Relevant bibliographies by topics / Mine spoil waste

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Academic literature on the topic 'Mine spoil waste'

Author: Grafiati
Published: 4 June 2021
Last updated: 11 February 2022

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Journal articles on the topic "Mine spoil waste"

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Nayak, Samrudhi, S. P. Mishra, and C. S. K. Mishra. "Nutrient and Exo-Enzyme Dynamics in Organically Amended Iron Mine Spoil." Journal of Solid Waste Technology and Management 46, no. 1 (February 1, 2020): 115–22. http://dx.doi.org/10.5276/jswtm/2020.115.

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The aim of this study is to restore the nutrient status of iron ore mine spoil through suitable organic interventions. This paper reports the effects of different organic manure and bio-fertilizer amendments with inoculation of the earthworm Eisenia fetida in iron mine spoil on certain chemical parameters, microbial load and soil exoenzyme activities. The mine spoil samples were collected at random from five years old spoil dump and amended with farmyard manure (FYM), poultry manure (PM) and vermimanure (VM) along with biofertilizer in different combinations. The pH, conductivity, % organic carbon, N, P, K, bacterial and fungal population with activities of soil exoenzymes amylase, cellulase and invertase were studied in organically amended mine spoil. Significant variations (p<0.05) in the chemical and biological parameters were observed between treatments and days of incubation. Higher values were obtained with PM followed by FYM and VM. Earthworm inoculation enhanced the values of all the chemical parameters except % organic carbon. Bacterial population and exoenzyme activities increased significantly (p<0.05) with earthworm. PM with biofertilizer was found to be the most suitable combination followed by FYM. Inoculation of Eisenia fetida could facilitate mineralization of organics resulting in higher nutrient availability, higher microbial load and exoenzyme activities required to facilitate spoil reclamation.
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Ghosh, Dipita, and Subodh Kumar Maiti. "Can biochar reclaim coal mine spoil?" Journal of Environmental Management 272 (October 2020): 111097. http://dx.doi.org/10.1016/j.jenvman.2020.111097.

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Denimal, Sophie, Florent Barbecot, Laurent Dever, Nicolas Tribovillard, and Francis Meilliez. "Tracage chimique et isotopique des eaux souterraines en relation avec les eaux de lixiviation de terrils, bassin minier du Nord-Pas-de-Calais (France)." Bulletin de la Société Géologique de France 172, no. 1 (January 1, 2001): 111–20. http://dx.doi.org/10.2113/172.1.111.

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Abstract Introduction. - In the Nord-Pas-de-Calais region (northern France), the mining activity linked to the coal extraction resulted in the existence of many mine spoils. Most of the time, the choice of the mine spoil location has been made without knowing the potential contamination of the aquifers contained in the underlying formations by substances which can be solubilized and released in relation with the weathering of these mine spoils. The aim of this study is to determine the possible role of the mine spoils in the sulfate mineralization of the chalk aquifer. Previous works [Bernard, 1979; Droz, 1985] allow to consider several possible sources of sulfate in the coal basin: the dissolution of evaporitic minerals present in the Carboniferous limestones Formation which can locally contaminate per ascensum the chalk aquifer; the dissolution of gypsum contained in the Tertiary formations (Argiles de Louvil, Sables d'Ostricourt); sulfates of anthropic origin linked to the waste water discharge and/or to the agricultural practices; finally, the weathering of mine spoils which leads to the oxydation of the pyrite contained in the Carboniferous shales, and can release sulfate ions that may be transferred to the aquifer. Two sites have been selected 30 km to the south of Lille: site 1 lies directly on the Senonian-Turonian chalk while site 2 lies on the sandy-clayey Tertiary formations overlying the chalk formations (fig. 1-3). Geology and hydrogeology. - The waters have been sampled within the chalk aquifer (fig. 2). This water table forms the main resource in drinking water, currently exploited. The chalk aquifer is a free water table except where the Tertiary formations make this water table confined, as is the case for site 2. The recharge of the chalk aquifer is made by the percolation of the impluvium through the microporosity of the chalk with an infiltration velocity of 0.5 to 0.7 m per year [Vachier et al., 1979]. The chalk aquifer flow is schematically SW-NE to the Orchies basin (fig. 1). This flow is caused by the piezometric depression in the Orchies basin linked to industrial pumpage. Since the decrease of these pumpages, we can observe a rise of the chalk aquifer piezometric level evaluated to 10 m in the studied area. Material and methods. - Rock samples have been collected on the surface of the two sites and below it at site 1. Mineralogical analyses have been carried out on the bulk fraction as on the clayey fraction, the elementary analysis of total carbon and total sulphur has also been performed. Two water sampling surveys have been carried out on 19 sites. Sampling has been made from piezometers which reach the chalk aquifer and that are placed close to the mine spoils but also in a radius of 5 to 10 km around. Chemical and isotopic analyses have been made on the waters sampled at hydraulic upstream and dowstream of the mine spoils. In situ measurements have been carried out during the sampling. Piezometric levels have been taken at all the sampling sites. Results and discussion. - The carbon and sulphur contents have shown a superficial leaching of these elements on the mine spoils (fig. 9). The use of isotopic geochemistry and in particular the sulphur isotopes as tracers of the sulfate origin has permitted to identify two contribution sources at the two sites: a "mine spoil" source with a delta 34 S weakly negative (delta 34 S = -2,8 per mil, -3,9 per mil) which corresponds to the oxidation of sulfides contained by the Carboniferous shales and another source (delta 34 S = -20 per mil) corresponding to the gypsum of the "Sables d'Ostricourt" which is present only at site 2 (fig. 7, 10 & 11). This study has revealed the different behaviour of the two sites: for site 1, with a free water-table zone, the mine spoil leaching carries sulfate ions directly to the table whereas in the second site, with a confined aquifer zone, a part of the sulfate ions are reduced once exported to the table (the redox potential presents negative values; fig. 6). This bacterial reduction is made possible by the organic carbon leaching concomitant to the sulphur leaching on the mine spoils. This carbon contribution has been confirmed by the 14 C activity analysis: 14 C activity is characteristic of the chalk aquifer waters at the upstream of the mine spoil and noticeably lower downstream, this decrease can be linked to the "dead carbon" supply from the mine spoils (fig. 8). This organic carbon is involved in bacterially-mediated sulfate reduction (2CH 2 O + SO 4 (super 2-) --&gt; 2HSO 3 (super -) + H (super +) + HS (super -) ). Conclusion. - Both studied mine spoils release sulfate ions to the Chalk aquifer, in response to the weathering and leaching of their surficial part. Using an isotope study-grounded approach, the influence of the mine spoils upon the sulfate enrichment of the water table can be distinguished from that of Cenozoic formations sometimes present between the chalk aquifer and the mine spoil basis. No other sulfate source seems to be involved in the studied area. Together with sulfate ions, the mine spoils export dissolved organic carbon. Both chemical species sustain bacterial activity (sulfate reducers) that develops where the water table is made confined by overlying, almost impervious, Cenozoic deposits. In that case, reducing conditions in the aquifer decrease the amount of sulfate ions present. Thus the simultaneous supply of sulfate and carbon by the mine spoils leads to a self-purification process where the aquifer is confined.
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Nagaraj, H. B., and C. Shreyasvi. "Compressed Stabilized Earth Blocks Using Iron Mine Spoil Waste - An Explorative Study." Procedia Engineering 180 (2017): 1203–12. http://dx.doi.org/10.1016/j.proeng.2017.04.281.

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Stalker, Jeralee, Arthur w. Rose, and Louise H. Michaud. "REMEDIATION OF ACID MINE DRAINAGE WITHIN STRIP MINE SPOIL BY SULFATE REDUCTION USING WASTE ORGANIC MATTER." Journal American Society of Mining and Reclamation 1996, no. 1 (1996): 321–35. http://dx.doi.org/10.21000/jasmr96010321.

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Paszek, Natalia, and Marcin Górski. "Defining the optimal mixture composition of geopolymers based on the coal mine waste and the shale." MATEC Web of Conferences 274 (2019): 01002. http://dx.doi.org/10.1051/matecconf/201927401002.

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Nowadays, industry plays one of the main roles in daily life. Extractive industry is one of the oldest industries, present in almost each country. Unfortunately, besides the benefits connected with development of the extractive industry, there are also disadvantages such as enlarging amounts of stored industrial wastes. One of the ideas how to manage with unnecessary wastes is geopolymer, relatively new material which parameters are similar to the parameters of the concrete. The paper shows the following attempts to define optimal mixture composition of geopolymer based on the wastes from the coal mine and geopolymer based on the shale from the post-mining spoil tip. Coal mine waste, shale, powdered glass waste, metakaolin and sand were used as the raw materials. Sodium hydroxide and sodium silicate were used as activators. Mixtures consisting of mentioned components used in different ratios were prepared and poured into small moulds. The compressive strength of samples was tested after 3, 5 and 7 days. From the best mixture, the bigger samples of dimensions 4x4x4cm were prepared and tested after 7 and 14 days. The paper presents characteristics of used wastes, preparation and curing processes, test procedure and finally, compressive strengths and densities of tested geopolymers.
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Smith, J. A., G. E. Schuman, E. J. De Puit, and T. A. Sedbrook. "Wood Residue and Fertilizer Amendment of Bentonite Mine Spoils: I. Spoil and General Vegetation Responses." Journal of Environmental Quality 14, no. 4 (October 1985): 575–80. http://dx.doi.org/10.2134/jeq1985.00472425001400040020x.

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Smith, J. A., G. E. Schuman, E. J. DePuit, and T. A. Sedbrook. "Wood Residue and Fertilizer Amendment of Bentonite Mine Spoils: I. Spoil and General Vegetation Responses." Journal of Environmental Quality 14, no. 4 (October 1985): NP. http://dx.doi.org/10.2134/jeq1985.00472425001400040021x.

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Smith, J. A., G. E. Schuman, E. J. DePuit, and T. A. Sedbrook. "Wood Residue and Fertilizer Amendment of Bentonite Mine Spoils: I. Spoil and General Vegetation Responses." Journal of Environmental Quality 15, no. 2 (April 1986): 200. http://dx.doi.org/10.2134/jeq1986.00472425001500020024x.

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Zarychta, Adrian, and Roksana Zarychta. "Aplication of IDW and RBF methods to develop models of temperature distribution within a spoil tip located in Wojkowice, Poland." Environmental & Socio-economic Studies 6, no. 1 (March 1, 2018): 38–45. http://dx.doi.org/10.2478/environ-2018-0005.

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AbstractThis article describes two methods of showing the distribution of temperature on the surface and inside a spoil tip (coal mine waste dump) located in Wojkowice (in the Silesian Voivodeship). Two deterministic estimation methods were tested, i.e., Inverse Distance Weighting (IDW) and Radial Basis Functions (RBF). According to isotherm maps the highest temperature on the surface of the “Wojkowice” spoil tip was in the NE area, while inside the heap the highest temperature noted was in the SW area. Better results were obtained from the application of the RBF method. A three-dimensional model (3D model) was generated by the method, which visualized the temperature distribution within the “Wojkowice” spoil tip. According to the 3D model of the temperature distribution the greatest heat centre inside the heap in Wojkowice was located in the SW part with a temperature of around 300°C. As a result, it can be concluded that the material of the “Wojkowice” spoil tip is burning out in a NW direction. On the basis of the model obtained it is possible to determine the location of potentially dangerous places which are exposed to possible deformations caused by the material burning under the surface. The results of the research presented make it possible to assess the thermal state of the spoil heap located in Wojkowice, Poland.
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Dissertations / Theses on the topic "Mine spoil waste"

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Barajas-Aceves, Martha. "Soil microbial biomass and organic matter dynamics in metal-contaminated soils." Thesis, University of Nottingham, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.260604.

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Gizikoff, Katherine Gould. "Spoil management and revegetation success on waste rock dumps at a southern interior B.C. copper mine." Thesis, University of British Columbia, 1990. http://hdl.handle.net/2429/29031.

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The primary aim of this study was to investigate vegetation production and soil management factors influencing forage establishment on the waste rock dumps at a Southern Interior B.C. copper mine. Total plant cover on the waste rock dumps ranged from less than 5 to greater than 80 percent. Vegetation and spoil from the major reclaimed sites were analyzed to determine possible causes for the differences in plant cover. Test case areas, which varied in production, topography, and treatment, were then selected for an investigation into the relationships between spoil and vegetation variables. Waste rock and overburden glacial till materials were generally low in N, P, and Mg. Spoil N and K levels varied throughout each reclaimed site, likely as a result of fertilizer placement. Significant positive relationships were found between spoil N and grass cover and spoil K and both grass and legume cover. P levels in legumes from most fertilized sites were still in a deficiency range. A negative relationship between coarse fragment content and legume cover was observed. High coarse fragment content, accompanied with low water holding capacity and dry climatic conditions, suggests that moisture deficiencies are likely a critical problem for revegetation success, particularly on the lower portions of the slope faces. High bulk density values on the flat terraces indicated that compaction could be impeding root growth. Multivariate cluster analysis, based on total percent plant cover and percent composition legumes, was used to categorize all study sites into four vegetation production groups: low cover, grass cover, mixed grass and legume cover, and high production legume dominated cover. Spoil characteristics that differentiated between groups were: N, P, K, Mg, pH, coarse fragment content, and bulk density. This classification system will assist in identifying the management requirements of each vegetation type, such as: level and type of fertilization, overburden capping to reduce coarse fragment content, and scarification. Multiple regression analysis was used to generate equations for predicting biomass production from spoil N, P, K, Mg, pH, and coarse fragment content. Reclamation costs were estimated and it was demonstrated that grass cover and mixed grass and legume cover types were the most desirable. Although costs per hectare were lowest for the low cover type, efficiency of reclamation dollars (dollars invested per tonne forage produced) was also lowest for this type. Establishment of a legume dominated cover type may not be desirable due to forage quality considerations: Cu:Mo ratios in legume foliage averaged less than the recommended 2:1 for cattle grazing.
Science, Faculty of
Resources, Environment and Sustainability (IRES), Institute for
Graduate
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Modinger, Heinrich. "Micro-organisms involved in iron oxidation and acid mine drainage formation in KwaZulu-Natal and their control by soil covers on coal waste dumps." Thesis, Stellenbosch : Stellenbosch University, 1998. http://hdl.handle.net/10019.1/55926.

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Thesis (MSc)--Stellenbosch University, 1998.
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ENGLISH ABSTRACT: The biologically catalysed oxidation of pyrite in the outer layers of coal waste dumps leads to the formation of acid mine drainage. The oxidation of pyrite to ferric iron and sulphate is a complex process involving various abiotic and biologically catalysed reactions. Pyrite is abiotically oxidized by ferric iron, with the formation of thiosulphate and ferrous iron. Thiosulphate decomposes to form various inorganic sulphur compounds. Bacterial catalysis of pyrite oxidation is achieved by iron-oxidizing bacteria oxidizing ferrous iron to ferric iron. Bacteria that oxidize sulphur compounds assist the catalysis by oxidizing thiosulphate and its decomposition products. Heterotrophic organisms may play a role by consuming organic substances inhibitory to the lithotrophic bacteria. Abiotic ecological factors, acid formation and populations of iron-oxidizing bacterial groups were studied in 10 differently constructed pilot scale coal waste dumps, as the second phase of a study which started in September 1993. Gas samples were withdrawn weekly from coal waste through permanently buried stainless steel probes, for analysis in the field using a portable oxygen/carbon dioxide meter. Samples of coal waste were extracted by auger for analysis of moisture, pH and microbial populations. The analyses of oxygen and pH can be recommended for the routine monitoring of rehabilitated waste dumps. Covers of Avalon soil 0.3 or 0.5 m thick, were not adequate to prevent acidification. Coal waste covered with 0.7 m compacted beneath 0.3 m uncompacted Avalon soil, showed a slow pH decline, but reached approximately pH 3 in 1997. Covers of compacted Estcourt soil beneath tmcompacted Avalon soil to a cover depth of 1 m were effective in preventing acidification and generally kept the coal waste anaerobic. However, all covers developed cracks during drought conditions in 1995, allowing aeration. Low pH of some samples from these dumps during 1995/1996 may have indicated the start of acidification. Bacteria oxidizing high concentrations of ferrous iron and considered to be Thiobacillus ferrooxidans, were monitored routinely, but may not have been the dominant iron-oxidizer, as population counts using media with a lower ferrous iron concentration were higher. The majority of the latter organisms could also not oxidize sulphur, hence were not T. ferrooxidans. The populations of the high ferrous iron-oxidizing bacteria were affected by pH, tending to be high in acidified and low in non-acidified coal waste. Investigations of microbial populations forming iron-oxidizing consortia in enrichment cultures from coal waste and acid drainage samples showed the presence of T. ferrooxidans, the heterotrophic bacterial genus Acidiphilium, fungi of the genus Penicillium, unidentified filamentous fungi, including Cladophialophora-like morphological types, and a yeast of the genus Dipodascus. In interaction studies, the Penicillium isolate had an inhibitory effect on T. ferrooxidans (subjected to organic compound stress), but the Cladophialophora-like fungi reduced inhibition by organics. Fungi have not previously been studied in detail as components of iron-oxidizing consortia, but the bacterial isolations agree with those elsewhere, indicating that appropriate conclusions from acid mine drainage research in other parts of the world can be applied in KwaZulu-Natal.
AFRIKAANSE OPSOMMING: Die biologies gekataliseerde oksidasie van piriet in die buitenste lae van steenkoolafvalhope lei tot die vorming van suur mynafloopwater. Die oksidasie van piriet tot ferri-yster en sulfaat is 'n komplekse proses wat abiotiese en biologies gekataliseerde reaksies insluit. Piriet word abioties deur ferri-yster geoksideer, met die vrystelling van tiosulfaat en ferro-yster. Tiosulfaat verval om verskeie anorganiese swawelverbindings te vorm. Bakteriese katalise van pirietoksidasie word deur ysteroksiderende bakteriee wat ferro-yster na ferri-yster oksideer, bewerkstellig. Bakteriee wat swawelverbindings oksideer maak 'n bydrae tot die katalise deur tiosulfaat en vervalprodukte daarvan te oksideer. Heterotrofe organismes mag ook 'n rol speel deur organiese verbindings wat die litotrofe bakteriee mag inhibeer, te verbruik. Abiotiese ekologiese faktore, suurvorming en bevolkings ysteroksiderende bakteriee is in 10 verskillend gekonstrueerde loodsskaal steenkoolafvalhope bestudeer, as die tweede fase van 'n studie wat in September 1993 begin het. Gas monsters is weekliks uit die steenkoolafval onttrek deur vlekvrye staal peilers wat permanent daarin begrawe is, en met behulp van 'n draagbare suurstoflkoolstofdioksiedanaliseerder in die veld ontleed. Monsters van die steenkoolafval is met behulp van 'n kleiboor vir die analise van vog, pH en mikrobepopulasies geneem. Die analise van suurstof en pH kan aanbeveel word vir die roetiene monitering van gerehabiliteerde afvalhope. Bedekkings van 0.3 of 0.5 m Avalongrond was nie voldoende om suurvorming te verhoed nie. Steenkoolafval wat met 0.7 m gekompakteerde en 0.3 m ongekompakteerde Avalongrond bedek is, het 'n stadige pH-daling getoon, maar het in 1997 ongeveer pH 3 bereik. Bedekkings van gekompakteerde Estcourtgrond onder ongekompakteerde A valongrond met 'n totale dikte van 1 m, was effektief in die voorkoming van suurvorming. Hulle het oor die algemeen die steenkoolafval anaerobies gehou, maar aile bedekings het tydens die droogte in 1995 krake ontwikkel, wat suurstof laat binnedring het. 'n Lae pH gedurende 1995/1996 by sommige monsters uit hierdie hope mag die begin van suurvorming aangedui het. Bakteriee wat hoe konsentrasies ferro-yster oksideer en wat as Thiobacillus ferrooxidans beskou is, was moontlik nie die dominante ysteroksideerder nie, aangesien bevolkingstellings waar 'n medium met 'n laer konsentrasie ferro-yster gebruik is, hoer bevolkings getoon het. Die meerderheid van laasgenoemde organismes kon ook nie swawel benut nie en dus nie T. ferrooxidans was nie. Die bevolkings van die hoe ferro-ysteroksiderende bakteriee is deur pH beInvloed, met 'n geneigdheid tot hoe bevolkings in suur en lae bevolkings in minder suur steenkoolafval. Ondersoeke na die rnilcrobebevollcings wat in ysteroksiderende konsortia in verryldngslculture vanaf steenkoolafval- en suur mynafloopwatermonsters voorgekom het, het die teenwoordigheid van 7'. ferrooxidans, die heterotrofe balcteriegenus Acidiphilium, fungi van die genus Penicillium, ongeIdentifiseerde fungi, insluitend Cladophialophora-agtige tipes en 'n gis van die genus Dipodascus aangetoon. By interaksiestudies het die Penicillium-isolaat 'n inhiberende effek op T ferrooxidans (onderworpe aan organiese verbindingstres) gehad, maar die Cladophialophora-agtige fungi het die inhibisie deur organiese verbindings verminder. Fungi is nog the in detail as komponente van ysteroksiderende konsortia bestudeer the, maar die isolasies van bakteried stem saam met die van elders wat aandui dat toepaslike gevolgtreldcings ten opsigte van suur mynafloopwatemavorsing vanaf ander dele van die wereld ook in KwaZulu-Natal toegepas kan word.
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Burkey, Michael F. "A REVIEW OF IRON SULFIDES AND OXIDES IN COAL MINE WASTE, HUFF RUN WATERSHED, OHIO." Kent State University Honors College / OhioLINK, 2018. http://rave.ohiolink.edu/etdc/view?acc_num=ksuhonors1525905282950671.

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Cleghorn, Charles 1970. "Effect of soil covers on coal waste dumps in KwaZulu-Natal on abiotic factors and bacteria causing acid mine drainage." Thesis, Stellenbosch : Stellenbosch University, 1997. http://hdl.handle.net/10019.1/55521.

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Thesis (MSc)--Stellenbosch University, 1997.
ENGLISH ABSTRACT: The activity of iron-oxidizing bacteria, for example, Thiobacillut. ferrooxidans, in the outer layers of coal waste dumps results in the oxidation of pyrite with the formation of large volumes of acid mine drainage. The process requires atmospheric oxygen and moisture. Acid mine drainage may possibly be controlled by creating unfavourable environmental conditions in dumps for the iron-oxidizing bacteria. The present research investigated the possibility of inhibiting these bacteria and consequently acid formation in coal waste dumps by means of different dump construction techniques. Physical and chemical conditions, acid formation and populations of four groups of bacteria which might produce acid were studied in the outer layers of ten differently constructed pilot scale coal waste dumps at the Kilbarchan Mine near Newcastle, Kwazulu-Natal, from September 1993 to July 1995. Dump covers consisting of a 30-cm or 70-cm layer of Estcourt soil of low permeability covered with 70 cm or 30 cm, respectively, of more permeable Avalon soil produced anaerobic conditions in the dumps throughout most of the 22 months of the test period, as did a cover of 70 cm compacted plus 30 cm uncompacted Avalon soil alone. An uncoMpacted 30-cm or compacted 50- cm Avalon soil cover proved ineffective in causing prolonged anaerobic conditions. Uncovered dumps showed only slight reduction of oxygen in the coal waste after heavy rains. Pockets of acidity were detected on several occasions in the coal waste below the 50-cm Avalon soil layer from the time of construction and progressively increasing acidity in the uncovered dumps and the waste below the 30-cm Avalon soil cover. Iron-oxidizing bacterial populations of the T. ferrooxidans type have tended to be higher in the uncovered dumps and Avalon soil-covered dumps showing acidification than in the non-acidified dumps covered with 1 m of Avalon soil or Avalon and Estcourt soil. Associated populations of iron-oxidizing bacteria of the Metallogenium type, acidophilic and non-acidophilic thiosulphate-oxidizing bacteria were generally low in the coal waste of the dumps. Thus, five of the soil covers, all with a thickness of 1 m, but not covers with a thickness of 0.5 m or less, proved effective for almost 2 years in inhibiting the diffusion of oxygen to the underlying coal waste in the pilot scale dumps and also appeared to suppress the populations of iron-oxidizing bacteria believed to be implicated in acid formation in the coal waste. These results suggest that coal waste dumps in South Africa should be covered with soil layers of 0.5-1.0 m thick to prevent the generation of acid mine drainage.
AFRIKAANSE OPSOMMING: Die aktiwiteit van ysteroksiderende bakteriee soos Thiobacillus ferrooxidans, in die buitenste lae van steenkoolafvalhope, veroorsaak die oksidasie van piriet met die gevolg dat groot volumes suur mynafloopwater gevorm word. Hierdie proses benodig suurstof en vog. Suur mynafloopwater kan moontlik beheer word deur 'n situasie te skep waar die toestande in die hope ongunstig is vir die ysteroksiderende bakteriee. Die huidige navorsing het die moontlikheid ondersoek om hierdie bakteriee te inhibeer deur verskillende afvalhoopontwerpe op die proef te stel en sodoende suurvorming in steenkoolmynhope te beperk. Die fisiese en chemies kondisies, suurvorming en populasies van vier verskillende bakterie-groepe wat dalk by suurvorming betrokke is, is vanaf September 1993 tot Julie 1995 bestudeer in die buitenste lae van tien verskillend gekonstrueerde loodsskaalafvalhope by die Kilbarchan myn naby Newcastle in KwaZulu-Natal. Afvalhoopbedekkings bestaande uit 'n 30-cm of 70-cm Estcourt grond met 'n lae permeabiliteit bedek met'n 70-cm of 30-cm laag van meer deurlaatbare Avalon grond het anaerobe kondisies veroorsaak. Ongekompakteerde 30-cm en gekompakteerde 50-cm Avalon grondlae het egter nie bestendige anaerobe kondisies in die hope veroorsaak nie. Die onbedekte hope het aerobics gebly met slegs effense dalings van suurstofkonsentrasies gedurende en na swaar reens. Geisoleerde monsters uit die steenkoolafval onder die 50-cm Avalon grondlaag het vanaf die begin van die toetsperiode tekens van suurvorming getoon. Die onbedekte steenkoolafval en die van die sel met 'n 30-cm Avalon grondlaag het met verloop van tyd al hoe meer suur geword. Die ysteroksiderende bakterie-populasies van die T. ferrooxidans tipe het geblyk om in die onbedekte en Avalon grondbedekte hope wat tekens van suurvorming getoon het hoer te wees as in die hope wat met 'n 1-m laag Avalon grond of Avalon en Estcourt grond bedek is en geen tekens van suurvorming getoon het nie. Ysteroksiderende bakteriepopulasies van die Metallogenium tipe, nieasidofiele en asidofiele tiosulfaatoksiderende populasies was oor die algemeen laag in die steenkoolafvalhope. Vyf van die grondlae wat alma! 1 m dik was het dus geblyk om effektief te wees in die bekamping van die infiltrasie van suurstof na die onderliggende steenkoolafval in die loodskaalhope. Dit lyk asof daardie lae die ysteroksiderende populasies betrokke by suurvorming onderdruk het. Die 0.5-m grondbedekking het egter nie so 'n sterk onderdrukkende effek op die suurstofinfiltrasie of die bakteriepopulasie gehad nie. Na aanleiding van hierdie resultate blyk dit dat steenkoolafvalhope in Suid-Afrika met minstens 0.5 tot 1..0 m grond bedek moet word om effektief die probleem van suur mynafloopwater te bekamp.
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Langdon, Caroline Juliet. "Relationships between lumbricid earthworms and arsenic-rich mine spoil wastes." Thesis, Lancaster University, 2001. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.274279.

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Books on the topic "Mine spoil waste"

1

Boldt, C. M. K. Remote sensing of mine waste. Washington, DC: U.S. Dept.of the Interior, 1987.

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Boldt, C. M. K. Remote sensing of mine waste. Pittsburgh, Pa: U.S. Dept. of the Interior, Bureau of Mines, 1987.

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Jobling, J. Tree planting in colliery spoil. Edinburgh: Forestry Commission, 1985.

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Francis, Richard E. Vegetation establishment on reclaimed coal mine spoils in northwestern New Mexico. Fort Collins, Colo: USDA Forest Service, Rocky Mountain Forest and Range Experiment Station, 1991.

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Broughton, L. M. Mine rock guidelines: Design and control of drainage water quality. [Prince Albert, Canada]: The Branch, 1992.

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Colorado State University. Geotechnical Engineering Program., ed. Tailings and mine waste '98: Proceedings of the Fifth International Conference on Tailings and Mine Waste '98, Fort Collins, Colorado, USA, 26-28 January 1998. Rotterdam: A.A. Balkema, 1998.

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Dierichs, Dieter. Untersuchungen zum Verhalten locker gelagerter wassergesättigter Sande als Basis für die Bewertung der Standsicherheit von Kippenböschungen. Leipzig: Deutscher Verlag für Grundstoffindustrie, 1988.

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International, Conference on Tailings and Mine Waste (9th 2002 Fort Collins Colo ). Tailings and mine waste '02: Proceedings of the ninth International Conference on Tailings and Mine Waste, Fort Collins, Colorado, USA, 27-30 January 2002. Rotterdam: Balkema, 2002.

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International Conference on Tailings & Mine Waste (4th 1997 Fort Collins, Colo.). Tailings and mine waste '97: Proceedings of the Fourth International Conference on Tailings and Mine Waste '97, Fort Collins, Colorado, USA, 13-17 January 1997. Rotterdam: A.A. Balkema, 1997.

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International Conference on Tailings and Mine Waste (7th 2000 Fort Collins, Colo.). Tailings and mine waste '00: Proceedings of the Seventh International Conference on Tailings and Mine Waste '00, Fort Collins, Colorado, USA, 23-26 January 2000. Rotterdam: Balkema, 2000.

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Book chapters on the topic "Mine spoil waste"

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Lamb, Dane, Peter Sanderson, Liang Wang, Mohammed Kader, and Ravi Naidu. "Phytocapping of Mine Waste at Derelict Mine Sites in New South Wales." In Spoil to Soil, 215–39. Taylor & Francis Group 6000 Broken Sound Parkway NW, Suite 300 Boca Raton, FL 33487-2742: CRC Press, 2017. http://dx.doi.org/10.1201/9781351247337-18.

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Simmers, J. W., G. S. Wilhelm, J. M. Marquenie, R. G. Rhett, and S. H. Kay. "Reclamation of Pyritic Mine Spoil Using Contaminated Dredged Material." In Environmental Management of Solid Waste, 208–23. Berlin, Heidelberg: Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-642-61362-3_12.

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Loxham, M. "The Predictive Assessment of the Migration of Leachate in the Subsoils Surrounding Mine Tailing and Dredging Spoil Sites." In Environmental Management of Solid Waste, 3–23. Berlin, Heidelberg: Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-642-61362-3_1.

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Sarkar, Binoy, Hasintha Wijesekara, Sanchita Mandal, Mandeep Singh, and Nanthi S. Bolan. "Characterization and Improvement in Physical, Chemical, and Biological Properties of Mine Wastes." In Spoil to Soil, 3–15. Taylor & Francis Group 6000 Broken Sound Parkway NW, Suite 300 Boca Raton, FL 33487-2742: CRC Press, 2017. http://dx.doi.org/10.1201/9781351247337-3.

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Roque, Antonio Jose, and Vitor Monteiro. "Hazardous Waste Dumped on the Spoils of an Old Coal Mine (Portugal) – Environmental Rehabilitation of the Site for Reuse." In Environmental Science and Engineering, 764–71. Singapore: Springer Singapore, 2018. http://dx.doi.org/10.1007/978-981-13-2221-1_86.

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Vacher, Cameron, David Williams, and Rob Loch. "Risk assessment applied to tunnel erosion of mine spoils." In Tailings and Mine Waste '04, 63–70. Taylor & Francis, 2004. http://dx.doi.org/10.1201/9780203021637.ch8.

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Conference papers on the topic "Mine spoil waste"

1

Bohn, D., G. H. Dibelius, R. U. Pitt, R. Faatz, G. Cerri, and C. Salvini. "Optimizing a Pressurized Fluidized Bed Combustion Combined Cycle With Gas Turbine Topping Cycle." In ASME 1993 International Gas Turbine and Aeroengine Congress and Exposition. American Society of Mechanical Engineers, 1993. http://dx.doi.org/10.1115/93-gt-390.

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Abstract:
Combined Cycles for the generation of electricity or co-generation of heat and power with Pressurized Fluidized Bed Combustion (PFBC) of coal and a gas turbine topping cycle fired with a fuel suitable for gas turbines have been studied to set up optimum process parameters with respect to net efficiency, emissions including CO2, and keeping in mind the feasibility of the plant components. As a basic approach, natural gas has been considered as a fuel for the topping gas turbine. Net efficiencies up to 50% (LHV) are acheived. For the calculations, a Recursive Equality Constraint Quadratic Programming Method (RECQPM) is applied. The method is semi-implicit, i. e. the equations describing the process are solved using a non-linear equations system solver; the modular structure of the cycle is, however, made up for by programme modules set up for the relevant components/units. With the process layouts studied, the PFBC should be operated at a pressure level to allow for a compact design of the PFBC steam generator and the Hot Gas Clean-Up Unit (HGCU), and to take advantage of the pressure with respect to combustion efficiency, in-bed sulfur retention and NOx-reduction. The overall pressure ratio of the topping gas turbine, e. g. consisting of an LP-compressor plus a free running HP spool, and exhausting to the PFB combustor, should be in the range of 30. Further developments of gas turbine technology with respect to pressure ratio and turbine inlet temperature can be incorporated into the process and will be associated with an increase of overall efficiency. The heat to be extracted from the coal fired PFBC at the typical combustion temperature of 850°C allows for steam generation at conventional live steam and reheat temperatures (and pressures). The incorporation of advanced steam cycle parameters, as actually considered for pulverized coal fired boilers, would again increase the overall net efficiency of the cycle by some 5% with an increase of both the live steam and the reheat temperature from 540°C to 600°C. In contrast to conventional combined cycles with an unfired waste heat boiler for steam generation, the overall efficiency of the PFBC combined cycle with gas turbine topping cycle is only marginally affected by dual pressure steam cycle arrangements, except for very sophisticated and costly designs. To use gas from an integrated coal gasification unit rather than natural gas as a fuel for the topping gas turbine would result in an entirely coal based process. Due to the capability of the PFBC to burn residues of coal gasification and gas purification, this process, compared to pure Integrated Gasification Combined Cycles (IGCC), is less sensitive to the carbon conversion acheived. Even more, the raw gas purification might be simplified, and the process efficiency might be increased as a result of the sulphur removal to be acheived in the PFBC rather than in a raw gas sweetening process. Some preliminary findings for a process with an integrated partial gasification unit are discussed.
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