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Redox Geochemistry

Redox Geochemistry

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Redox Geochemistry. WHY?. Redox gradients drive life processes! The transfer of electrons between oxidants and reactants is harnessed as the battery, the source of metabolic energy for organisms - PowerPoint PPT Presentation

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Page 1: Redox Geochemistry

Redox Geochemistry

Page 2: Redox Geochemistry

WHY?• Redox gradients drive life processes!

– The transfer of electrons between oxidants and reactants is harnessed as the battery, the source of metabolic energy for organisms

• Metal mobility redox state of metals and ligands that may complex them is the critical factor in the solubility of many metals– Contaminant transport– Ore deposit formation

Page 3: Redox Geochemistry

J. Willard Gibbs• Gibbs realized that for a reaction, a certain

amount of energy goes to an increase in entropy of a system.

• G = H –TS or G0R = H0

R – TS0R

• Gibbs Free Energy (G) is a state variable, measured in KJ/mol or Cal/mol

• Tabulated values of G0R available…

)reactants()( 000i

iii

iiR GnproductsGnG

Page 4: Redox Geochemistry

Equilibrium Constant

• for aA + bB cC + dD:

• Restate the equation as:

GR = G0R + RT ln Q

• GR= available metabolic energy (when negative = exergonic process as opposed to endergonic process for + energy) for a particular reaction whose components exist in a particular concentration

QRTaa

aaRT

bB

aA

dD

cC lnln

Page 5: Redox Geochemistry

Activity

• Activity, a, is the term which relates Gibbs Free Energy to chemical potential:

i-G0i = RT ln ai

• Why is there now a correction term you might ask…– Has to do with how things mix together– Relates an ideal solution to a non-ideal solution

Page 6: Redox Geochemistry

Ions in solution

• Ions in solutions are obviously nonideal states!

• Use activities (ai) to apply thermodynamics and law of mass action

ai = imi

• The activity coefficient, i, is found via some empirical foundations

Page 7: Redox Geochemistry

Activity Coefficients

• Extended Debye-Huckel approximation (valid for I up to 0.5 M):

• Where A and B are constants (tabulated), and a is a measure of the effective diameter of the ion (tabulated)

I

aBII

IAz2.0log

2

1

2

12

Page 8: Redox Geochemistry

Speciation• Any element exists in a solution, solid, or

gas as 1 to n ions, molecules, or solids

• Example: Ca2+ can exist in solution as: Ca++ CaCl+ CaNO3

+

Ca(H3SiO4)2 CaF+ CaOH+

Ca(O-phth) CaH2SiO4 CaPO4-

CaB(OH)4+ CaH3SiO4

+ CaSO4

CaCH3COO+ CaHCO3+ CaHPO4

0

CaCO30

• Plus more species gases and minerals!!

Page 9: Redox Geochemistry

Mass Action & Mass Balance

• mCa2+=mCa2++MCaCl+ + mCaCl20 + CaCL3- +

CaHCO3+ + CaCO3

0 + CaF+ + CaSO40 +

CaHSO4+ + CaOH+ +…

• Final equation to solve the problem sees the mass action for each complex substituted into the mass balance equation

lc

nc

i HLC

HCL

][][

][][

nxLmCamCa 22

Page 10: Redox Geochemistry

Geochemical models

• Hundreds of equations solved iteratively for speciation, solve for GR

• All programs work on same concept for speciation thermodynamics and calculations of mineral equilibrium – lots of variation in output, specific info…

Page 11: Redox Geochemistry

Oxidation – Reduction Reactions

• Oxidation - a process involving loss of electrons.

• Reduction - a process involving gain of electrons.

• Reductant - a species that loses electrons.

• Oxidant - a species that gains electrons.

• Free electrons do not exist in solution. Any electron lost from one species in solution must be immediately gained by another.

Ox1 + Red2 Red1 + Ox2LEO says GER

Page 12: Redox Geochemistry

Half Reactions• Often split redox reactions in two:

– oxidation half rxn e- leaves left, goes right• Fe2+ Fe3+ + e-

– Reduction half rxn e- leaves left, goes right• O2 + 4 e- 2 H2O

• SUM of the half reactions yields the total redox reaction

4 Fe2+ 4 Fe3+ + 4 e-

O2 + 4 e- 2 H2O

4 Fe2+ + O2 4 Fe3+ + 2 H2O

Page 13: Redox Geochemistry

Half-reaction vocabulary part II

• Anodic Reaction – an oxidation reaction

• Cathodic Reaction – a reduction reaction

• Relates the direction of the half reaction:

• A A+ + e- == anodic

• B + e- B- == cathodic

Page 14: Redox Geochemistry

ELECTRON ACTIVITY

• Although no free electrons exist in solution, it is useful to define a quantity called the electron activity:

• The pe indicates the tendency of a solution to donate or accept a proton.

• If pe is low, there is a strong tendency for the solution to donate protons - the solution is reducing.

• If pe is high, there is a strong tendency for the solution to accept protons - the solution is oxidizing.

e

ape log

Page 15: Redox Geochemistry

THE pe OF A HALF REACTION - I

Consider the half reaction

MnO2(s) + 4H+ + 2e- Mn2+ + 2H2O(l)

The equilibrium constant is

Solving for the electron activity

24

2

eH

Mn

aa

aK

21

2

4

H

Mne Ka

aa

Page 16: Redox Geochemistry

DEFINITION OF EhEh - the potential of a solution relative to the SHE.

Both pe and Eh measure essentially the same thing. They may be converted via the relationship:

Where = 96.42 kJ volt-1 eq-1 (Faraday’s constant).

At 25°C, this becomes

or

EhRT

pe303.2

Ehpe 9.16

peEh 059.0

Page 17: Redox Geochemistry

Free Energy and Electropotential

• Talked about electropotential (aka emf, Eh) driving force for e- transfer

• How does this relate to driving force for any reaction defined by Gr ??

Gr = - nE– Where n is the # of e-’s in the rxn, is Faraday’s

constant (23.06 cal V-1), and E is electropotential (V)

• pe for an electron transfer between a redox couple analagous to pK between conjugate acid-base pair

Page 18: Redox Geochemistry

Electropotentials• E0 is standard electropotential, also standard

reduction potential (write rxn as a reduction ½ rxn) – EH is relative to SHE (Std Hydrogen Electrode)

At non-standard conditions:

dD

cC

bB

aA

HH aa

aa

nF

RTEE ln0

dD

cC

bB

aA

HH aa

aa

n

VEE log

0592.00At 25° C:

Page 19: Redox Geochemistry

Electromotive Series• When we put two redox species together, they will

react towards equilibrium, i.e., e- will move which ones move electrons from others better is the electromotive series

• Measurement of this is through the electropotential for half-reactions of any redox couple (like Fe2+ and Fe3+)– Because Gr =-nE, combining two half reactions in a

certain way will yield either a + or – electropotential (additive, remember to switch sign when reversing a rxn)

+E - Gr, therefore spontaneous

• In order of decreasing strength as a reducing agent strong reducing agents are better e- donors

Page 20: Redox Geochemistry

• Redox reactions with more negative reduction potentials will donate electrons to redox reactions with more positive potentials.

NADP+ + 2H+ + 2e- NADPH + H+ -0.32O2 + 4H+ + 4e- 2H2O +0.81

NADPH + H+ NADP+ + 2H+ + 2e- +0.32O2 + 4H+ + 4e- 2H2O +0.812 NADPH + O2 + 2H+ 2 NADP+ + 2 H2O +1.13

Page 21: Redox Geochemistry

ELECTRON TOWERmore negative

more positiveBOM – Figure 5.9

oxidized/reduced formspotential acceptor/donor

Page 22: Redox Geochemistry
Page 23: Redox Geochemistry

Microbes, e- flow

• Catabolism – breakdown of any compound for energy

• Anabolism – consumption of that energy for biosynthesis

• Transfer of e- facilitated by e- carriers, some bound to the membrane, some freely diffusible

Page 24: Redox Geochemistry

NAD+/NADH and NADP+/NADPH• Oxidation-reduction reactions use NAD+ or

FADH (nicotinamide adenine dinucleotide, flavin adenine dinucleotide).

• When a metabolite is oxidized, NAD+ accepts two electrons plus a hydrogen ion (H+) and NADH results.

NADH then carries

energy to cell for other uses

Page 25: Redox Geochemistry

• transport ofelectrons coupledto pumping protons

glucosee-

CH2O CO2 + 4 e- + H+0.5 O2 + 4e- + 4H+ H2O

Page 26: Redox Geochemistry

Proton Motive Force (PMF)

• Enzymatic reactions pump H+ outside the cell, there are a number of membrane-bound enzymes which transfer e-s and pump H+ out of the cell

• Develop a strong gradient of H+ across the membrane (remember this is 8 nm thick)

• This gradient is CRITICAL to cell function because of how ATP is generated…

Page 27: Redox Geochemistry

HOW IS THE PMF USED TO SYNTHESIZE ATP?• catalyzed by ATP

synthase

BOM – Figure 5.21

Page 28: Redox Geochemistry

ATP generation II

• Alternative methods to form ATP:

• Phosphorylation coupled to fermentation, low yield of ATP

Page 29: Redox Geochemistry

ATP• Your book says ATP: “Drives

thermodynamically unfavorable reactions” BULLSHIT, this is impossible

• The de-phosphorylation of ATP into ADP provides free energy to drive reactions!

Page 30: Redox Geochemistry

Minimum Free Energy for growth

• Minimun free energy for growth = energy to make ATP?

• What factors go into the energy budget of an organism??

Page 31: Redox Geochemistry

REDOX CLASSIFICATION OF NATURAL WATERS

Oxic waters - waters that contain measurable dissolved oxygen.

Suboxic waters - waters that lack measurable oxygen or sulfide, but do contain significant dissolved iron (> ~0.1 mg L-1).

Reducing waters (anoxic) - waters that contain both dissolved iron and sulfide.

Page 32: Redox Geochemistry

The Redox ladder

H2O

H2

O2

H2O

NO3-

N2 MnO2

Mn2+

Fe(OH)3

Fe2+SO4

2-

H2S CO2

CH4

Oxic

Sub-oxicanaerobic

Sulfidic

Methanic

Aerobes

Denitrifiers

Manganese reducers

Sulfate reducers

Methanogens

Iron reducers

The redox-couples are shown on each stair-step, where the most energy is gained at the top step and the least at the bottom step. (Gibb’s free energy becomes more positive going down the steps)