AMD is the product of water coming into contact with sulfide minerals and being exposed to the atmosphere; it occurs at almost all mines that have sulfide deposits. The same process occurs as a natural process on natural outcrops, this is known as acid rock drainage (ARD). AMD usually occurs in greater quantities than ARD because mining increases the surface area of sulfide minerals exposed to the environment.

AMD has many effects on the environment. Firstly, it lowers the pH: at Parys mountain water samples taken from the streams leading into Afon Goch were found to have a pH of 2.8 or lower; this was maintained along a 1 km stretch of the stream [2] . This lower pH makes the environment uninhabitable for many flora and fauna but those that can survive the lower pH are threatened by toxic metals, which are more bio-available in low pH environments [3] .

The generation of AMD involves multiple reactions and follows different chemical routes depending on the pH of the environment. The first step (Equation (1)) is the oxidation of pyrite to aqueous iron and sulphuric acid [4] ; this reaction lowers the pH.

If the environment is sufficiently oxidising, the second step will occur, (Equation (2)) [4] .

At this stage, the reaction depends on the pH of the environment; if it is above 2.3 then (reaction 3) [4] will dominate, but if the pH is lower then (reaction 4) [4] will dominate.

Based on (Equations (1)-(3)), where the final product is Fe(OH)₃, it is possible to show the whole process as (Equation (5)) [5] . This umbrella equation is agreed by most of the scientific community to be an accurate representation of AMD, but it ignores the fact that in the more acidic conditions Fe³⁺ is the primary oxidant of pyrite as opposed to oxygen as shown in (Equation (4)). (Equation (6)) [5] better shows this and also has 8.5 moles of H⁺ per mole of pyrite, as opposed to 4 moles H⁺ per mole of pyrite.

At Parys Mountain Equation (2) will be closer to the truth on site; but downstream of Parys Mountain the acidity reduces, (reaction 3) will be able to occur and hence (Equation (5)) will be more accurate. In reality neither of these umbrella equations show the overall reaction as both ignore part of the process to create a balanced equation [6] ; the equations also ignore other minerals involved in the generation of AMD, such as chalcopyrite (CuFeS₂) and chalcocite (Cu₂S) [5] , as well as ignoring the increased rates that iron bacteria, such as Thiobacillus Ferro-oxidans and Leptospirillum Ferro-oxidans, can provide, which have both been isolated at Parys Mountain [2] .

Several primary factors have been identified to determine the rate of AMD formation [5] , which are: pH; temperature; [O₂] in the gas phase, in areas with poor airflow e.g. deep mines; [O₂] in the water phase; [Fe²⁺] within water; surface area of exposed metal sulfide e.g. [FeS₂]; bacterial activity. Controlling these factors is key to successful remediation, including remediation at Parys Mountain.

Despite Parys Mountains historical significance and visible impact on the environment, (Figure 1) there is a limited supply of peer-reviewed research available

on levels of AMD surrounding the site; the research that does exists was carried out before the controlled breaking of an underground dam in 2003 [1] , [7] , which altered the flow of AMD leaving the site.

Table 1 shows the mean range of metal concentrations and pH collected by Walton et al. [2] across a period of 3 years in the 1980’s and 90’s. His samples focused on the stream that flows from the centre of Parys Mountain through the central ponds to the southern stream over a distance of 900 m. The results showed a decrease in concentration with distance downstream but no other visible trends.

Walton’s study shows that iron, zinc, lead and arsenic all exceed their environmental quality standards of 0.73, 0.0005, 0.005 and 0.005 mg/L respectively, as set out by the Water Framework Directive [8] [9] [10] .

Parys Mountain has a complicated surface hydrology (Figure 1) with two catchments, one heading north and one heading south, these collect water from the north and south-east sides of Parys Mountain respectively. There are also many settling ponds that appear to have no outflows, presumably draining underground. There is a large network of underground mine shafts [7] , of which the details are not publicly available.

During the sampling exercise, the northern stream was fast-flowing, narrow and had no active methods of remediation in place; whereas the southern stream had a slow flow rate; large settling ponds and marshland in its path. The streams, therefore, provide an interesting contrast in remediation potential.

pH values recorded had a range of 2.3 - 6.2 (Figure 2). Unlike element concentrations

there is no correlation between distance downstream and an increase in pH, there is a difference when results are plotted with the environments. The settling ponds and southern streams had pH’s of 2 - 3 whereas the bogs had a pH range of 5 - 6; excluding the anomaly at site D in November with a pH of 3.2 (Figure 2).

Across all sites the most abundant element analysed was Iron, with a maximum concentration measured of 126.1 mg/L, (Figure 3) followed by in descending order Aluminum, Zinc, Copper, Manganese, and Lead, with respective maximum values of 34.03, 29.05, 14.61, 10.37, and 0.706 mg/L (Figures 4-8). All other elements characterised were below 0.01 mg/L and Arsenic, Mercury and Vanadium were not detected by the ICP at any concentration.

When all sample sites are plotted against distance from the Parys Mountain no trends are visible; but when the two catchment zones (Figure 1) are treated separately, distinct trends are shown. Both show a decrease in concentration of metal ions in both months, but the rates at which the metal ions decrease in concentration varies depending on the month and stream.

For all elements except Lead and Manganese concentrations were higher in the northern stream compared to the southern stream (Figures 3-6). However, these elements in January at site A had a higher concentration than the northern stream but by site B the concentration had decreased to within the range of the northern stream’s concentrations (Figures 3-6).

Manganese followed the same trend as most other elements in November however in January both the northern and southern streams had similar values of approximately 1 mg/L (Figure 7). In both months Lead had a substantially

higher concentration in the southern stream when compared to the northern stream (Figure 8).

When comparing the streams separately across the two months, the northern stream had higher concentrations in November for all elements; and the southern stream had higher concentrations in January for Iron and Copper (Figure 3 and Figure 4) but not Zinc Aluminium Manganese or Lead (Figures 5-8).

January’s results (Figure 9) had percentage reduction in concentration (PRC) that are similar for each element excluding Manganese but varied across sites. The southern stream shows higher PRC for all stages except the 2nd settling pond (B to C) when compared to the northern stream.

November’s results (Figure 10) were a lot less consistent; Iron and Manganese specifically did not have similar levels to the other metals and in some cases increased in concentration after passing between sites.

Sites A to B and B to C (the settling ponds) showed higher PRC compared to the northern stream some of the time; but only sites C to D and D to E which covered the bog area had constantly high PRC over both months compared to other sites.

Out of all the elements analysed Iron had the highest Concentration; this is almost certainly due to the fact that FeS₂ is the predominant sulphide mineral at Parys Mountain [12] ; also, iron has a higher affinity for the sulphate ions in solution.

The order of element concentration correlates with the work of Walton et al. [2] who found that the element he analysed had the decreasing order of Iron, Aluminium, Zinc, Copper and Lead. Walton et al. did find Arsenic to have a maximum concentration of 1.6 mg/L where this study found no trace of Arsenic, this matches up as all elements Walton analysed were substantially higher than the values this study found e.g. 550 mg/L for Iron by Walton et al. compared to a maximum value of 126 mg/L found by this study.

Walton et al. study looked at the southern stream alone; the highest result from this study for the southern stream showed a maximum value of 106 and 34 mg/L for Iron and Aluminium respectively compared to 550 and 90 mg/L from Walton et al.; this was to be expected as the de-watering project in 2003 [7] changed the northern stream to the primary outlet for Parys Mountains AMD [1] .

The two sampling trips were carried out in very different weather conditions; in November the weather was wet but mild, the Met Office recorded 59.4 mm [13] of rainfall in the month preceding sampling; this is in sharp contrast to January; when the Met Office recorded 146.4 mm [13] of rainfall. This made a substantial difference to the visible level of the streams with parts being up to approximately 15 - 20 cm higher.

This difference in rainfall is the most likely the factor in the difference seen across the 2 sampling trips. In the northern catchment zone, there is more bedrock containing Sulphide minerals [14] in addition to this the majority of the underground workings drain into the northern catchment zone [1] . Both of these sources gain there O₂ and H₂O from groundwater. As groundwater levels are not affected by seasonal rain there will be a constant level of AMD being generated, but the high rainfall in January would dilute the AMD in the stream hence the lower concentrations observed in January.

In the southern catchment zone, there are a large number of spoil heaps these spoil heaps could potentially contribute to the increase in element concentration in the southern stream in two ways. Spoil heaps have large surface areas but the majority will not be in contact with H₂O (a requirement for AMD generation) during drier weather hence they generate more AMD when there is more rain. The second factor is pore water inside spoil heaps; there will be pore water that will allow AMD to be created but it is stagnant in dry weather. When large rainfall occurs it flushes out pore water and hence an increase in element concentrations is observed in the southern stream.

Unlike element concentrations pH did not decrease with distance downstream (Figure 2 this could be due to (Equation (3)) the reaction of ferric iron with water producing iron oxide and hydrogen ions, which occurs at pH’s above 2.3, this reaction produces hydrogen ions which in turn lower the pH acting as a pH buffer preventing the pH from rising.

Sites D and E were the only sites to have pH’s higher than 3, as these sites were both bogs this is the most likely cause of the increased pH.

To identify if the streams were successfully remediating the AMD leaving Parys Mountain, the percentage reduction in concentration (PRC) was calculated for each element (calculations are shown in methodology).

PRC was similar for each element at sample sites in January (Figure 9) but in November (Figure 10) this was not the case; this could be due to the complex interplay of redox reactions favouring the removal of certain elements over others, for example (Equation (8)) reacts iron hydroxide with copper ions in acid to produce solid copper and ferric iron ions and water, removing copper from the water column but adding iron back in. but if this was the case then the inconsistent PRCs should be visible in January. A more likely explanation is that Novembers results were anomalous but as samples were not collected in triplicate this cannot be verified.

As well as reduction levels being varied in November, iron increased in concentration between sites A to B and D to E, and manganese increased across sites A to B. in addition to this iron had very low PRC, these results could be due to the effects of redox reactions like (Equation (8)); but there is also the possibility that the areas around these sites contain large amounts of iron and manganese sulphates that are submerged in groundwater and drain in to the stream between sample sites. This would explain why these results were not seen in January and why they do not occur at all sites.

In January all sites except B to C had higher PRCs; one theory for this is that the increased rainfall meant water sources (small streams and surface runoff) from surrounding farmland that did not contain AMD were not active in November but were active in January due to the increased rainfall; which diluted the elements between sample sites. B to C could have decreased in PRC again because of water sources not active in November but these water sources came from Parys Mountain adding AMD to the stream masking the true PRC across sites B to C

There are several reasons that could explain why the removal efficiency is higher in the southern steam. The first is that between sites A-B and B-C there are large settling ponds in which the water moves slowly; allowing a longer time for the (reaction 3) to occur converting Ferric iron into iron hydroxide, which would leave the water column through sedimentation. In a fast-flowing stream, AMD would be able to travel further before oxidising and settling out. Then between sites C-D and D-E are the wetlands with the raised pH; this allows for (reaction 3) at a higher rate, in addition to this the large areas of mud act as filters with AMD binding to the soil as the water percolates through.