Selected geotechnical properties of various biosolids, sewage sludge and WTR materials
| Material | Liquid limit: % | Plastic limit: % | Plasticity index: % | Specific gravity | TVS: % | pH | Silt- and clay-sized particles: wt% | Rate dependence parameter, μ b | Soil classificationb (BSI, 2015) |
|---|---|---|---|---|---|---|---|---|---|
| Sewage sludge 1 (O’Kelly 2006, 2008b, 2013a, 2013c) | 315 | 55 | 260 | 1·55 | 70 | 8·0 | — | — | Organic clay of extremely high plasticity |
| Sewage sludge 2 (Chen et al., 2014) | 115 | 75 | 40 | 2·05 | 61–70 | — | 48 | — | Organic silt of extremely high plasticity |
| Sewage sludge 3 (Diliūnas et al., 2010) | 352 | 215 | 137 | 1·69 | 57·0 | 7–8 | — | — | Organic silt of extremely high plasticity |
| Sewage sludge 4 (Lin et al., 2013) | — | — | 256 | 1·61 | 43·0 | — | — | — | — |
| Sewage sludge 5 (Zhan et al., 2014) | 353 | 106 | 247 | 1·73–1·95 | 32·3–51·0 | — | 75 | — | Organic clay of extremely high plasticity |
| Sewage sludges 6a–6e (from drying beds) (Stone et al., 1998) | 66–165a | 57–117a | 0–48a | 0·93–2·04 | 14·3–67·2 | — | 0·5–3·5 | — | Organic silt of high to extremely high plasticity |
| Sewage sludge 7 (He et al., 2015) | 515·1 | 94·8 | 420·3 | 1·61 | — | — | — | — | Organic clay of extremely high plasticity |
| Biosolids 1d | 458 | 68 | 390 | 1·68 | 63 | 7·8 | 78 | 0·39 (w = 100%) | Organic clay of extremely high plasticity |
| Biosolids 2 (Kayser et al., 2011) | 666 | 105 | 561 | 1·62 | 66–70 | 8·3 | >92·1 | 0·38 (w = 355%) | Organic clay of extremely high plasticity |
| Biosolids 2 (w = 355%) amended with 20% lime (Kayser et al., 2011) | — | — | — | — | 50–55 | 12·4 | — | 0·34 | — |
| Biosolids 3 (air-dried) (Kim et al., 2005) | 99 | 49 | 50 | 1·56 | 38–41 | 7·9–8·1 | — | — | Organic silt of extremely high plasticity |
| Biosolids 4 (GLSEC, 2003) | 71–119a | 54–85a | 17–53a | 1·81–2·17 | 32–34 | — | 40–50 | — | Organic silt of high to extremely high plasticity |
| Aged biosolids 1 (stockpiled) (Arulrajah et al., 2011, 2013) | 100–110a | 79–83a | 21–27a | 1·86–1·88 | 35·4–38·5 | 4·67 | 37–50 | — | Organic silt of extremely high plasticity |
| Aged biosolids 2 (stockpiled) (Wanigaratne and Udamulla, 2012) | 79·8a | Non-plastica | 0a | 1·93 | 25·5 | — | — | — | Organic silt (non plastic) |
| Aged biosolids 3 (air-dried in stockpile) (Maghoolpilehrood et al., 2013) | 100 | 80 | 20 | 1·77 | 27 | — | — | — | Organic silt of extremely high plasticity |
| Aged biosolids 4 (air-dried in stockpile) (Maghoolpilehrood et al., 2014, 2015) | 61·5a | 25·1a | 36·4a | 2·58 | 9·9–10·4 | 7·38 | 40 | — | Organic clay of high plasticity |
| Aged biosolids 5 (stockpiled, >12 years) (Ukwatta et al., 2015) | 46–67a | 21–41a | 25–33a | 2·43–2·52 | 6·3–14·4 | — | 10–18 | — | Organic clay of intermediate to high plasticity |
| Aged biosolids 6 (stockpiled) (Ukwatta et al., 2016) | 53a | 27a | 26a | 2·51 | 7·1 | — | 10 | — | Organic clay of high plasticity |
| Alum WTR 1 (O’Kelly, 2008a) | 490 | 240 | 250 | 1·86 | 57 | 8·6 | — | — | Organic silt of extremely high plasticity |
| Alum WTR 2 (O’Kelly, 2010) | 550 | 260 | 290 | 1·99 | 45 | 7·1 | — | — | Organic silt of extremely high plasticity |
| Alum WTR 3 (O’Kelly, 2010) | 430 | 220 | 210 | 1·90 | 46 | 7·2 | — | — | Organic silt of extremely high plasticity |
| Alum WTR 4 (O’Kelly, 2014a, 2014b, 2016c) | 513 | 268 | 245 | 1·86 | 57 | 8·6 | — | 0·20 (w = 222%) | Organic silt of extremely high plasticity |
| Alum WTR 5 (Wang et al., 1992; Wang and Tseng, 1993) | 550 | 239 | 311 | 2·26 | — | — | — | — | Organic silt of extremely high plasticity |
| Alum WTR 6 (Wang et al., 1992) | 423 | 137 | 286 | 2·33 | — | — | — | — | Organic silt of extremely high plasticity |
| Alum WTR 7 (Basim, 1999) | 371 | 228 | 143 | 1·88 | 38 | — | 81 | — | Organic silt of extremely high plasticity |
| Alum WTR 8 (Basim, 1999) | 206 | 115 | 91 | 2·00 | 30 | — | 69 | — | Organic silt of extremely high plasticity |
| Alum WTR 9 (Roque and Carvalho, 2006) | 107·5 | 81·7 | 25·8 | 2·27 | 10 | — | 86 | — | Organic silt of extremely high plasticity |
| Alum and lime WTR 1 (Basim, 1999) | 329 | 200 | 129 | 2·38 | 30 | — | 98 | — | Organic silt of extremely high plasticity |
| Alum and lime WTR 2 (Raghu and Hsieh, 1986) | — | — | c | 1·90 | 33·5 | — | 84 | — | — |
| Alum and polymer WTR 1 (Basim, 1999) | 690 | 20 | 670 | 2·12 | 38 | — | 56 | — | Organic clay of extremely high plasticity |
| Polymer WTR 1 (Basim, 1999) | 161 | 57 | 104 | 2·26 | 31 | — | 71 | — | Organic clay of extremely high plasticity |
| Iron WTR 1 (Wang et al., 1992) | 108 | 47 | 61 | 2·72 | — | — | — | — | Organic silt of extremely high plasticity |
| Lime-softening sludge 1 (Raghu and Hsieh, 1986) | 38 | 31 | 7 | 2·65 | 9·3 | — | 51 | — | Silt of intermediate plasticity |
| Lime-softening sludge 2 (Fei et al., 2016) | 38 | 32 | 6 | 2·57 | — | 11 | 83 | — | Silt of intermediate plasticity |
| Material | Liquid limit: % | Plastic limit: % | Plasticity index: % | Specific gravity | pH | Silt- and clay-sized particles: wt% | Rate dependence parameter, | Soil classification | |
|---|---|---|---|---|---|---|---|---|---|
| Sewage sludge 1 ( | 315 | 55 | 260 | 1·55 | 70 | 8·0 | — | — | Organic clay of extremely high plasticity |
| Sewage sludge 2 ( | 115 | 75 | 40 | 2·05 | 61–70 | — | 48 | — | Organic silt of extremely high plasticity |
| Sewage sludge 3 ( | 352 | 215 | 137 | 1·69 | 57·0 | 7–8 | — | — | Organic silt of extremely high plasticity |
| Sewage sludge 4 ( | — | — | 256 | 1·61 | 43·0 | — | — | — | — |
| Sewage sludge 5 ( | 353 | 106 | 247 | 1·73–1·95 | 32·3–51·0 | — | 75 | — | Organic clay of extremely high plasticity |
| Sewage sludges 6a–6e (from drying beds) ( | 66–165 | 57–117 | 0–48 | 0·93–2·04 | 14·3–67·2 | — | 0·5–3·5 | — | Organic silt of high to extremely high plasticity |
| Sewage sludge 7 ( | 515·1 | 94·8 | 420·3 | 1·61 | — | — | — | — | Organic clay of extremely high plasticity |
| Biosolids 1 | 458 | 68 | 390 | 1·68 | 63 | 7·8 | 78 | 0·39 ( | Organic clay of extremely high plasticity |
| Biosolids 2 ( | 666 | 105 | 561 | 1·62 | 66–70 | 8·3 | >92·1 | 0·38 ( | Organic clay of extremely high plasticity |
| Biosolids 2 ( | — | — | — | — | 50–55 | 12·4 | — | 0·34 | — |
| Biosolids 3 (air-dried) ( | 99 | 49 | 50 | 1·56 | 38–41 | 7·9–8·1 | — | — | Organic silt of extremely high plasticity |
| Biosolids 4 ( | 71–119 | 54–85 | 17–53 | 1·81–2·17 | 32–34 | — | 40–50 | — | Organic silt of high to extremely high plasticity |
| Aged biosolids 1 (stockpiled) ( | 100–110 | 79–83 | 21–27 | 1·86–1·88 | 35·4–38·5 | 4·67 | 37–50 | — | Organic silt of extremely high plasticity |
| Aged biosolids 2 (stockpiled) ( | 79·8 | Non-plastic | 0 | 1·93 | 25·5 | — | — | — | Organic silt (non plastic) |
| Aged biosolids 3 (air-dried in stockpile) ( | 100 | 80 | 20 | 1·77 | 27 | — | — | — | Organic silt of extremely high plasticity |
| Aged biosolids 4 (air-dried in stockpile) ( | 61·5 | 25·1 | 36·4 | 2·58 | 9·9–10·4 | 7·38 | 40 | — | Organic clay of high plasticity |
| Aged biosolids 5 (stockpiled, >12 years) ( | 46–67 | 21–41 | 25–33 | 2·43–2·52 | 6·3–14·4 | — | 10–18 | — | Organic clay of intermediate to high plasticity |
| Aged biosolids 6 (stockpiled) ( | 53 | 27 | 26 | 2·51 | 7·1 | — | 10 | — | Organic clay of high plasticity |
| Alum WTR 1 ( | 490 | 240 | 250 | 1·86 | 57 | 8·6 | — | — | Organic silt of extremely high plasticity |
| Alum WTR 2 ( | 550 | 260 | 290 | 1·99 | 45 | 7·1 | — | — | Organic silt of extremely high plasticity |
| Alum WTR 3 ( | 430 | 220 | 210 | 1·90 | 46 | 7·2 | — | — | Organic silt of extremely high plasticity |
| Alum WTR 4 ( | 513 | 268 | 245 | 1·86 | 57 | 8·6 | — | 0·20 ( | Organic silt of extremely high plasticity |
| Alum WTR 5 ( | 550 | 239 | 311 | 2·26 | — | — | — | — | Organic silt of extremely high plasticity |
| Alum WTR 6 ( | 423 | 137 | 286 | 2·33 | — | — | — | — | Organic silt of extremely high plasticity |
| Alum WTR 7 ( | 371 | 228 | 143 | 1·88 | 38 | — | 81 | — | Organic silt of extremely high plasticity |
| Alum WTR 8 ( | 206 | 115 | 91 | 2·00 | 30 | — | 69 | — | Organic silt of extremely high plasticity |
| Alum WTR 9 ( | 107·5 | 81·7 | 25·8 | 2·27 | 10 | — | 86 | — | Organic silt of extremely high plasticity |
| Alum and lime WTR 1 ( | 329 | 200 | 129 | 2·38 | 30 | — | 98 | — | Organic silt of extremely high plasticity |
| Alum and lime WTR 2 ( | — | — | 1·90 | 33·5 | — | 84 | — | — | |
| Alum and polymer WTR 1 ( | 690 | 20 | 670 | 2·12 | 38 | — | 56 | — | Organic clay of extremely high plasticity |
| Polymer WTR 1 ( | 161 | 57 | 104 | 2·26 | 31 | — | 71 | — | Organic clay of extremely high plasticity |
| Iron WTR 1 ( | 108 | 47 | 61 | 2·72 | — | — | — | — | Organic silt of extremely high plasticity |
| Lime-softening sludge 1 ( | 38 | 31 | 7 | 2·65 | 9·3 | — | 51 | — | Silt of intermediate plasticity |
| Lime-softening sludge 2 ( | 38 | 32 | 6 | 2·57 | — | 11 | 83 | — | Silt of intermediate plasticity |
Measured for air-dry material
Deduced in present investigation
Reported as possessing slight to little plasticity
From forthcoming article entitled ‘Shear strength of biosolids for monofill design’ by Oettle, O’Kelly and Ramos
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