Proceedings of the 21st International Seminar on Paste and Thickened Tailings 2018
DOI: 10.36487/acg_rep/1805_09_reid
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A geological principle for the density of thickened tailings

Abstract: The strength of thickened tailings, under both static and earthquake loads, depends on its state parameter. The state parameter can be measured by cone penetration test (CPT) soundings within an existing impoundment, but that does not help when designing/planning a new storage facility. In particular, there are currently no known laboratory sample preparation methods that can reliably replicate the depositional environment of silt/sand tailings within a tailings area, including the resulting in situ state. The… Show more

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Cited by 3 publications
(2 citation statements)
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“…The CSL measured using moist tamped (MT) specimens is shown along with the range of consolidated densities achieved from 10 tests on intact specimens trimmed from blocks. These are seen to 'straddle' the CSL, exactly consistent with the observations of Reid & Jefferies (2018) with respect to the likely states of such deposits. Conversely, the SD triaxials carried out achieve significantly denser states than appear realistic for in situ conditions.…”
Section: Comparison To In Situ Densitiessupporting
confidence: 83%
“…The CSL measured using moist tamped (MT) specimens is shown along with the range of consolidated densities achieved from 10 tests on intact specimens trimmed from blocks. These are seen to 'straddle' the CSL, exactly consistent with the observations of Reid & Jefferies (2018) with respect to the likely states of such deposits. Conversely, the SD triaxials carried out achieve significantly denser states than appear realistic for in situ conditions.…”
Section: Comparison To In Situ Densitiessupporting
confidence: 83%
“…The Plewes Method indicates a quite loose state within the sampled depth range of 7.0 to 8.8m, with Ψ values of +0.10 to +0.20. This is consistent with this area having historically undergone subaqueous deposition, which tends to result in extremely loose states (Shuttle and Cunning 2007;Reid and Jefferies 2017;Reid et al 2018;Reid et al 2019). Outside of this particular zone of subaqueous deposition, Ψ ranges between about -0.05 and +0.10, which is a range more consistent (e.g.…”
Section: Cpt Interpretationsupporting
confidence: 82%