(a) Plain view of the tailings dam, and (b) crosssectional view of line B-B'.

(a) Plain view of the tailings dam, and (b) crosssectional view of line B-B'.

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Acid mine drainage (AMD), the very acidic and highly contaminated leachate generated in closed/abandoned mines, is commonly managed by neutralization to raise the pH and precipitate most of the heavy metals. Although effective, this approach does not generate any product of economic value, so it is very costly and unsustainable in the long-term. Un...

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... Acid mine drainage in this site has a pH between 3 and 4, flows at a rate of around 0.04 m 3 /min, and contains substantial amounts of dissolved iron (Fe) (~70 mg/l), Cu (~1 mg/l), Zn (~9 mg/l), and Pb (~0.06 mg/l). It is mostly generated from the tailings dams and underground mine workings and has been treated by neutralization since the 1970s. Fig. 1 shows the plain and cross-sectional views of the tailings dam including the location of borehole core samples. The tailings dam is divided into three sections and is located between a stream and a ...
Context 2
... used to simulate AMD formation and flow paths in the tailings dam including the migration of heavy metals. In addition, possible countermeasures like barriers with low permeability and recharge reduction were evaluated using the model. Fig. 2 shows the twodimensional model of the tailings dam formulated based on the cross-sectional line B-B' in Fig. 1 and the measured hydraulic conductivity (K) and Zn distribution coefficient (Kd) of each distinct lithological feature. In all simulations, MODFLOW 2005 and MT3DMS were used to model AMD/groundwater flow and solute migration, ...
Context 3
... Acid mine drainage in this site has a pH between 3 and 4, flows at a rate of around 0.04 m 3 /min, and contains substantial amounts of dissolved iron (Fe) (~70 mg/l), Cu (~1 mg/l), Zn (~9 mg/l), and Pb (~0.06 mg/l). It is mostly generated from the tailings dams and underground mine workings and has been treated by neutralization since the 1970s. Fig. 1 shows the plain and cross-sectional views of the tailings dam including the location of borehole core samples. The tailings dam is divided into three sections and is located between a stream and a ...
Context 4
... used to simulate AMD formation and flow paths in the tailings dam including the migration of heavy metals. In addition, possible countermeasures like barriers with low permeability and recharge reduction were evaluated using the model. Fig. 2 shows the two- dimensional model of the tailings dam formulated based on the cross-sectional line B-B' in Fig. 1 and the measured hydraulic conductivity (K) and Zn distribution coefficient (Kd) of each distinct lithological feature. In all simulations, MODFLOW 2005 and MT3DMS were used to model AMD/groundwater flow and solute migration, ...

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... AMD can also be generated from old, decommissioned metal and coal mines whose operations have ceased even hundreds of years ago (Johnston et al., 2009;Buzatu et al., 2016). AMD involves the oxidation of metal sulfides, such as pyrite, marcasite, and pyrotite (Khalil et al., 2013;Phillips, 2016;Tabelin et al., 2019). When these minerals are exposed to water and atmospheric oxygen, chemical reactions occur that result in the oxidation of sulfides (Blowes et al., 2003;Jodeiri et al., 2020). ...
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... The software has been employed to simulate acid mine drainage in tailings dams, and the simulation results have revealed the migration pathway of heavy metals. The model further predicts that the volume of acidic mine drainage, and the concentration of Zn can be reduced through the installation of a low-permeability barrier downstream of the tailings dam or the utilization of ground-sealing techniques to minimize backfilling [101]. Furthermore, scholars [102] have employed both the MOD-FLOW and MT3DMS models as simulation models, utilizing genetic algorithms as the optimization algorithm, and encoding the optimization process of the genetic algorithm in MATLAB software, thereby achieving the potential of combining models with algorithms. ...
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... In their research on the migration of heavy metals, scholars have paid more attention to how heavy metal elements migrate in the soil and how they accumulate in rivers and other sediments. Tabelin et al. (2019) used a coal mine as the research object and analyzed the whole process of heavy metal elements from their release to entering the soil and finally leaching into the groundwater and also established a heavy metal migration model. Jiang and Liang (2007) studied the heavy metal migration model in the saturated-unsaturated state and simulated the process of groundwater pollution of coal gangue leachates by using numerical calculations and laid a foundation for the study of pollutant migration patterns. ...
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... Active treatment strategies are very effective but become costly and unsustainable in the long-term [26]. This is because AMD formation could persist for hundreds to thousands of years [27,28]. As an alternative, researchers have developed technologies that allow natural chemical and biological treatments for passively treating AMDs [29]. ...
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... The geogenic sources of SO 4 −2 contain gypsum (CaSO 4 . 2H 2 O), and pyrite (FeS 2 minerals (Nyirenda et al., 2015;Tabelin et al., 2019). However, the anthropogenic sources of SO 4 −2 include metallurgical refineries, coal mining, phosphate refineries, and power plants. ...
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... activities (Spitz and Trudinger 2019). The remaining heavy metals (HMs) are biologically toxic substances that are not biodegradable, and long-term exposure to HMs threaten the natural environment and human health (Tabelin et al. 2019;Bari et al. 2020). With the extensive development of iron ore resources, a great number of large-scale iron tailings ponds have been produced. ...
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... In Japan, for example, chemical neutralization of AMDs from legacy mines has been subsidized by the government to the tune of ~70 B JPY (~US$ 770 M) for the last 40 years (Tomiyama et al., 2019). Although effective, this process generates voluminous sludge that is also a source of secondary pollution and may have to be continued for hundreds to thousands of years (Davis Jr, et al., 2000;Tabelin et al., 2019a;Tabelin et al., 2019b). To address these sustainability issues, several authors proposed the harvesting of other valuable elements, minerals and energy from AMDs to reduce treatment costs (Table 10). ...
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... Also, in Japan MTs containing pyrite (FeS2) and substantial quantities of Cu and Zn were reported in a study by Tabelin et al. (2019). For O'Kiep, MSW severely contaminated nearby soils and acidified the soils, thus increasing the mobility of PTEs (Moncho et al., 2017), to areas in the vicinity of the houses (Figure 2-1). ...
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South Africa is faced with challenges related to potable water quality, which has periodically deteriorated, coupled with inconsistent supply of tap water to households. On the other hand, South Africa is an important mining region, and nearly every province has remnants of active and closed metalliferous mining sites. Metalliferous mines produce a large quantity of metalliferous solid waste (MSW), which should be effectively managed to minimise the negative effects as it has the potential to produce acid rock drainage (ARD). The mobility of drainage alters the scarce water resources and aquatic species. These challenges are a primary concern to the community in the arid O’Kiep region, which is located in the Namaqualand district, South Africa, whereby the community has few alternatives to groundwater as a source of drinking water. The aim of this study was to assess species dispersion from a closed Namaqualand metalliferous mine into water sources in O’Kiep, Northern Cape province, South Africa. This study aimed to determine the issues related to the deterioration of the surface water quality from the source to the point-of-use (POU) and contributing to the inadequate drinking water supply and shortages in O’Kiep. Quantitative and qualitative assessments of water quality parameters were taken; and the adverse human health outcomes experienced by the residents were surveyed. Furthermore, disease patterns were estimated based on administered questionnaires. Approximately 88% of community members indicated that the water supplied is often turbid, while a high number of people with teeth discolouration (72%) are living in the area and experience diarrhoea-like symptoms, which are likely associated with the ingestion of toxin-contaminated water. This was confirmed by some physicochemical parameters quantified from the drinking water supply system (DWSS), such as sulfate, that were not within the range prescribed for drinking water quality guidelines (SANS241-1, 2015; WHO, 2011). The statistical models did not suggest physicochemical properties as predictors of any of the health symptoms. However, regular monitoring and evaluation of the DWSS are essential for this vulnerable community. From this, it was recommended that a feasible way for water security in O’Kiep might be groundwater resources, as an alternative source to irregular surface water. The hydrogeochemical parameters of groundwater assessed indicated that the continuous consumption of the groundwater without pre-treatment might result in possible human health risks as the groundwater quality index (GWQI) confirmed that the groundwater quality could be classified as being of moderate concern. Furthermore, the hydrogeochemical indices and cationic exchange values indicated that the aquifer is of inland origin, whereas the piper trilinear diagram revealed that the groundwater type in the area is categorised as saline, which was confirmed by sodium adsorption ratio (SAR). Similarly, the seasonal variation of the hydrogeochemical characteristic changes of an open-pit groundwater (OPGW) near a closed metalliferous mine (CMM) were investigated against standards for drinking and irrigation usage. Based on the results, it was evident that the OPGW quality varied seasonally. The PHREEQC model indicated that cation exchanges played a significant role in the groundwater hydrogeochemical characteristic. Furthermore, the seasonal fluctuation in the groundwater quality was attributed to the water-table-level fluctuations, resulting in some instances in a lack of compliance to the drinking water quality guidelines (SANS241-1, 2015; WHO, 2011). Overall, the groundwater was slightly acidic with permissible levels for irrigation purposes. Therefore, excessive usage of the OPGW may have undesirable effects on plant growth. The groundwater hydrogeochemical characteristics of OPGW contamination suggested acid rock drainage formation potential (ARDP). The contamination of the groundwater by potentially toxic elements (PTEs) from soils and MSW in the study area was a matter of concern requiring further investigation. Samples of the metalliferous soils and MSW were then evaluated for their ARDP using an integrated approach, combining geochemical characterisation, static tests and humidity cell tests (HCTs) assessing the balance between acidity potential (AP) and neutralisation potential (NP) of the slurry. Metalliferous soil leachates (MSL), stockpiled metalliferous waste leachates (SMWL) and metalliferous tailing leachates (MTL) were measured and quantified weekly for hydrogeochemical parameters. The static tests suggested that the metalliferous soils had a high acid-producing potential. This was confirmed by the results of the HCTs, which revealed signs of ARDP. Furthermore, the results also demonstrated weathering and production of ARD. The HCT results showed that the soils around the old mining town of O’Kiep are susceptible to ARDP and can release acid for elongated periods. Similarly, this study assessed ARDP from the stockpiled metalliferous waste (SMW) and metalliferous tailings (MTs) in O’Kiep. The static test results for the SMW were inconclusive, whereas the HCTs allowed the classification of the SMW as acid-producing material. In addition, the MTs were classified as acid-producing by the static tests and HCTs, with low mobility of PTEs when compared to SMW. Leaching of the SMW and MTs increases the risk of PTEs and acid contamination of surrounding soil and groundwater bodies in O’Kiep. Additionally, there are increasing concerns over significant potential environmental health effects of the SMW and MTs, including the mobility of PTEs.
... of years (Davis Jr. et al., 2000;Tabelin et al., 2019a), and (2) disposal of huge amounts of bulky and hazardous sludge produced by the treatment (Gazea et al., 1996;Kefeni et al., 2015;Park et al., 2020b;Taylor et al., 2005). ...
Article
Acid mine drainage (AMD) formation is mainly caused by the oxidation of pyrite. Carrier-microencapsulation (CME) using metal-catecholate complexes has been proposed to passivate sulfide minerals by forming surface-protective coatings on their surfaces. Among the various metal-catecholate complexes, Ti-catecholate formed stable coatings having superior acid-resistance, but a thick enough passivating film required considerable time (ca. 14 days) to grow. Meanwhile, Fe-catecholates can form Fe-oxyhydroxide coatings within 2 days, however, they are less stable than Ti-based coating. To address these drawbacks of using a single metal-complex, this study investigated the concurrent use of Fe-catechol and Ti-catechol complexes for accelerating the formation of stable passivating coating on pyrite. Compared with a single metal-complex system, the coating formation was significantly accelerated in mixed system. Linear sweep voltammetry showed the simultaneous decomposition of [Fe(cat)]⁺ and [Ti(cat)3]2– as the main reason for improved coating formation. Electrochemical properties of coatings formed by single and mixed complex systems, confirmed by electrochemical impedance spectroscopy and cyclic voltammetry, indicated the coating formed in the mixed system had higher resistance and more electrochemically inert than the other cases. The simultaneous use of Fe-catechol and Ti-catechol complexes enhanced pyrite passivation by accelerating metal-complex decomposition and forming more stable coating composed of Fe2TiO5.
... 2020) as well as the improved harvesting ferrites ). These methods have been proven to be effective; unfortunately, the generation of AMD is a lasting process (Orbecido et al. 2019). Therefore, these methods require continuous cost input and monitoring, making them expensive and unsustainable. ...
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Pyrite, as one of the most abundant sulfide minerals, can be easily oxidized to generate acid mine drainage (AMD). In the present study, a new composite passivator named PropS-SH/sepiolite (PSPT) using γ-mercaptopropyltrimethoxysilane (PropS-SH) as the main passivator and natural sepiolite particles as filler was fabricated and used to suppress the oxidation of pyrite. Electrochemical tests and chemical leaching experiments were carried out to evaluate the passivation performance of PSPT coatings with different amount of sepiolite particles on pyrite oxidation. The results showed that the addition of appropriate sepiolite could significantly improve the inhibition ability of PropS-SH against pyrite oxidation. However, excessive addition of sepiolite particles weakened the inhibition ability of the PSPT coatings owing to aggregations of sepiolite. Additionally, the coating mechanism of PSPT on pyrite was also proposed based on the characterization of FTIR, XPS, and ²⁹SiNMR measurements, which indicated that sepiolite particles could be embedded in PropS-SH network through oxygen bridges, thus improving the stability of the composite coatings.