Redox Geochemistry

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Redox Geochemistry

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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 DG0R ... – PowerPoint PPT presentation

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Title: Redox Geochemistry


1
Redox Geochemistry
2
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 DG0R DH0R TDS0R
  • Gibbs Free Energy (G) is a state variable,
    measured in KJ/mol or Cal/mol
  • Tabulated values of DG0R available

3
Equilibrium Constant
  • for aA bB ? cC dD
  • Restate the equation as
  • DGR DG0R RT ln Q
  • DGR 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

4
Activity
  • Activity, a, is the term which relates Gibbs Free
    Energy to chemical potential
  • mi-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

5
Ions in solution
  • Ions in solutions are obviously nonideal states!
  • Use activities (ai) to apply thermodynamics and
    law of mass action
  • ai gimi
  • The activity coefficient, gi, is found via some
    empirical foundations

6
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)

7
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 CaHPO40
  • CaCO30
  • Plus more species ? gases and minerals!!

8
Mass Action Mass Balance
  • mCa2mCa2MCaCl mCaCl20 CaCL3- CaHCO3
    CaCO30 CaF CaSO40 CaHSO4 CaOH
  • Final equation to solve the problem sees the mass
    action for each complex substituted into the mass
    balance equation

9
Geochemical models
  • Hundreds of equations solved iteratively for
    speciation, solve for DGR
  • All programs work on same concept for speciation
    thermodynamics and calculations of mineral
    equilibrium lots of variation in output,
    specific info

10
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 Ox2

LEO says GER
11
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

12
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

13
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 electron.
  • If pe is low, there is a strong tendency for the
    solution to donate electron - the solution is
    reducing.
  • If pe is high, there is a strong tendency for the
    solution to accept electron - the solution is
    oxidizing.

14
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

15
DEFINITION OF Eh
  • Eh - 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 (Faradays
    constant).
  • At 25C, this becomes
  • or

16
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 DGr ??
  • DGr - n?E
  • Where n is the of e-s in the rxn, ? is
    Faradays 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

17
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

At 25 C
18
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 DGr -n?E, combining two half reactions
    in a certain way will yield either a or
    electropotential (additive, remember to switch
    sign when reversing a rxn)
  • E ? - DGr, therefore ? spontaneous
  • In order of decreasing strength as a reducing
    agent ? strong reducing agents are better e-
    donors

19
  • Redox reactions with more negative reduction
    potentials will donate electrons to redox
    reactions with more positive potentials.
  • NADP 2H 2e- ? NADPH H -0.32
  • O2 4H 4e- ? 2H2O 0.81
  • NADPH H ? NADP 2H 2e- 0.32
  • O2 4H 4e- ? 2H2O 0.81
  • 2 NADPH O2 2H ? 2 NADP 2 H2O 1.13

20
ELECTRON TOWER
more negative
oxidized/reduced forms potential acceptor/donor
more positive
BOM Figure 5.9
21
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22
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

23
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

24
  • transport of
  • electrons coupled
  • to pumping protons

CH2O ? CO2 4 e- H 0.5 O2 4e- 4H ?
H2O
25
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

26
HOW IS THE PMF USED TO SYNTHESIZE ATP?
  • catalyzed by ATP synthase

BOM Figure 5.21
27
ATP generation II
  • Alternative methods to form ATP
  • Phosphorylation ? coupled to fermentation, low
    yield of ATP

28
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!

29
Minimum Free Energy for growth
  • Minimum free energy for growth energy to make
    ATP?
  • What factors go into the energy budget of an
    organism??

30
Growth Efficiency
  • How much energy does it take to grow a new
    microbe?
  • How much energy does a microbe gain from any
    metabolic reaction?
  • How much energy is wasted, i.e., how much
    energy does it cost the microbe to hang out in
    its environment that is not directly attributed
    to the energy required for growth and division
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