Modern Aspects of Electrochemistry
DOI: 10.1007/0-306-46916-2_4
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Electro-Osmotic Dewatering of Clays, Soils, and Suspensions

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Cited by 4 publications
(2 citation statements)
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“…If one conducts electroosmosis without the externally applied pressure, the governing equation for total volume flux of water, q , reads as follows [ 25 ]: where Δ U [V] is the electric potential difference, l [cm] is the length of soil specimen, k e [cm 2 /(s•V)] is the electroosmotic permeability, A [cm 2 ] is the effective cross section. In this experiment, V/cm, A = 100 cm 2 , Q / t = 13.59/3600 = 3.775 ×10 −3 mL/s ( t < 12 h ).…”
Section: Resultsmentioning
confidence: 99%
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“…If one conducts electroosmosis without the externally applied pressure, the governing equation for total volume flux of water, q , reads as follows [ 25 ]: where Δ U [V] is the electric potential difference, l [cm] is the length of soil specimen, k e [cm 2 /(s•V)] is the electroosmotic permeability, A [cm 2 ] is the effective cross section. In this experiment, V/cm, A = 100 cm 2 , Q / t = 13.59/3600 = 3.775 ×10 −3 mL/s ( t < 12 h ).…”
Section: Resultsmentioning
confidence: 99%
“…If one conducts electroosmosis without the externally applied pressure, the governing equation for total volume flux of water, q, reads as follows [25]:…”
Section: Plos Onementioning
confidence: 99%