1973
DOI: 10.1007/bf00645873
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Heats of transport of some chlorides in H2O and D2O

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1974
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Cited by 6 publications
(5 citation statements)
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“…( 9) for α ± is probably not accurate when D + ≈ D − , as the term 1/(D + − D − ) becomes very sensitive to uncertainty (and ρ s -dependence) in the ionic diffusivities. Interestingly, the aforementioned works [7,16,17,45] that determined α + +α − from S early − S late did not suffer from the same diverging factor, probably because these authors included into Eq. ( 1) only the cationic species with which their electrodes reacted electrochemically.…”
Section: B Determining Single-ion Soret Coefficients From the Time-dependent Seebeck Coefficientmentioning
confidence: 99%
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“…( 9) for α ± is probably not accurate when D + ≈ D − , as the term 1/(D + − D − ) becomes very sensitive to uncertainty (and ρ s -dependence) in the ionic diffusivities. Interestingly, the aforementioned works [7,16,17,45] that determined α + +α − from S early − S late did not suffer from the same diverging factor, probably because these authors included into Eq. ( 1) only the cationic species with which their electrodes reacted electrochemically.…”
Section: B Determining Single-ion Soret Coefficients From the Time-dependent Seebeck Coefficientmentioning
confidence: 99%
“…The above-mentioned literature values for Q * i essentially all derive from Soret effect experiments that measured the sum α + +α − [1,7,16,17,45]. From these data, the single-ion Soret coefficients α + and α − were determined either by (arbitrarily) setting α Cl = 0 as a reference point [1] or by the "reduction rule" of Takeyema and Nakashima [18].…”
Section: B Determining Single-ion Soret Coefficients From the Time-dependent Seebeck Coefficientmentioning
confidence: 99%
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