The importance of controlling oxygen addition during the thiosulfate leaching of gold ores

2003 ◽  
Vol 72 (1-4) ◽  
pp. 323-330 ◽  
Author(s):  
M.I. Jeffrey ◽  
P.L. Breuer ◽  
C.K. Chu
1992 ◽  
Vol 29 (1-3) ◽  
pp. 191-203 ◽  
Author(s):  
J.W. Langhans ◽  
K.P.V. Lei ◽  
T.G. Carnahan

2002 ◽  
Vol 66 (1-3) ◽  
pp. 1-21 ◽  
Author(s):  
Ellen Molleman ◽  
David Dreisinger

Metals ◽  
2020 ◽  
Vol 10 (8) ◽  
pp. 1029
Author(s):  
Mooki Bae ◽  
Sookyung Kim ◽  
Jeongsoo Sohn ◽  
Donghyo Yang ◽  
Hyunju Lee

Ammonium thiosulfate is an alternative lixiviant for the hydrometallurgical treatment of sulfide gold ores. The present study is primarily focused on ammonium thiosulfate leaching of gold (Au) and silver (Ag) from the sulfide ore (Sunshin mine in Korea). The main chemical composition of the concentrate was Au (84 ppm), Ag (852 ppm), Fe (18.9%), Si (23.2%), and S (21.1%). The effects of various parameters on the process, such as leaching time (1–4 h), ammonium thiosulfate concentration (0.05–0.5 M), copper sulfate (CuSO4), concentration (0.05–0.25 M), solid to liquid ratio (0.2–0.5), and reaction temperature (40–60 °C) were systematically examined. Optimum Au leaching efficiency (>99%) was obtained under the following leaching conditions: 0.5 M ammonium thiosulfate with 0.05 M CuSO4 concentration, 0.2 S/L ratio at 60 °C for 2 h. The results indicate that the behavior of Ag was similar to that of Au. Almost complete dissolution of Ag occurred under following leaching conditions: 0.5 M ammonium thiosulfate with 0.05 M CuSO4 concentration at 60 °C for 4 h. This study would be useful in understanding the eco-friendly leaching systems of Au and Ag during the hydrometallurgical process of sulfide gold ore.


2021 ◽  
Author(s):  
Xin Sun ◽  
Claudia Frey ◽  
Emilio Garcia-Robledo ◽  
Amal Jayakumar ◽  
Bess B. Ward

AbstractNitrite is a pivotal component of the marine nitrogen cycle. The fate of nitrite determines the loss or retention of fixed nitrogen, an essential nutrient for all organisms. Loss occurs via anaerobic nitrite reduction to gases during denitrification and anammox, while retention occurs via nitrite oxidation to nitrate. Nitrite oxidation is usually represented in biogeochemical models by one kinetic parameter and one oxygen threshold, below which nitrite oxidation is set to zero. Here we find that the responses of nitrite oxidation to nitrite and oxygen concentrations vary along a redox gradient in a Pacific Ocean oxygen minimum zone, indicating niche differentiation of nitrite-oxidizing assemblages. Notably, we observe the full inhibition of nitrite oxidation by oxygen addition and nitrite oxidation coupled with nitrogen loss in the absence of oxygen consumption in samples collected from anoxic waters. Nitrite-oxidizing bacteria, including novel clades with high relative abundance in anoxic depths, were also detected in the same samples. Mechanisms corresponding to niche differentiation of nitrite-oxidizing bacteria across the redox gradient are considered. Implementing these mechanisms in biogeochemical models has a significant effect on the estimated fixed nitrogen budget.


2019 ◽  
Vol 1347 ◽  
pp. 012127
Author(s):  
Guodong Chen ◽  
Hongying Yang ◽  
Huiqun Niu ◽  
Linlin Tong ◽  
Shuiping Zhong ◽  
...  
Keyword(s):  

2014 ◽  
Vol 88 (s2) ◽  
pp. 252-253 ◽  
Author(s):  
E.V. BELOGUB ◽  
E.E. PALENOVA ◽  
A.V. CHUGAEV ◽  
O.Yu. PLOTINSKAYA
Keyword(s):  

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