Streaming current

Last updated February 18, 2022

A streaming current and streaming potential are two interrelated electrokinetic phenomena studied in the areas of surface chemistry and electrochemistry. They are an electric current or potential which originates when an electrolyte is driven by a pressure gradient through a channel or porous plug with charged walls.^[1]^[2]^[3]

Applications

Streaming currents in well-defined geometries are a sensitive method to characterize the zeta potential of surfaces, which is important in the fields of colloid and interface science.^[1] In geology, measurements of related spontaneous potential are used for evaluations of formations. Streaming potential has to be considered in design for flow of poorly conductive fluids (e.g., gasoline lines) because of the danger of buildup of high voltages. The streaming current monitor (SCM) is a fundamental tool for monitoring coagulation in wastewater treatment plants. The degree of coagulation of raw water may be monitored by the use of an SCM to provide a positive feedback control of coagulant injection. As the streaming current of the wastewater increases, more coagulant agent is injected into the stream. The higher levels of coagulant agent cause the small colloidal particles to coagulate and sediment out of the stream. Since less colloid particles are in the wastewater stream, the streaming potential decreases. The SCM recognizes this and subsequently reduces the amount of coagulant agent injected into the wastewater stream. The implementation of SCM feedback control has led to a significant materials cost reduction, one that was not realized until the early 1980s.^[4] In addition to monitoring capabilities, the streaming current could, in theory, generate usable electrical power. This process, however, has yet to be applied as typical streaming potential mechanical to electrical efficiencies are around 1%.^[5]

Origin

Adjacent to the channel walls, the charge-neutrality of the liquid is violated due to the presence of the electrical double layer: a thin layer of counterions attracted by the charged surface.^[1]^[6]

The transport of counterions along with the pressure-driven fluid flow gives rise to a net charge transport: the streaming current. The reverse effect, generating a fluid flow by applying a potential difference, is called electroosmotic flow.^[6]^[7]^[8]

Measurement method

A typical setup to measure streaming currents consists of two reversible electrodes placed on either side of a fluidic geometry across which a known pressure difference is applied. When both electrodes are held at the same potential, the streaming current is measured directly as the electric current flowing through the electrodes. Alternatively, the electrodes can be left floating, allowing a streaming potential to build up between the two ends of the channel.

A streaming potential is defined as positive when the electric potential is higher on the high pressure end of the flow system than on the low pressure end.

The value of streaming current observed in a capillary is usually related to the zeta potential through the relation:^[9]

I_{str}=-{\frac {\epsilon _{rs}\epsilon _{0}a^{2}\pi }{\eta }}{\frac {\Delta P}{L}}\zeta

.

The conduction current, which is equal in magnitude to the streaming current at steady state, is:

I_{c}=K_{L}a^{2}\pi {\frac {U_{str}}{L}}

At steady state, the streaming potential built up across the flow system is given by:

U_{str}={\frac {\epsilon _{rs}\epsilon _{0}\zeta }{\eta K_{L}}}\Delta P

Symbols:

I_str - streaming current under short-circuit conditions, A
U_str - streaming potential at zero net current conditions, V
I_c - conduction current, A
ε_rs - relative permittivity of the liquid, dimensionless
ε₀ - electrical permittivity of vacuum, F·m⁻¹
η - dynamic viscosity of the liquid, kg·m⁻¹·s⁻¹
ζ - zeta potential, V
ΔP - pressure difference, Pa
L - capillary length, m
a - capillary radius, m
K_L - specific conductivity of the bulk liquid, S·m⁻¹

The equation above is usually referred to as the Helmholtz–Smoluchowski equation.

The above equations assume that:

the double layer is not too large compared to the pores or capillaries (i.e., $\kappa a\gg 1$ ), where κ is the reciprocal of the Debye length
there is no surface conduction (which typically may become important when the zeta potential is large, e.g., |ζ| > 50 mV)
there is no electrical double layer polarization
the surface is homogeneous in properties^[10]
there is no axial concentration gradient
the geometry is that of a capillary/tube.

Literature

J. Lyklema, Fundamentals of Interface and Colloid Science
F.H.J. van der Heyden et al., Phys. Rev. Lett. 95, 116104 (2005)
C. Werner et al., J. Colloid Interface Sci. 208, 329 (1998)
Mansouri et al. The Journal of Physical Chemistry C, 112(42), 16192 (2008)

Related Research Articles

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References

1 2 3 Lyklema, J. (1995). Fundamentals of Interface and Colloid Science. Academic Press.
↑ Li, D. (2004). Electrokinetics in Microfluidics. Academic Press.
↑ Chang, H.C., Yeo, L. (2009). Electrokinetically Driven Microfluidics and Nanofluidics. Cambridge University Press.{{cite book}}: CS1 maint: multiple names: authors list (link)
↑ "Archived copy" (PDF). Archived from the original (PDF) on 2016-03-04. Retrieved 2013-05-07.{{cite web}}: CS1 maint: archived copy as title (link)
↑ Olthuis, Wouter; Schippers, Bob; Eijkel, Jan; Van Den Berg, Albert (2005). "Energy from streaming current and potential". Sensors and Actuators B: Chemical. 111–112: 385–389. CiteSeerX 10.1.1.590.7603 . doi:10.1016/j.snb.2005.03.039.
1 2 Kirby, B.J. (2010). Micro- and Nanoscale Fluid Mechanics: Transport in Microfluidic Devices. Cambridge University Press. ISBN 978-0-521-11903-0.
↑ Bruus, H. (2007). Theoretical Microfluidics. Oxford University Press.
↑ Karniadakis, G.M., Beskok, A., Aluru, N. (2005). Microflows and Nanoflows. Springer Verlag.{{cite book}}: CS1 maint: multiple names: authors list (link)
↑ "Measurement and Interpretation of Electrokinetic Phenomena", International Union of Pure and Applied Chemistry, Technical Report, published in Pure Appl. Chem., vol 77, 10, pp. 1753–1805, 2005 (pdf).
↑ Menachem Elimelech and Amy E. Childress, "Zeta Potential of Reverse Osmosis Membranes: Implications for Membrane Performance". U.S. Department of the Interior, Bureau of Reclamation, Denver Office. Water Treatment Technology Program Report No. 10. December 1996.

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[Lyklema-1] 1 2 3 Lyklema, J. (1995). Fundamentals of Interface and Colloid Science. Academic Press.

[Li-2] Li, D. (2004). Electrokinetics in Microfluidics. Academic Press.

[Chang-3] Chang, H.C., Yeo, L. (2009). Electrokinetically Driven Microfluidics and Nanofluidics. Cambridge University Press.{{cite book}}: CS1 maint: multiple names: authors list (link)

[4] "Archived copy" (PDF). Archived from the original (PDF) on 2016-03-04. Retrieved 2013-05-07.{{cite web}}: CS1 maint: archived copy as title (link)

[5] Olthuis, Wouter; Schippers, Bob; Eijkel, Jan; Van Den Berg, Albert (2005). "Energy from streaming current and potential". Sensors and Actuators B: Chemical. 111–112: 385–389. CiteSeerX 10.1.1.590.7603 . doi:10.1016/j.snb.2005.03.039.

[Kirby-6] 1 2 Kirby, B.J. (2010). Micro- and Nanoscale Fluid Mechanics: Transport in Microfluidic Devices. Cambridge University Press. ISBN 978-0-521-11903-0.

[Bruus-7] Bruus, H. (2007). Theoretical Microfluidics. Oxford University Press.

[Karniadakis-8] Karniadakis, G.M., Beskok, A., Aluru, N. (2005). Microflows and Nanoflows. Springer Verlag.{{cite book}}: CS1 maint: multiple names: authors list (link)

[9] "Measurement and Interpretation of Electrokinetic Phenomena", International Union of Pure and Applied Chemistry, Technical Report, published in Pure Appl. Chem., vol 77, 10, pp. 1753–1805, 2005 (pdf).

[10] Menachem Elimelech and Amy E. Childress, "Zeta Potential of Reverse Osmosis Membranes: Implications for Membrane Performance". U.S. Department of the Interior, Bureau of Reclamation, Denver Office. Water Treatment Technology Program Report No. 10. December 1996.

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