Streaming vibration current

The streaming vibration current (SVI) and the associated streaming vibration potential is an electric signal that arises when an acoustic wave propagates through a porous body in which the pores are filled with fluid.

Streaming vibration current was experimentally observed in 1948 by M. Williams.[1] A theoretical model was developed some 30 years later by Dukhin and coworkers.[2] This effect opens another possibility for characterizing the electric properties of the surfaces in porous bodies.

See also

References

  1. ↑ Williams, M. "An Electrokinetic Transducer" The review of scientific instruments, 19, 10, 640–646, 1948
  2. ↑ Dukhin, S.S., Mischuk, N.A., Kuz’menko, B.B and Il’in, B.I. "Flow current and potential in a high-frequency acoustic field" Colloid J., 45, 5, 875–881,1983


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