Critical state lines (CSLs) properties of tailings geomaterials
| Tailings type | FC: % | Γ / ℓ | a/b/c | Gs | Μ | Main minerals | Transitional behaviour |
|---|---|---|---|---|---|---|---|
| CoT – copper (current study) | 47·5 | 86S: 1·725/0·060/0·40 | 2·814 | 1·46 (TC) | 17·9% Qtz; 28·4% Alb; 8·3% Feld; 4·9% Bio; 10·1% Chlo; 14·2% Acti; 6·3% Mag | Yes (TC)/No (SS) | |
| 91S: 1·655/0·040/0·40 | |||||||
| 95S: 1·618/0·030/0·40 | |||||||
| 1·720/0·121/0·55 | 1·02 (SS) | ||||||
| CoP – copper (current study) | 42·3 | 2·053/0·074 | 3·149 | 1·40 (TC)/0·99 (SS) | 16·4% Qtz; 4·5% Alb; 3·9% Feld; 23·6% Bio; 15·4% Chlo; 12·0% Grun; 9·1% Gar; 7·9% Mag | No | |
| Copper upper beach (Velten et al., 2024) | 12·5 | 86 N: 1·93/0·05/0·55 | 2·844 | 1·50 (TC) | 25·1% Qtz; 33·5% Feld; 8·4% Scp; 5·8% Amp; 5·8 Chlo; 5·3% Bio; 3·0% Mag | Yes | |
| 91 N: 1·90/0·05/0·55 | |||||||
| 95 N: 1·865/0·05/0·55 | |||||||
| Copper lower beach (Velten et al., 2024) | 25·5 | 86 N: 1·895/0·05/0·55 | 2·943 | 1·40 (TC) | 25·1% Qtz; 33·5% Feld; 8·4% Scp; 5·8% Amp; 5·8 Chlo; 5·3% Bio; 3·0% Mag | Yes | |
| 91 N: 1·865/0·05/0·55 | |||||||
| 95 N: 1·830/0·05/0·55 | |||||||
| Copper S1 (Vergaray et al., 2023) | 15 | 2·013/0·045 | 1·924/0·096/0·421 | 2·70 | 1·55 (TC) | No | |
| Copper S2 (Vergaray et al., 2023) | 38 | 1·876/0·033 | 1·865/0·123/0·275 | 2·60 | 1·54 (TC) | No | |
| Copper S3 (Vergaray et al., 2023) | 75 | 1·860/0·033 | 1·742/0·022/0·856 | 2·75 | 1·49 (TC) | No | |
| Copper TSF2 (Karim et al., 2023) | 3 | — | 1·76/0·0769/0·54 | 2·682 | (τ/σ′N)CS = 0·53 (DSS) | 32% Qtz; 30% Alb; 23% Mu3T; 12% Micr; 2% Kaol; 1% clin | No |
| Deixing copper (Li, 2017) | 95 | 1·84 (Γ100)/0·126 | 1·92/0·070/0·42 | 3·75 | 1·43 (TC) | 78% Fay; 22% Mag | No |
| Brazilian gold (Bedin et al., 2012) | 65 | 1·89 (Γ100)/0·206 | 1·955/0·070/0·65 | 2·89–3·20 | 1·33 (TC) | 27% Qtz; 25% Alb; 35% Chlo | No |
| Brazilian gold (Li et al., 2018) | 95 | 1·89 (Γ100)/0·176 | 2·150/0·25/0·25 | 2·89 | 1·41 (TC) | 27% Qtz; 25% Alb; 35% Chlo | No |
| Panzhihua UB – iron (Li, 2017) | 19 | 1·79 (Γ100)/0·252 | 1·795/0·090/0·39 | 3·37 | 1·41 (TC) | 30% Dio; 32% Lab; 11% Hrb; 9% Chlo | No |
| Panzhihua MB – iron (Li, 2017) | 68 | 1·81 (Γ100)/0·152 | 1·875/0·080/0·39 | 3·14 | 1·36 (TC) | 46% Dio; 40% Lab; 6% Hrb; 5% Chlo | No |
| Panzhihua PO — iron (Li, 2017) | 93 | 1·76 (Γ100)/0·185 | 3·11 | 1·40 (TC) | 28% Dio; 24% Lab; 22% Hrb; 16% Chlo | No | |
| Iron-flotation (Consoli et al., 2024) | 38·6 | 2·00/0·15/0·245 | 2·83 | 1·30 (TC) | 98·3% Qtz; 1·7% Haema | No | |
| Iron-slimes (Consoli et al., 2024) | 86·2 | 1·95/0·15/0·232 | 4·02 | 1·35 (TC) | 54·8% Qtz; 42·3% Haema; 2·9% Kaol | No | |
| Iron-S1 (Wagner et al., 2023) | 52·2 | 1·86/0·045/0·46 | 3·05 | 1·40 (TC)/0·98 (TE) | 76·2% Qtz; 20·9% Ioxi | No | |
| Iron-S2 (Wagner et al., 2023) | 33·3 | 1·74/0·045/0·46 | 2·97 | 1·35 (TC)/0·96 (TE) | 78·4% Qtz; 17·2% Ioxi | No |
| Tailings type | FC: % | Γ / | Μ | Main minerals | Transitional behaviour | ||
|---|---|---|---|---|---|---|---|
| CoT – copper (current study) | 47·5 | 86S: 1·725/0·060/0·40 | 2·814 | 1·46 ( | 17·9% Qtz; 28·4% Alb; 8·3% Feld; 4·9% Bio; 10·1% Chlo; 14·2% Acti; 6·3% Mag | Yes ( | |
| 91S: 1·655/0·040/0·40 | |||||||
| 95S: 1·618/0·030/0·40 | |||||||
| 1·720/0·121/0·55 | 1·02 ( | ||||||
| CoP – copper (current study) | 42·3 | 2·053/0·074 | 3·149 | 1·40 ( | 16·4% Qtz; 4·5% Alb; 3·9% Feld; 23·6% Bio; 15·4% Chlo; 12·0% Grun; 9·1% Gar; 7·9% Mag | No | |
| Copper upper beach ( | 12·5 | 86 N: 1·93/0·05/0·55 | 2·844 | 1·50 ( | 25·1% Qtz; 33·5% Feld; 8·4% Scp; 5·8% Amp; 5·8 Chlo; 5·3% Bio; 3·0% Mag | Yes | |
| 91 N: 1·90/0·05/0·55 | |||||||
| 95 N: 1·865/0·05/0·55 | |||||||
| Copper lower beach ( | 25·5 | 86 N: 1·895/0·05/0·55 | 2·943 | 1·40 ( | 25·1% Qtz; 33·5% Feld; 8·4% Scp; 5·8% Amp; 5·8 Chlo; 5·3% Bio; 3·0% Mag | Yes | |
| 91 N: 1·865/0·05/0·55 | |||||||
| 95 N: 1·830/0·05/0·55 | |||||||
| Copper S1 ( | 15 | 2·013/0·045 | 1·924/0·096/0·421 | 2·70 | 1·55 ( | No | |
| Copper S2 ( | 38 | 1·876/0·033 | 1·865/0·123/0·275 | 2·60 | 1·54 ( | No | |
| Copper S3 ( | 75 | 1·860/0·033 | 1·742/0·022/0·856 | 2·75 | 1·49 ( | No | |
| Copper TSF2 ( | 3 | — | 1·76/0·0769/0·54 | 2·682 | ( | 32% Qtz; 30% Alb; 23% Mu3T; 12% Micr; 2% Kaol; 1% clin | No |
| Deixing copper ( | 95 | 1·84 (Γ100)/0·126 | 1·92/0·070/0·42 | 3·75 | 1·43 ( | 78% Fay; 22% Mag | No |
| Brazilian gold ( | 65 | 1·89 (Γ100)/0·206 | 1·955/0·070/0·65 | 2·89–3·20 | 1·33 ( | 27% Qtz; 25% Alb; 35% Chlo | No |
| Brazilian gold ( | 95 | 1·89 (Γ100)/0·176 | 2·150/0·25/0·25 | 2·89 | 1·41 ( | 27% Qtz; 25% Alb; 35% Chlo | No |
| Panzhihua | 19 | 1·79 (Γ100)/0·252 | 1·795/0·090/0·39 | 3·37 | 1·41 ( | 30% Dio; 32% Lab; 11% Hrb; 9% Chlo | No |
| Panzhihua | 68 | 1·81 (Γ100)/0·152 | 1·875/0·080/0·39 | 3·14 | 1·36 ( | 46% Dio; 40% Lab; 6% Hrb; 5% Chlo | No |
| Panzhihua | 93 | 1·76 (Γ100)/0·185 | 3·11 | 1·40 ( | 28% Dio; 24% Lab; 22% Hrb; 16% Chlo | No | |
| Iron-flotation ( | 38·6 | 2·00/0·15/0·245 | 2·83 | 1·30 ( | 98·3% Qtz; 1·7% Haema | No | |
| Iron-slimes ( | 86·2 | 1·95/0·15/0·232 | 4·02 | 1·35 ( | 54·8% Qtz; 42·3% Haema; 2·9% Kaol | No | |
| Iron-S1 ( | 52·2 | 1·86/0·045/0·46 | 3·05 | 1·40 ( | 76·2% Qtz; 20·9% Ioxi | No | |
| Iron-S2 ( | 33·3 | 1·74/0·045/0·46 | 2·97 | 1·35 ( | 78·4% Qtz; 17·2% Ioxi | No |
FC, fine content; Γ100, intercept of CSL at p′= 100 kPa; Γ, intercept of linear CSL at p′= 1·0 kPa; ℓ, slope of linear CSL; a, intercept of curved CSL at p′ = 1·0 kPa; b, slope of curved CSL; c, exponent of curved CSL; Gs, specific gravity; ϕ′cs, critical state friction angle; TC, triaxial compression; DSS, direct simple shear; SS, simple shear; Minerals: Qtz, quartz (tectosilicate); Feld, feldspar (tectosilicate); Alb, albite (feldspar group – tectosilicate); Lab, Labradorite (feldspar group – tectosilicate); Micr., microcline (feldspar group – tectosilicate); Scp, scapolite (tectosilicate); Mu3T, muscovite-3T (mica group – phyllosilicate); Chl, chlorite (chlorite group – phyllosilicate); Clin, clinochlore (chlorite group – phyllosilicate); Bio, biotite (mica group – phyllosilicate); Kaol, kaolinite (clay group – phyllosilicate); Acti, actinolite (amphibole group – inosilicate double chain); Grun, grunerite (amphibole group – inosilicate double chain); Amp, amphibole (inosilicate double chain); Hrb, hornblende (amphibole group – inosilicate double chain); Dio, diopside (pyroxene group – inosilicate single chain); Gar, garnet (nesosilicate); Fay, fayalite (Olivine group – nesosilicate); Mag, magnetite (iron oxide); Haem, haematite (iron oxide); Ioxi, Iron oxide; Cal, calcite (calcium carbonate); Dol, dolomite (calcium–magnesium carbonate)
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