Aqueous Geochemistry Flashcards

1
Q

Physical geologic processes

A

With or without participation of geofluids

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2
Q

Chemical geologic processes

A

Participated by geofluids

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3
Q

Composition of geofluids

A

Variable amounts of components derived from dissolution of solid materials and gases

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4
Q

Dissolved species

A

Materials dissolved in water may be in the forms of molecules or ions

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5
Q

What reaction is always in the background?

A

H2O = H+ + OH-

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6
Q

Dissolved components

A

May be in the form of different species.
The total amount of the dissolved component is the sum of all the dissolved species

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7
Q

Avogadro’s number

A

1 mole of a substance = 6.02 x 10^23 that substance

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8
Q

Molality (m) is = to what?

A

moles / kg water

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9
Q

Molarity (M) is = to what?

A

moles / liter solution

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10
Q

What are the two types of geochemical reactions?

A

1) fluid-fluid reactions
2) fluid-rock reactions

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11
Q

Open system

A
  • Fluid flows through the fluid-rock system
  • Composition is controlled externally
  • Fluid-rock ratio = high
  • Chem eq = not reached
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12
Q

Closed system

A
  • Fluid is stagnant in the fluid-rock system
  • Composition is controlled internally
  • Fluid-rock ratio = low
  • Chem eq = reached
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13
Q

True or False: The geochemical reaction equation is NOT unique for a given pair of reactant & product

A

True

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14
Q

Chemical reaction equilibrium

A

Forward reaction rate = Reverse reaction rate

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15
Q

Le Chatelier’s Principle

A

If equilibrium is disturbed, reaction will proceed in the direction that will counteract the disturbance

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16
Q

Difference between concentration and activity

A

Concentration: (A)
Activity: [A]

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17
Q

Law of mass action equation

A

K =[C]^c [D]^d / [A]^a [B]^b

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18
Q

How is equilibrium constant K determined?

A
  • Experiment at specific P-T-X conditions
  • Calculations from thermodynamic database
19
Q

Congruent dissolution

A

The dissolution of one mineral is not accompanied by precipitation of another mineral

20
Q

Incongruent dissolution

A

The dissolution of one mineral is accompanied by the precipitation of another

21
Q

Solubility of a mineral

A

The max amount of a compound in a mineral that can be dissolved in solution at a given P-T condition (must be in eq)

22
Q

Mineral solubility constant (Ksp)

A

Chemical reaction constant (K) for the mineral dissolution equation

23
Q

Ion activity product (IAP)

A

The activity of dissolved ions before chemical equilibrium

24
Q

What happens when IAP = Ksp?

A

Saturation

25
What happens when IAP < Ksp?
Undersaturation
26
What happens when IAP > Ksp?
Oversaturation
27
Geochemical divide
When the solution ratio approaches zero. Precipitation stops
28
Solubility diagram
A diagram that shows the variation in solubility of a mineral and the change of the dominant dissolved species
29
Mineral stability diagram
A diagram that shows the fields in which different minerals are stable
30
How are mineral stability diagrams constructed? (4 steps)
1) List all minerals involved 2) Construct the chemical reactions between pairs of minerals 3) Law of mass action to construct activity-activity equations for each pair 4) Plot all activity-activity relations
31
Redox
Chemical reaction where electrons are transferred from one species to another
32
Oxidized: _____ electrons
Gives away
33
Reduced: _____ electrons
Gains
34
Oxidized --> _____ agent
Reducing
35
Reduced --> _____ agent
Oxidizing
36
True or False: Reduction and oxidation always occur together
True
37
Fugacity
Effective partial pressure of a gas in a system
38
Oxygen fugacity
Effective partial pressure of O2 in a system
39
Eh
Redox state of a solution
40
What is the pH equation?
pH = -log [H+]
41
What happens when two different geologic fluids encounter each other?
They react with one another
42
What happens when a geologic fluid is in contact with a rock?
Chemical reaction. Rock will be slightly dissolved
43
How to predict the direction of geochemical reactions?
Le Chatelier's Principle
44
What controls the composition (including Eh and pH) of geologic fluids?
Different locations Different history Different rocks reacting with one another