Physical, chemical and mineralogical influences on the rheology of remoulded low-activity sensitive marine clay

• Published in: Applied clay science 1999-04, Vol.14 (4), p.199-223
• Main Author: Torrance, J.Kenneth
• Format: Article
• Language: English
• Subjects: Earth sciences; Earth, ocean, space; Exact sciences and technology; grain size; ion saturation; Mineralogy; oxide minerals; primary minerals; rheology; salinity; sensitive clays; Silicates; yield stress
• ISSN: 0169-1317; 1872-9053
• DOI: 10.1016/S0169-1317(98)00057-X

The rheological response of remoulded Leda clay from the South Nation River landslide (1971) site has been investigated using a coaxial viscometer. The yield stress at constant water content was found to: decrease as the pore-water salinity decreased, with the decrease occurring at much lower salinity when Ca-saturated than when Na-saturated; decrease as the clay content of the soil was decreased; decrease upon the extraction of oxide minerals by dithionite–citrate–bicarbonate; decrease when the phyllosilicate content of the soil was depleted by a severe alternating acid/base extraction procedure; increase as the pH of the marine clay, whether carbonate-containing or carbonate-free, was lowered by acid addition. The effects are in agreement with expectations based on electrical double-layer theory. The relative effects of the various pretreatments are qualitatively discussed. Viscoplastic-shear-thinning and Bingham plastic response most commonly occurred, although at low salinities viscoplastic-shear-thickening response was exhibited for materials with high silt contents and after phyllosilicate-depletion. No relationship between flow type and the tendency to exhibiting quick clay behaviour is apparent.