler particles, the larger the capilary raise

20
Q

What is free or gravitational water?

A

the water below the groundwater table where the soil is fully saturated with water

  • the groundwater layer
21
Q

How can disolved contaminants move in soil?

A
  • advection: same conc al the time (moves lika an object?)
  • dispersion and diffusion: high cons in middle, lower further out
  • sorption/desorption: adsorption to solid phases (ex. Org matter, clay minerals, metal oxides)
22
Q

What are the assumptions for the adsorption isotherm? what is not consider?

A
  • adsorption stops after all monolayer are filled
  • alla surface sites are alike and can hold no more then one atom
  • possibiity for a molecule to be sorbed onto surface

NOT consider:
- microbiological activity
- precipitation
- dissolution
- density difference
- complex and volatile material