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Clay Minerals; December 2005; v. 40; no. 4; p. 493-497; DOI: 10.1180/0009855054040186
© 2005 Mineralogical Society of Great Britain and Ireland
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Research Paper

Hydraulic conductivity and imbibition speed of solid clay aggregates: two different approaches involving the tortuosity of pathways

J. KONTA

Professor Emeritus, Charles University, Albertov 6, CZ 128 43 Prague 2, Czech Republic

(Received 28 February 2005; revised 27 August 2005)

Two different approaches used to express the tortuosity of water pathways in a solid clay body are known: (1) a static approach based on microscopic measurement in thin sections; and (2) a dynamic approach based on ‘imbibition’ speed. Each is expressed by a corresponding equation. The second method has the following advantages over the first: (a) it enables the testing of a much larger volume than that observed in a common thin section; (b) it measures the effects of all particles, including the finest fragments barely visible under optical microscope which also have influence on hydraulic conductivity or the imbibition speed of water; (c) in the case of expansible clays, the magnitude of k (tortuosity of pathways including the shape of particles) can be compared with k for non-expansible clays using a non-polar liquid, e.g. tetraline; (d) the measurement of the imbibition speed into the clay aggregate through a constant area is automated. Specific properties and processes important for sealing clays are discussed in the connection with the dynamic approach.

KEYWORDS: compacted clays, hydraulic conductivity, imbibition speed, tortuosity of pathways, non-expansible clays, expansible clays




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