Reprocessing feasibility of polymetallic waste rock for cleaner and sustainable mining

被引:31
作者
Amar, Hicham [1 ,2 ]
Benzaazoua, Mostafa [1 ,2 ]
Edahbi, Mohamed [1 ,3 ]
Villeneuve, Mathieu [1 ]
Joly, Marc-Andre [4 ]
Elghali, Abdellatif [1 ,5 ]
机构
[1] Univ Quebec Abitibi Temiscamingue, Res Inst Mines & Environm RIME, 445 Boul Univ, Rouyn Noranda, PQ J9X 5E4, Canada
[2] Mohammed VI Polytech Univ UM6P, Min Environm & Circular Econ, Ben Guerir 43150, Morocco
[3] Univ Saskatchewan, Dept Geol Sci, Saskatoon, SK S7N 5E2, Canada
[4] Mine Langlois, Route 1000,Km 42 CP 6000, Lebel Sur Quevillon, PQ J0Y 1X0, Canada
[5] Mohammed VI Polytech Univ UM6P, Geol & Sustainable Min Dept, Ben Guerir 43150, Morocco
基金
加拿大自然科学与工程研究理事会;
关键词
Waste rock; Desulphurisation; Kinetic tests; Contaminated mine drainage; Gravity separation; Flotation; Waste rock management; MINE TAILINGS; ENVIRONMENTAL DESULFURIZATION; ACID ROCK; REACTIVITY; MANAGEMENT; FLOTATION; TESTS; PREDICTION; PYRITE;
D O I
10.1016/j.gexplo.2020.106683
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Mining operation produces significant volumes of waste rocks (WR) characterised by high heterogeneity in their physical, mineralogical and hydrogeological properties. The purposes of this study were to assess the acid-generating potential, evaluate reprocessing feasibility of polymetallic WR using desulphurisation process (i.e., gravity separation and flotation) and study the geochemical behaviour of desulphurised materials. The fresh WR was collected in the waste dump from Langlois mine at Lebel-sur-Que ' villon (Quebec, Canada). The WR sample was divided into six fractions using wet screening: D < 0.053 mm, 0.053 < D < 0.3 mm, 0.3 < D < 0.85 mm, 0.85 < D < 2.4 mm and 2.4 < D < 5 mm. Chemical and mineralogical characterisations showed that fine fractions (D < 2.4 mm) were enriched in sulphide minerals (i.e., 4.6 wt% pyrite, 3.5 wt% sphalerite, etc.) and carbonates (i.e., 3.7 wt% calcite and 5.1 wt% ankerite) compared to coarse fractions (1.2 wt% pyrite, 1.1 wt% sphalerite, 3.2 wt% calcite, 5.2 wt% ankerite). The acid-generating potentials of different fractions were evaluated using acid-base accounting (ABA) and net acid generation (NAG) tests. Only one size fraction (F2) was acid generating and others were classified as uncertain. The degree of liberation of sulphides in the size fractions greater than 2.4 mm was negligible (<16%). Consequently, for this WR sample, 2.4 mm was defined as the diameter of physical locking of sulphide (DPLS). Based on DPLS, the WR were separated into two fractions; reactive (<2.4 mm), non-reactive (<2.4 mm) and then submitted to kinetic tests. Geochemical analyses of leachates of the coarse fraction (2.4 < D < 10 mm), the total sample (D < 5 mm) and -DPLS fractions (D < 2.4 mm) and the benign desulphurised materials (D < 2.4 mm) showed that pH values remained between 6.62 and 8.11 and the instantaneous concentrations of metals such as iron (Fe), copper (Cu) and lead (Pb) were below environmental limits (D019, Quebec, Canada), except for zinc (Zn) leached from the total sample which indicates a risk of contaminated neutral drainage. The pyrite oxidation rate within the coarse fraction was low (16.6 mu mol/ kg/day) compared to fine fraction (35.8 mu mol/kg/day). A combined gravity-flotation process gave better results to decontaminate the waste rock (D < 2.4 mm), with a benign desulphurised material reaching a low sulphur content (0.23 wt%) and high sulphur recovery (89 wt%). The final concentrates from the combined gravity-flotation process showed high base metals (Zn, Cu and Pb) recovery (more than 87 wt%).
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页数:15
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