- Streaming current
A streaming current or potential is an
electric current or potential which originates when anelectrolyte is driven by a pressure gradient through a channel or porous plug with charged walls. The first observation of the streaming potential is generally attributed to the German physicistGeorg Hermann Quincke in 1859. Streaming currents in well-defined geometries are a sensitive method to characterize thezeta potential of surfaces, which is important in the fields ofcolloid and interface science. They can also be used to generate electrical power, a process which has not been widely applied so far due to its low efficiency.Origin of the streaming current
Adjacent to the channel walls, the charge-neutrality of the liquid is violated due to the presence of an
electrical double layer : a thin layer ofcounterion s attracted by the charged surface. The transport of these counterions along with the pressure-driven fluid flow gives rise to a net charge transport: the streaming current. The opposite effect, generating a fluid flow by applying a potential difference, is calledelectroosmotic flow .Measurement method
A typical setup to measure streaming currents consists of two
electrode s 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 electrical current flowing through the electrodes. Alternatively, the electrodes can be left floating, allowing a streaming potential to build up.References:
1) J. Lyklema, Fundamentals of Interface and Colloid Science
2) F.H.J. van der Heyden et al., Phys. Rev. Lett. 95, 116104 (2005)
3) C. Werner et al., J. Colloid Interface Sci. 208, 329 (1998)
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