Geochemistry. William M. White

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Geochemistry - William M. White

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electrode potential, or simply the potential of the reaction.

      If we could measure the potential of two separate half-cell reactions:

equation equation

       3.11.1.1 Hydrogen scale potential, EH

      The established convention is to measure potentials in a standard hydrogen electrode cell (at standard temperature and pressure). The cell consists on one side of a platinum plate coated with fine Pt powder that is surrounded by H2 gas maintained at a partial pressure of 1 atm and immersed in a solution of unit H+ activity. The other side consists of the electrode and solution under investigation. A potential of 0 is assigned to the half-cell reaction:

      (3.104)equation

      where the subscript g denotes the gas phase. The potential measured for the entire reaction is then assigned to the half-cell reaction of interest. Thus, for example, the potential of the reaction:

equation

      is –0.763 V. This value is assigned to the reaction:

Half-cell reaction EH° (V) pε°
Li+ + e ⇌ Li −3.05 −51.58
Ca2+ + 2 e ⇌ Ca −2.93 −49.55
Th4+ + 4e ⇌ Th −1.83 −30.95
U4+ + 4e ⇌ U −1.38 −23.34
Mn2+ +2e ⇌ Mn −1.18 −19.95
Zn2+ + 2e ⇌ Zn −0.76 −12.85
Cr3+ +3e ⇌ Cr −0.74 −12.51
CO2(g) + 4H+ + 4e ⇌ CH2O*+2H2O −0.71 −12.01
Fe2+ + 2e ⇌ Fe −0.44 −7.44
Eu3+ + e ⇌ Eu2+ −0.36 −6.08
Ni2+ + 2e ⇌ Ni −0.26 −4.34
Pb2+ + 2e ⇌ Pb −0.13 −2.2
CrO42− + 4H2O +3e ⇌ Cr(OH)3 + H2O −0.13 −2.2
2H+ + 2e ⇌ H2(g) 0 0
N2(g) + 6H+ + 6e ⇌ 2NH3 0.093 1.58
Cu2+ + 2e ⇌ Cu 0.34 5.75
UO22+ + 2e ⇌ UO2 0.41 6.85
S + 2e ⇌ S2− 0.44 7.44
Cu+ + e ⇌ Cu 0.52 8.79
Fe3+ + e ⇌ Fe2+ 0.77 13.02
NO3+ + 2H+ + e ⇌ NO2(g) + H2O 0.80 13.53
Ag+ + e ⇌ Ag 0.80 13.53
Hg2+ + 2e ⇌ Hg 0.85 14.37
MnO2(s) + 4H+ + 2e ⇌ Mn2+ + 2H2O 1.22 20.63
O2 + 4H+ + 4e ⇌ 2H2O 1.23 20.80
MnO4– + 8H+ + 5e ⇌ Mn2+ + 4H2O 1.51 25.53
Au+ + e ⇌ Au 1.69 28.58
Ce4+ + e ⇌ Ce3+ 1.72 29.05
Pt+ + e ⇌ Pt 2.64 44.64

      *

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