Current-Induced Membrane Discharge
Publication: Research - peer-review › Journal article – Annual report year: 2012
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Current-Induced Membrane Discharge. / Andersen, Mathias Bækbo; van Soestbergen, M.; Mani, A.; Bruus, Henrik; Biesheuvel, P. M.; Bazant, M. Z.
In: Physical Review Letters, Vol. 109, No. 10, 2012, p. Paper 108301.Publication: Research - peer-review › Journal article – Annual report year: 2012
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TY - JOUR
T1 - Current-Induced Membrane Discharge
A1 - Andersen,Mathias Bækbo
A1 - van Soestbergen,M.
A1 - Mani,A.
A1 - Bruus,Henrik
A1 - Biesheuvel,P. M.
A1 - Bazant,M. Z.
AU - Andersen,Mathias Bækbo
AU - van Soestbergen,M.
AU - Mani,A.
AU - Bruus,Henrik
AU - Biesheuvel,P. M.
AU - Bazant,M. Z.
PB - American Physical Society
PY - 2012
Y1 - 2012
N2 - Possible mechanisms for overlimiting current (OLC) through aqueous ion-exchange membranes (exceeding diffusion limitation) have been debated for half a century. Flows consistent with electro-osmotic instability have recently been observed in microfluidic experiments, but the existing theory neglects chemical effects and remains to be quantitatively tested. Here, we show that charge regulation and water self-ionization can lead to OLC by "current-induced membrane discharge'' (CIMD), even in the absence of fluid flow, in ion-exchange membranes much thicker than the local Debye screening length. Salt depletion leads to a large electric field resulting in a local pH shift within the membrane with the effect that the membrane discharges and loses its ion selectivity. Since salt co-ions, H+ ions, and OH- ions contribute to OLC, CIMD interferes with electrodialysis (salt counterion removal) but could be exploited for current-assisted ion exchange and pH control. CIMD also suppresses the extended space charge that leads to electroosmotic instability, so it should be reconsidered in both models and experiments on OLC.
AB - Possible mechanisms for overlimiting current (OLC) through aqueous ion-exchange membranes (exceeding diffusion limitation) have been debated for half a century. Flows consistent with electro-osmotic instability have recently been observed in microfluidic experiments, but the existing theory neglects chemical effects and remains to be quantitatively tested. Here, we show that charge regulation and water self-ionization can lead to OLC by "current-induced membrane discharge'' (CIMD), even in the absence of fluid flow, in ion-exchange membranes much thicker than the local Debye screening length. Salt depletion leads to a large electric field resulting in a local pH shift within the membrane with the effect that the membrane discharges and loses its ion selectivity. Since salt co-ions, H+ ions, and OH- ions contribute to OLC, CIMD interferes with electrodialysis (salt counterion removal) but could be exploited for current-assisted ion exchange and pH control. CIMD also suppresses the extended space charge that leads to electroosmotic instability, so it should be reconsidered in both models and experiments on OLC.
UR - http://prl.aps.org/abstract/PRL/v109/i10/e108301
U2 - 10.1103/PhysRevLett.109.108301
DO - 10.1103/PhysRevLett.109.108301
JO - Physical Review Letters
JF - Physical Review Letters
SN - 0031-9007
IS - 10
VL - 109
SP - Paper 108301
ER -