| Records |
| Author |
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| Title |
Selecting Mine Drainage Treatment Systems |
Type |
Journal Article |
| Year |
1995 |
Publication |
E&Mj-Engineering and Mining Journal |
Abbreviated Journal |
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| Volume |
196 |
Issue  |
10 |
Pages |
Rr24-& |
| Keywords |
mine water treatment |
| Abstract |
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| Notes |
Selecting Mine Drainage Treatment Systems; Wos:A1995ta62400001; Times Cited: 0; ISI Web of Science |
Approved |
no |
| Call Number |
CBU @ c.wolke @ 8900 |
Serial |
87 |
| Permanent link to this record |
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| Author |
Lovell, H.L. |
| Title |
Limestone Treatment Of Coal Mine Drainage |
Type |
Journal Article |
| Year |
1971 |
Publication |
Min. Congr. J. |
Abbreviated Journal |
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| Volume |
57 |
Issue |
10 |
Pages |
28-& |
| Keywords |
mine water treatment |
| Abstract |
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Series Issue |
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Edition |
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| ISSN |
0026-5160 |
ISBN |
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| Notes |
Limestone Treatment Of Coal Mine Drainage; Wos:A1971k631900002; Times Cited: 1; J Allen Overton Jr, 1920 N St Nw, Washington, DC 20036; ISI Web of Science |
Approved |
no |
| Call Number |
CBU @ c.wolke @ 9263 |
Serial |
101 |
| Permanent link to this record |
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| Author |
Sasaki, K. |
| Title |
Immobilization of Mn(II) ions by a Mn-oxidizing fungus – Paraconiothyrium sp.-like strain at neutral pHs |
Type |
Journal Article |
| Year |
2006 |
Publication |
Mater. Trans. |
Abbreviated Journal |
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| Volume |
47 |
Issue |
10 |
Pages |
2457-2461 |
| Keywords |
mine water treatment |
| Abstract |
A Mn-oxidizing fungus was isolated from a constructed wetland of Hokkaido (Japan), which is receiving the Mn-impacted drainage, and genetically and morphologically identified as Paraconiothyrium sp.-like strain. The optimum pHs were 6.45-6.64, where is more acidic than those of previously reported Mn-oxidizing fungi. Too much nutrient inhibited fungal Mn-oxidation, and too little nutrient also delayed Mn oxidation even at optimum pH. In order to achieve the oxidation of high concentrations of Mn like mine drainage containing several hundreds g-m(-3) of Mn, it is important to find the best mix ratio among the initial Mn concentrations, inocolumn size and nutrient concentration. The strain has still Mn-tolerance with more than 380 g-m(-3) of Mn, but high Mn(II) oxidation was limited by pH control and supplied nutrient amounts. The biogenic Mn deposit was poorly crystallized birnessite. The strain is an unique Mn-oxidizing fungus having a high Mn tolerance and weakly acidic tolerance, since there has been no record about the property of the strain. There is a potentiality to apply the strain to the environmental bioremediation. |
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Immobilization of Mn(II) ions by a Mn-oxidizing fungus – Paraconiothyrium sp.-like strain at neutral pHs; Wos:000242429300002; Times Cited: 0; ISI Web of Science |
Approved |
no |
| Call Number |
CBU @ c.wolke @ 16940 |
Serial |
103 |
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| Author |
Chen, M.; Li, L.; Grace, J.; Tazaki, K.; Shiraki, K.; Asada, R.; Watanabe, H. |
| Title |
Remediation of acid rock drainage by regenerable natural clinoptilolite |
Type |
Journal Article |
| Year |
2007 |
Publication |
Water, Air, Soil Pollut. |
Abbreviated Journal |
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| Volume |
180 |
Issue |
1-4 |
Pages |
11-27 |
| Keywords |
mine water treatment |
| Abstract |
Clinoptilolite is investigated as a possible regenerable sorbent for acid rock drainage based on its adsorption capacity for Zn, adsorption kinetics, effect of pH, and regeneration performance. Adsorption of Zn ions depends on the initial concentration and pH. Adsorption/Desorption of Zn reached 75% of capacity after 1-2 h. Desorption depended on pH, with an optimum range of 2.5 to 4.0. The rank of desorption effectiveness was EDTAEDTA > NaCl > NaNO3 > NaOAc > NaHCO3 > Na2CO3 > NaOH > CeCa(OH)(2). For cyclic absorption/desorption, adsorption remained satisfactory for six to nine regenerations with EDTA and NaCl, respectively. The crystallinity and morphology of clinoptilolite remained intact following 10 regeneration cycles. Clinoptilolite appears to be promising for ARD leachate treatment, with significant potential advantages relative to current treatment systems. |
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Edition |
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| ISSN |
0049-6979 |
ISBN |
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| Notes |
Mar; Remediation of acid rock drainage by regenerable natural clinoptilolite; Wos:000244030000003; Times Cited: 0; ISI Web of Science |
Approved |
no |
| Call Number |
CBU @ c.wolke @ 7319 |
Serial |
17 |
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| Author |
Al, T.A. |
| Title |
Storm-water hydrograph separation of run off from a mine-tailings impoundment formed by thickened tailings discharge at Kidd Creek, Timmins, Ontario |
Type |
Journal Article |
| Year |
1996 |
Publication |
Journal of Hydrology |
Abbreviated Journal |
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| Volume |
180 |
Issue |
1-4 |
Pages |
55-78 |
| Keywords |
mine water treatment |
| Abstract |
The Kidd Creek Cu-Zn sulphide mine is located near Timmins, Ontario. Mill tailings are thickened and deposited as a thickened slurry in a circular, conical-shaped pile with an area of approximately 1200 ha. Deposition of tailings as a thickened slurry results in a relatively uniform grain-size distribution and hydraulic conductivity, and a thick tension-saturated zone above the water table. The tailings are drained by numerous small, ephemeral stream channels, which have developed in a radial pattern. During storms, water from these streams collects in catchment ponds where it is held before treatment. The contribution of tailings pore water to the run off is of interest because of the potential for discharge of pore water containing high concentrations of Fe(II)-acidity, metals and SO4 to the stream. Hydraulic head measurements, measurements of water-table elevation and groundwater how modelling were conducted to determine the mechanisms responsible for tailings pore water entering the surface streams. Chemical hydrograph separation of storm run off in one of these streams, during three rainfall events, using Na and Cl as conservative tracers, indicates that the integrated tailings pore water fraction makes up between less than 1% and 20% of the total hydrograph. This range is less than the maximum fraction of tailings pore water of 22-65% reported for run off from a conventional tailings deposit. At this site, preferential flow through permeable fractures may be the dominant mechanism causing discharge of tailings pore water to storm run off. Estimates of the mass of Fe(II) that discharges to the surface run off from the pore water range up to 2800 mg s(-1) during a moderate intensity, long duration rainfall event. The greatest potential for discharge of significant masses of solutes derived from the pore water exists during long duration rainfall events, when the water table rises to the surface over large areas of the tailings impoundment. |
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| Notes |
Storm-water hydrograph separation of run off from a mine-tailings impoundment formed by thickened tailings discharge at Kidd Creek, Timmins, Ontario; Wos:A1996up76700004; Times Cited: 7; ISI Web of Science |
Approved |
no |
| Call Number |
CBU @ c.wolke @ 17162 |
Serial |
85 |
| Permanent link to this record |
