2010
DOI: 10.1061/(asce)gt.1943-5606.0000367
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Evaporation, Unsaturated Flow, and Salt Accumulation in Multilayer Deposits of “Paste” Gold Tailings

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Cited by 49 publications
(35 citation statements)
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“…This decline may be accelerated by high salinity (or high concentrations of dissolved mass in the pore water) -as salinity decreases evaporation by multiple mechanisms of osmotic suction, high albedo (reflectivity to shortwave radiation), and formation of a salt crust Dunmola 2012). While cracking does occur, the frequency and size of the cracks appear insufficient to substantially increase evaporation in low-plasticity hard rock tailings (Simms et al 2007;Fisseha et al 2010;Daliri et al 2016). In tailings with significant clay content, however, cracking appears to be a very important mechanism to maintain relatively high evaporation rates.…”
Section: Evaporationmentioning
confidence: 99%
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“…This decline may be accelerated by high salinity (or high concentrations of dissolved mass in the pore water) -as salinity decreases evaporation by multiple mechanisms of osmotic suction, high albedo (reflectivity to shortwave radiation), and formation of a salt crust Dunmola 2012). While cracking does occur, the frequency and size of the cracks appear insufficient to substantially increase evaporation in low-plasticity hard rock tailings (Simms et al 2007;Fisseha et al 2010;Daliri et al 2016). In tailings with significant clay content, however, cracking appears to be a very important mechanism to maintain relatively high evaporation rates.…”
Section: Evaporationmentioning
confidence: 99%
“…For hard rock thickened tailings of low plasticity, the evaporation rate follows classic soil drying (Simms et al 2007;Fisseha et al 2010;Daliri et al 2016), where evaporation decreases with time after deposition of fresh tailings. This decline may be accelerated by high salinity (or high concentrations of dissolved mass in the pore water) -as salinity decreases evaporation by multiple mechanisms of osmotic suction, high albedo (reflectivity to shortwave radiation), and formation of a salt crust Dunmola 2012).…”
Section: Evaporationmentioning
confidence: 99%
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“…The water-retention curves were determined using the axis-translation technique with sample volume measurement in a 'Fredlund' soil water characteristic curve (SWCC) device from GCTS for matric suction values less than 500 kPa, while drier samples were analysed using a WP4 hygrometer for total suction (Leong et al, 2003). The axistranslation technique with volume change was performed as first described by Fisseha et al (2010). Vertical volume change is estimated using non-contact ultrasonic displacement sensors, between each stage in the axis-translation test, while crack volumes are estimated by hand measurements using callipers.…”
Section: Methodsmentioning
confidence: 99%