oxidation reduction - department of chemistry

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Oxidation Reduction Oxidation-Reduction Reactions

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Page 1: Oxidation Reduction - Department of Chemistry

Oxidation Reduction

Oxidation-Reduction Reactions

Page 2: Oxidation Reduction - Department of Chemistry

ReductionOxidation

Oxidation-Reduction Reactions

Page 3: Oxidation Reduction - Department of Chemistry

Half Cell Potentials are always written as reductions:

Half Cell Potentials

EFeECe

Page 4: Oxidation Reduction - Department of Chemistry

Half Cell Reaction for Hydrogen:

Since we always use half cell differences, we can add an arbitrary constant to all half cells. By convention, we assume that the Eo for the normal hydrogen electrode (NHE) is equal to zero:

Page 5: Oxidation Reduction - Department of Chemistry

Half Cell Potentials are always written as reductions:

Half Cell Potentials

EFeECe

E°(Fe) = +0.77 V E°(Ce) = +1.61 V

E°(Cell) = E°(Fe) - E°(Ce) = - 0.91 V

Spontaneous?

Page 6: Oxidation Reduction - Department of Chemistry

Half Cell Potentials are always written as reductions:

Half Cell Potentials

EFeECe

E°(Fe) = +0.77 V E°(Ce) = +1.61 V

E°(Cell) = E°(Fe) - E°(Ce) = - 0.91 V

Not Spontaneous - Electrolytic Cell!

The reverse reaction is spontaneous - Galvanic Cell.

Page 7: Oxidation Reduction - Department of Chemistry

UC Davis chemwiki.

Redox Titrations

Ce4+

Fe2+

Ce4+ + Fe2+ = Ce3+ + Fe3+

This reaction is spontaneous!

Page 8: Oxidation Reduction - Department of Chemistry
Page 9: Oxidation Reduction - Department of Chemistry

Electrochemical Alpha Fractions

EFe is called theRedox Potential

Page 10: Oxidation Reduction - Department of Chemistry

Electrolysis of Water

At the positively charged anode, an oxidation reaction occurs, generating oxygen gas (these equations are for acidic pH):

Oxidation at anode: 2 H2O(l) → O2(g) + 4 H+(aq) + 4e

At the negatively charged cathode, a reduction reaction occurs,generating hydrogen gas:

Reduction at cathode: 2 H+(aq) + 2e− → H2(g)

Half Cell Potentials:

O2(g) + 4 H+(aq) + 4e− → 2 H2O(l) E° = +1.229 V

2 H+(aq) + 2e− → H2(g) E° = -0.8277 V

E°(cell) = E°(red) - E°(ox) = -0.8277 – 1.229 = -2.056 V

Reduction is on the left in this picture (sorry)

Spontaneous?

Page 11: Oxidation Reduction - Department of Chemistry

Electrolysis of Water

At the positively charged anode, an oxidation reaction occurs, generating oxygen gas (these equations are for acidic pH):

Oxidation at anode: 2 H2O(l) → O2(g) + 4 H+(aq) + 4e

At the negatively charged cathode, a reduction reaction occurs,generating hydrogen gas:

Reduction at cathode: 2 H+(aq) + 2e− → H2(g)

Half Cell Potentials:

O2(g) + 4 H+(aq) + 4e− → 2 H2O(l) E° = +1.229 V

2 H+(aq) + 2e− → H2(g) E° = -0.8277 V

E°(cell) = E°(red) - E°(ox) = -0.8277 – 1.229 = -2.056 V

Reduction is on the left in this picture (sorry)

Not Spontaneous - Electrolytic Cell!

Page 12: Oxidation Reduction - Department of Chemistry

pE and Pourbaix Diagrams

“In complex mixtures such as natural waters and cellular fluids, a variety of redox couples are usually present. In most cases of practical interest one couple will dominate all the other redox equilibria by virtue of its greater concentration. Just as the pH of a solution containing a mixture of weak acid-base systems can be considered as a master variable that defines the composition of the system (which can then be manipulated by addition of strong acid or strong base), so the pE of a dominant redox system can be regarded as a similar master variable that controls the redox balance of the other couples in the system.

There is one major distinction in this analogy between the pH and the pE that cannot be too strongly emphasized, however. Whereas proton-transfer reactions are among the most rapid ones known, electron-transfer reactions are frequently extremely slow, so in the absence of catalytic mediation, one cannot depend on redox systems to be anywhere near equilibrium.”

pE = E/0.0592E is the Redox Potential vs. NHE

From: Redox equilibria in natural watersStephen K. Lower

Simon Fraser University

Page 13: Oxidation Reduction - Department of Chemistry

Water Stability pE Range

pE = E/0.0592

Redox equilibria in natural waters, S. K. Lower, SFU

Page 14: Oxidation Reduction - Department of Chemistry

Iron speciation plot with water stability region outlined

Redox equilibria in natural waters, S. K. Lower, SFU

Page 15: Oxidation Reduction - Department of Chemistry

Pourbaix Diagram: pE vs pH

Redox equilibria in natural waters, S. K. Lower, SFU

sometimes EH instead of pE

Page 16: Oxidation Reduction - Department of Chemistry

Aquatic Chemistry Concepts, JF Pankow 1991.

Pourbaix Diagram: pE vs pH

Page 17: Oxidation Reduction - Department of Chemistry

Aquatic Chemistry Concepts, JF Pankow 1991.

CarbonatesPourbaix Diagram: pE vs pH

Page 18: Oxidation Reduction - Department of Chemistry

Aquatic Chemistry Concepts, JF Pankow 1991.

Nitrogen SpeciesPourbaix Diagram: pE vs pH

Page 19: Oxidation Reduction - Department of Chemistry

Wikipedia.

Trace Metals

Chromium Uranium

Pourbaix Diagram: pE vs pH

Page 20: Oxidation Reduction - Department of Chemistry

Wikipedia.

Trace Metals

Vanadium

Pourbaix Diagram: pE vs pH

Four stable oxidation states:

V2+, V3+, VO2+, VO2+

Page 21: Oxidation Reduction - Department of Chemistry

Vanadium Redox Flow Battery

Seattle Business Magazine

Four stable oxidation states:

V2+, V3+, VO2+, VO2+

Galvanic Discharging Reaction

Anode (Oxidation): V2+ → V3+ + e- (E° = -0.26 V vs. SHE)

Cathode (Reduction): VO2+ + 2 H+ + e- → VO2+ + H2O (E° = 0.99 V)

E°(Cell) = E°(Red) - E°(Ox) = 0.99 + 0.26 = +1.25V

Page 22: Oxidation Reduction - Department of Chemistry
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Page 25: Oxidation Reduction - Department of Chemistry

Alkaline Battery (Zn-MnO2)