Lec 6 Flashcards

1
Q

What are the concepts that equilibrium concentrations of contaminants are based on?

A

Partitioning, sorption and exhange

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2
Q

Partitioning

A

Tendency of a contaminant to exist at equilibrium between two phases

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3
Q

Sorption

A

A partitioning and exchange phenomenon that describes a contaminant to accumulate at the solid surface from the surrounding solution/air

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4
Q

Exchange

A

Displacement of the charged species by another species that has higher affinity for the same site on the solid surface

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5
Q

Fugacity

A

Molecule’s tendency or driving force to escape the system it is in

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6
Q

Sorption types

A

Electrostatic
Physical
Chemical

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7
Q

Sorbent characteristics for sorption of organic compounds

A

Hydrophobicity
Specific surface

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8
Q

Sorbate (contaminant) characteristics to influence sorption

A

Hydrophobicity
Ionic charge
Kow
Water solubility (?)

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9
Q

Which do sorb charged species

A

Clays, smaller particles

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10
Q

Measures of hydrophobicity of a compound

A

Low water solubility ~ sorption tendency
Kow (octanol water partition coefficient)

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11
Q

Partition coefficients

A

Kow: octanol water partition coefficient
Kd: soil distribution coefficient
Koc: soil adsorption coefficient

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12
Q

Is Kow related with water solubility of the compound?

A

NOOOOO

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13
Q

high logKow means?

A

-more hydrophobic
-partitioning more into octanol than water
-potential to bioconcentrate in living organisms

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14
Q

-logKow ?

A

Kow < 1
İt is partitioning more into water than octanol

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15
Q

Soil components (extremely variable, heterogeneous)

A

inorganic fraction (45-49.9%)
organic matter (0.1-5%)
water
air

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16
Q

Most important soil properties of HWM & most critical factors im sorption of chemicals

A

CEC (cation exchange capacity)
SOM (soil organic matter)

17
Q

CEC

A

quantity of cations sorbed per mass of soil (meq/100g soil)

18
Q

Higher CEC

A

Higher removal potential
Higher sorption of ionic compounds into soil

19
Q

SOM

A

Determines how much a soil can adsorb org contaminants
Humic (org) + Non-humic (inorg)
MMMOST COMMON SORBENT IN SOILSSS

20
Q

Higher SOM

A

Higher sorption of org compounds into soil

21
Q

Humic fraction (org)

A

Humin
Humic acids
Fulvic acids

22
Q

Isotherm

A

Langmuir: monolayer adsorption of sorbate
Freundlich: multilayer adsorptionof sorbate

23
Q

Langmuir

A

Ce/qe (y) vs Ce (x)

slope: 1/a
y-intercept: 1/ab

24
Q

Freundlich

A

lnqe (y) vs lnCe (x)
slope: 1/n
y-intercept: lnKf

25
Q

Kd (mL/g)

A

Soil distribution coefficient
(mg/g) / (mg/mL)

26
Q

Koc (mL/g)

A

Soil adsorption coefficient
(mg/g) / (mg/L)

27
Q

Retardation factor (R)

A

If R > 1, contaminant is moving slower than groundwater: advantageous for waste management context

28
Q

What is R directly related with

A

HYDROPHOBICITY OF CONTAMINANT

29
Q

Non-polar sorbents

A

GAC
SOM (Soil organic matter)