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Cu, Pb and Fe release from sulfide-containing tailings in seawater: Results from laboratory simulation of submarine tailings disposal

机译:海水中含硫化物的尾矿中铜,铅和铁的释放:海底尾矿处置的实验室模拟结果

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Metal release from the deposition of sulfide-containing tailings in seawater was investigated using a batch reaction experiment inside a temperature and dissolved oxygen-controlled chamber. Two hundred grams of tailings from a porphyry Cu-Au and a sediment-hosted Cu deposit were submerged in 1.8 L synthetic seawater. The sulfides present in the porphyry Cu-Au tailings are pyrite (FeS2), chalcopyrite (CuFeS2) and bornite (Cu5FeS4) while in the sediment-hosted Cu tailings are bornite, chalcocite (Cu2S) and covellite (CuS). Galena occurs as a minor sulfide in both tailings. Pore water and overlying seawater samples were collected and analyzed for pH, redox potential and trace metals (Cu, Pb and Fe) concentration. Results show that there is very low Cu (10–40 μg/L), Pb (1–10 μg/L) and Fe (5–50 μg/L) released into solution throughout the course of 87 days. Long-term trace metal release from tailings in seawater is therefore theorized to be low and is a slow process.
机译:在温度和溶解氧控制室内进行分批反应实验,研究了海水中含硫化物尾矿沉积物中的金属释放。将斑岩型铜金中的200克尾矿和沉积有铜的矿床浸入1.8 L合成海水中。斑岩型Cu-Au尾矿中存在的硫化物为黄铁矿(FeS2),黄铜矿(CuFeS2)和褐铁矿(Cu5FeS4),而在沉积物承载的Cu尾矿中的斑岩矿,方铅矿(Cu2S)和Covellite(CuS)。方铅矿在两个尾矿中均以次要硫化物形式存在。收集孔隙水和上方的海水样品,并分析其pH,氧化还原电势和痕量金属(铜,铅和铁)的浓度。结果表明,在整个87天的时间内,释放到溶液中的Cu(10-40μg/ L),Pb(1-10μg/ L)和Fe(5-50μg/ L)都非常低。因此从理论上讲,海水中尾矿中的长期微量金属释放量很低,并且是一个缓慢的过程。

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