1994
DOI: 10.1016/0269-7491(94)90139-2
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Metal transport in a stream polluted by acid mine drainage—The Afon Goch, Anglesey, UK

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Cited by 81 publications
(34 citation statements)
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“…enhanced by the low pH conditions. These highly acidic waters from the tailing piles were observed to flow into the nearby streams, causing their contamination, where significant concentrations of Al, Cd, Cu, Fe, Mn, Pb, Zn and SO 4 were observed in the stream waters near the main tailing deposit, and similar to other AMD case studies (Boult et al, 1994;Brake et al, 2001;Sainz et al, 2003;Sracek et al, 2004). The main input was observed near sample AMW3, where a disruption in the wall of the dam allowed the output of acidic water (pH~1) with high concentrations of trace elements (Table 3).…”
Section: Discussionsupporting
confidence: 80%
“…enhanced by the low pH conditions. These highly acidic waters from the tailing piles were observed to flow into the nearby streams, causing their contamination, where significant concentrations of Al, Cd, Cu, Fe, Mn, Pb, Zn and SO 4 were observed in the stream waters near the main tailing deposit, and similar to other AMD case studies (Boult et al, 1994;Brake et al, 2001;Sainz et al, 2003;Sracek et al, 2004). The main input was observed near sample AMW3, where a disruption in the wall of the dam allowed the output of acidic water (pH~1) with high concentrations of trace elements (Table 3).…”
Section: Discussionsupporting
confidence: 80%
“…Thus, where the solubility of iron oxides has been exceeded a massive precipitation of ochre can occur. Additional possibilities for variation in plaques formation are tributary entry, antecedent rainfall and discharge variation (BOULT et al, 1994). Low discharge allows all precipitated particulates to drop out of suspension, whereas increased discharge results in transport in suspension and favours erosive processes such as resuspension and release of pore-waters from a previously deposited layer of iron oxyhydroxide (CHAPMAN et al, 1983).…”
Section: Discussionmentioning
confidence: 99%
“…As a result, many 286 of the headwater streams of the region have low acid-buffering capability, 287 resulting in extremely acidic discharges containing high levels of dissolved 288 toxic metals (Abdullah and Royle, 1972;Fuge et al, 1991;Boult et al, 1994;289 Neal et al, 2005). In contrast, in those parts of the English Peak District 290 where carbonate lithology predominates (Carboniferous Limestone), neutral to 291 basic mine discharges are common and these have significantly lower 292 concentrations of dissolved toxic metals (Smith et al, 2003).…”
Section: Mine Water Chemistry 262mentioning
confidence: 99%