2015
DOI: 10.1016/j.jes.2015.05.012
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Flow and geochemical modeling of drainage from Tomitaka mine, Miyazaki, Japan

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Cited by 13 publications
(6 citation statements)
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“…After measuring OCP under N 2 atmosphere, a fixed potential of 0.7 V vs. SHE was applied to the working electrode for 1 h with magnetic stirring at 250 rpm. This applied potential was chosen based on typical redox conditions where AMD has been formed (i.e., about 0.64-0.68 V) (Yamaguchi et al, 2015).…”
Section: Chronoamperometry Measurementsmentioning
confidence: 99%
“…After measuring OCP under N 2 atmosphere, a fixed potential of 0.7 V vs. SHE was applied to the working electrode for 1 h with magnetic stirring at 250 rpm. This applied potential was chosen based on typical redox conditions where AMD has been formed (i.e., about 0.64-0.68 V) (Yamaguchi et al, 2015).…”
Section: Chronoamperometry Measurementsmentioning
confidence: 99%
“…Groundwater flows through aquifers consisting of surface soil and weathered layers at this mine site. Groundwater in the aquifers flows to mining areas through faults and veins as shown in Figure 2 [42]. Groundwater in the mined area flows through the mining levels (−2 L, −3 L, and −5 L) to the adit mouth of the drainage level (−5 L).…”
Section: Conceptual Model Of Groundwater Flowmentioning
confidence: 99%
“…Rainwater flowing into the mines is then collected in a sump, and reused for spraying onto haul roads, conveyors and loading and unloading [23]. Excess water discharge is flowed to the surface using a drainage system.…”
Section: Parameters Of Mine Drainage Systemmentioning
confidence: 99%