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.

References

↑ Williams, Milton (1948). "An Electrokinetic Transducer". Review of Scientific Instruments (AIP Publishing) 19 (10): 640–646. doi:10.1063/1.1741068. ISSN 0034-6748. PMID 18888189.
↑ Dukhin, S.S.; Mischuk, N.A.; Kuz'Menko, B.B; Il'In, B.I. (1983). "Flow current and potential in a high-frequency acoustic field". Colloid J. 45 (5): 875–881.

0.00

(0 votes)

Original source: https://en.wikipedia.org/wiki/Streaming vibration current. Read more

[Williams_1948_pp._640–646-1] Williams, Milton (1948). "An Electrokinetic Transducer". Review of Scientific Instruments (AIP Publishing) 19 (10): 640–646. doi:10.1063/1.1741068. ISSN 0034-6748. PMID 18888189.

[2] Dukhin, S.S.; Mischuk, N.A.; Kuz'Menko, B.B; Il'In, B.I. (1983). "Flow current and potential in a high-frequency acoustic field". Colloid J. 45 (5): 875–881.

Streaming Vibration Current

See also

References