A fundamental understanding of the process of devolatilization requires extensive knowledge of not only the intrinsic properties of the parent coal and its subsequent formed products (tars, gases and chars), but also its characteristic reaction rate behaviour. Devolatilization behaviour has been extensively addressed in literature with the use of powdered coal samples, which normally do not adhere to particle size constraints of coal conversion processes utilizing lump coal. The aim of this investigation was therefore to assess the devolatilization behaviour (with respect to product yield and -quality; and reaction rate modelling) of four typical South African coals (UMZ, INY, G#5 and TSH) confined to the large particle regime. All four coals were found to be bituminous in rank, with vitrinite contents ranging between 24.4 vol.% and 69.2 vol.% (mineral matter free basis). Two were inertinite-rich coals (UMZ and INY) and the other two were vitrinite-rich coals (G#5 and TSH). From thermoplasticity measurements it was evident that only coal TSH displayed extensive thermoplastic behaviour, while a comparison between molecular properties confirmed the higher abundance of poly-condensed aromatic structures (aromaticity of 81%) present in this coal. Product evolution was evaluated under atmospheric conditions in a self-constructed, large particle, fixed-bed reactor, on two particle sizes (5 mm and 20 mm) at two isothermal reactor temperatures (450°C and 750°C) using a combination of both GC and MS techniques for gas species measurement, while standard gravimetric methods were used to quantify tar- and char yield respectively. Elucidation of tar- and char structural features involved the use of both conventional- and advanced analytical techniques. From the results it could be concluded that temperature was the dominating factor controlling product yield- and quality, with significant increases in both volatile- and gas yield observed for an increase in temperature. Tar yields ranged between 3.6 wt.% and 10.1 wt.% and increased in the order UMZ < INY < TSH < G#5, with higher tar yields obtained for coal G#5, being ascribed to larger abundances of vitrinite and liptinite present in this coal. For coal TSH, lower tar yields could mainly be attributed to the higher aromaticity and extensive swelling nature of this coal. Evolved gases were found to be mainly composed of H2, CH4, CO and CO2, low molecular weight olefins and paraffins; and some C4 homologues. Advanced analytical techniques (NMR, SEC, GC-MS, XRD, etc.) revealed the progressive increase of the aromatic nature of both tars and chars with increasing temperature; as well as subsequent differences in tar composition between the different parent coals. In all cases, an increase in devolatilization temperature led to the evolution of larger amounts of aromatic compounds such as alkyl-naphthalenes and PAHs, while significant decreases in the amount of aliphatics and mixed compounds could be observed. From 13C NMR, HRTEM and XRD carbon crystallite results it was clear that an increase in temperature led to the formation of progressively larger, more aromatic and structurally orientated polycondensed carbon structures. Reaction rate studies involved the use of non-isothermal (5-40 K/min) and isothermal (350- 900°C) thermogravimetry of both powdered (-200 μm) and large particle samples (20 mm) in order to assess intrinsic kinetics and large particle rate behaviour, respectively. Evaluation of the intrinsic kinetic parameters of each coal involved the numerical regression of non-isothermal rate data in MATLAB® 7.1.1 according to a pseudo-component modelling philosophy. Modelling results indicated that the intrinsic devolatilization behaviour of each coal could be adequately described by using a total number of eight pseudo-components, while reported activation energies were found to range between 22.3 kJ/mol and 244.3 kJ/mol. Description of the rate of large particle devolatilization involved the evaluation of a novel, comprehensive rate model accounting for derived kinetics, heat and mass transport effects, as well as physical changes due to particle swelling/shrinkage. Evaluation of the proposed model with the aid of the COMSOL Multiphysics 4.3 simulation software provided a suitable fit to the experimental data of all four coals, while simulation studies highlighted the relevant importance of not only the effect of particle size, but also the importance of including terms affecting for heat losses due to particle swelling/shrinkage, transport of volatile products through the porous char structure, heat of reaction and heat of vaporization of water. / Thesis (PhD (Chemical Engineering))--North-West University, Potchefstroom Campus, 2013

Alkali compounds were added to a South African coal with a high swelling propensity and the behaviour of the blends were investigated. A vitrinite-rich bituminous coal from the Tshikondeni coal mine in the Limpopo province of South Africa was used. To reduce the influence of the minerals in the coal, the coal was partially demineralized by leaching with HCl and HF. The ash content of the coal sample was successfully reduced from 17.7% to 0.6%. KOH, KCl, K2CO3 and KCH3CO2 were then added to the demineralized coal in mass percentages of 1%, 4%, 5% and 10%. The free swelling indices (FSI) of the blends were determined and the samples were subjected to acquisition of TMA and TG-MS data. Addition of these potassium compounds to the demineralized coal reduced the swelling of the vitrinite-rich coal. From the free swelling indices of the various mixtures, it was concluded that the potassium compounds reduce the swelling of the coal in the following order of decreasing impact: KCH3CO2 > KOH > K2CO3 > KCl. From dilatometry experiments done on the blends with the 10% addition of potassium compounds, it was seen that with the addition of potassium compounds to the demineralized coal, a reduction in dilatation volume was obtained. The influence of the potassium compound in decreasing order: K2CO3> KOH> KCH3CO2> KCl. An increase in the softening temperature was observed for the demineralized coal-alkali blends. Thermogravimetric analyses were performed on the demineralized coal-potassium blended samples (<75 μm). These samples were pyrolyzed under a nitrogen atmosphere to a maximum temperature of 1200 °C using a heating rate of 10 °C/min. The relative reactivity for each of the blends with the different wt% addition was determined. From these results it was seen that KCH3CO2 increased the relative reactivity, whereas the KOH, KCl and K2CO3 showed an inhibiting influence. The attached mass spectrometer provided information on the low molecular mass gaseous products formed in the various temperature ranges as the thermal treatment proceeded. From the mass spectroscopy results, it was found that the potassium compounds decreased the temperature at which maximum evolution of H2 takes place. Thermomechanical analyses were performed on the 10 wt% addition of the potassium compounds to the demineralized coal. During TMA analyses, the sample was heated to 1000 °C using a heating rate of 10 °C/min. From the TMA result obtained it was clear that the addition of KCl did not have an influence on the swelling of the demineralized coal. All results are discussed. / MSc (Chemistry), North-West University, Potchefstroom Campus, 2014

A fundamental understanding of the process of devolatilization requires extensive knowledge of not only the intrinsic properties of the parent coal and its subsequent formed products (tars, gases and chars), but also its characteristic reaction rate behaviour. Devolatilization behaviour has been extensively addressed in literature with the use of powdered coal samples, which normally do not adhere to particle size constraints of coal conversion processes utilizing lump coal. The aim of this investigation was therefore to assess the devolatilization behaviour (with respect to product yield and -quality; and reaction rate modelling) of four typical South African coals (UMZ, INY, G#5 and TSH) confined to the large particle regime. All four coals were found to be bituminous in rank, with vitrinite contents ranging between 24.4 vol.% and 69.2 vol.% (mineral matter free basis). Two were inertinite-rich coals (UMZ and INY) and the other two were vitrinite-rich coals (G#5 and TSH). From thermoplasticity measurements it was evident that only coal TSH displayed extensive thermoplastic behaviour, while a comparison between molecular properties confirmed the higher abundance of poly-condensed aromatic structures (aromaticity of 81%) present in this coal. Product evolution was evaluated under atmospheric conditions in a self-constructed, large particle, fixed-bed reactor, on two particle sizes (5 mm and 20 mm) at two isothermal reactor temperatures (450°C and 750°C) using a combination of both GC and MS techniques for gas species measurement, while standard gravimetric methods were used to quantify tar- and char yield respectively. Elucidation of tar- and char structural features involved the use of both conventional- and advanced analytical techniques. From the results it could be concluded that temperature was the dominating factor controlling product yield- and quality, with significant increases in both volatile- and gas yield observed for an increase in temperature. Tar yields ranged between 3.6 wt.% and 10.1 wt.% and increased in the order UMZ < INY < TSH < G#5, with higher tar yields obtained for coal G#5, being ascribed to larger abundances of vitrinite and liptinite present in this coal. For coal TSH, lower tar yields could mainly be attributed to the higher aromaticity and extensive swelling nature of this coal. Evolved gases were found to be mainly composed of H2, CH4, CO and CO2, low molecular weight olefins and paraffins; and some C4 homologues. Advanced analytical techniques (NMR, SEC, GC-MS, XRD, etc.) revealed the progressive increase of the aromatic nature of both tars and chars with increasing temperature; as well as subsequent differences in tar composition between the different parent coals. In all cases, an increase in devolatilization temperature led to the evolution of larger amounts of aromatic compounds such as alkyl-naphthalenes and PAHs, while significant decreases in the amount of aliphatics and mixed compounds could be observed. From 13C NMR, HRTEM and XRD carbon crystallite results it was clear that an increase in temperature led to the formation of progressively larger, more aromatic and structurally orientated polycondensed carbon structures. Reaction rate studies involved the use of non-isothermal (5-40 K/min) and isothermal (350- 900°C) thermogravimetry of both powdered (-200 μm) and large particle samples (20 mm) in order to assess intrinsic kinetics and large particle rate behaviour, respectively. Evaluation of the intrinsic kinetic parameters of each coal involved the numerical regression of non-isothermal rate data in MATLAB® 7.1.1 according to a pseudo-component modelling philosophy. Modelling results indicated that the intrinsic devolatilization behaviour of each coal could be adequately described by using a total number of eight pseudo-components, while reported activation energies were found to range between 22.3 kJ/mol and 244.3 kJ/mol. Description of the rate of large particle devolatilization involved the evaluation of a novel, comprehensive rate model accounting for derived kinetics, heat and mass transport effects, as well as physical changes due to particle swelling/shrinkage. Evaluation of the proposed model with the aid of the COMSOL Multiphysics 4.3 simulation software provided a suitable fit to the experimental data of all four coals, while simulation studies highlighted the relevant importance of not only the effect of particle size, but also the importance of including terms affecting for heat losses due to particle swelling/shrinkage, transport of volatile products through the porous char structure, heat of reaction and heat of vaporization of water. / Thesis (PhD (Chemical Engineering))--North-West University, Potchefstroom Campus, 2013

In this study, imaging with ionizing radiation was evaluated as a research technique in coal research. Part of the evaluation was to conduct a thorough literature survey as well as a preliminary investigation into coal pyrolysis and gasification with micro–focus X–ray tomography. The literature survey summarizes previous research experiences, primarily focussing on the possibility of utilizing a specific coal bed for carbon dioxide sequestration and methane production. This includes quantifying the fracture and cleat network and visualizing the orientation of this network. The cleat and fracture spacing and aperture are used to calculate certain parameters necessary to model gas flow. Other aspects include non–destructive characterization which consisted of determining the porosity and the minerals and macerals present and the respective mineral distribution. The literature survey also includes a section on the utilization of neutrons in coal research and a description of a neutron imaging facility in South Africa is presented. Three coal samples from the Waterberg and Highveld regions of South Africa were used to investigate the process of pyrolysis through micro–focus X–ray tomography. The samples swelled significantly when 50% pyrolysis was achieved after which the samples became brittle. This verified the plastic nature of the coal, that is prevalent under these conditions. It was also possible to perform qualitative characterizations prior to and during the process. Regions of low and high density materials could also be visualized. The distribution of the minerals is indicative of the permeability of the organic matrix. Two coal samples of the Highveld regions were used to investigate gasification up to a level of 30%. It was possible to verify that the reaction progressed according to the mechanisms proposed by the un–reacted shrinking core model. The mineral matter and the high density coal macerals did not influence the reaction in any way. / http://hdl.handle.net//10394/7008 / Thesis (M.Ing. (Chemical Engineering))--North-West University, Potchefstroom Campus, 2012.

In this study, imaging with ionizing radiation was evaluated as a research technique in coal research. Part of the evaluation was to conduct a thorough literature survey as well as a preliminary investigation into coal pyrolysis and gasification with micro–focus X–ray tomography. The literature survey summarizes previous research experiences, primarily focussing on the possibility of utilizing a specific coal bed for carbon dioxide sequestration and methane production. This includes quantifying the fracture and cleat network and visualizing the orientation of this network. The cleat and fracture spacing and aperture are used to calculate certain parameters necessary to model gas flow. Other aspects include non–destructive characterization which consisted of determining the porosity and the minerals and macerals present and the respective mineral distribution. The literature survey also includes a section on the utilization of neutrons in coal research and a description of a neutron imaging facility in South Africa is presented. Three coal samples from the Waterberg and Highveld regions of South Africa were used to investigate the process of pyrolysis through micro–focus X–ray tomography. The samples swelled significantly when 50% pyrolysis was achieved after which the samples became brittle. This verified the plastic nature of the coal, that is prevalent under these conditions. It was also possible to perform qualitative characterizations prior to and during the process. Regions of low and high density materials could also be visualized. The distribution of the minerals is indicative of the permeability of the organic matrix. Two coal samples of the Highveld regions were used to investigate gasification up to a level of 30%. It was possible to verify that the reaction progressed according to the mechanisms proposed by the un–reacted shrinking core model. The mineral matter and the high density coal macerals did not influence the reaction in any way. / http://hdl.handle.net//10394/7008 / Thesis (M.Ing. (Chemical Engineering))--North-West University, Potchefstroom Campus, 2012.

Please read the abstract in the section 00front of this document / Dissertation (M Eng (Metallurgical Engineering))--University of Pretoria, 2006. / Materials Science and Metallurgical Engineering / unrestricted

Over the past decade, the regulation of mining in South Africa has undergone a fundamental transformation in order to promote equitable access to the nation’s mineral and petroleum resources. The Mineral and Petroleum Resources Development Act 28 of 2002, drastically changed the regulation of mining by placing the nation’s mineral and petroleum resources under the custodianship of the state. The transformative objectives of resource reform, as envisaged in the Constitution of the Republic of South Africa, 1996, could however not be achieved without a measure of sacrifice -- most notably, that which had to be shouldered by the owners of the land in which the minerals are contained. Under common law, minerals vested in the owners of land and no one could compel them to extract or consent to the extraction of these minerals. Landowners were able to safeguard their land from mining activities by refusing to consent to mining. The Mineral and Petroleum Resources Development Act, 2002, changed this by providing that landowners could no longer prevent the state from granting qualifying applicants authorisation to mine. The transformative objectives of resource reform, have inevitably made great inroads into a landowner’s rights to use and enjoy his property optimally. The main focus of this study revolves around the limiting impact of South Africa’s current mineral-law dispensation on township development, and conversely, how township development impairs or limits the mining of coal. For a better understanding of the limitations which the current legislative provisions create in respect of the rights of landowners and holders of mining rights, a brief evaluation of the historical development of the right to mine coal is provided. The entitlements and reciprocal obligations of holders of mining rights and owners of the affected land are considered, and the parties’ legal remedies to resist interference in their respective rights are explored. In the process of considering possible remedies to resolve the conflict which inevitably arises, I explain why English-law principles governing lateral support (support owed by two adjacent properties [neighbour law]), and subjacent support (where the landowner may not be deprived of the vertical support his property derives from the sub-surface minerals) were incorrectly transplanted into our law. In Anglo Operations Ltd v Sandhurst Estates (Pty) Ltd, the South African Supreme Court of Appeal rejected the previously-held view that the right to subjacent support -- like the right to lateral support -- is a natural property right incidental to the ownership of the land. It was further held that conflict between holders of rights to minerals and owners of land should be resolved, not in accordance with English-law principles of neighbour law, but in terms of the law developed for rights relating to the use of servitudes. In summary, the court found that where the parties have not specifically contracted against the specific action (such as opencast or planned-subsidence mining), and provided that it was reasonably necessary for the mining right holder to use this invasive method, he may do so, so long as he does so in the manner least injurious to the entitlements of the surface owner. This decision, however, did not take into account the changes brought about by the comprehensive statutory framework of the Mineral and Petroleum Resources Development Act 28 of 2002 which I argue has replaced the earlier servitude construction. In this dissertation I consider whether possible solutions to resolve the conflict can be found in the principles relating to neighbour law, and whether the principles governing the use of servitudes remain relevant in resolving conflicts between landowners and holders of mining rights. I evaluate possible legal remedies and place special emphasis on the constitutionality of the curtailment of a landowner’s use and enjoyment of his property resulting from mining activities on or under his land. I further consider whether the exercise of a mining right, granted by the state, which results in a serious infringement of a landowner’s ownership, could in certain circumstances amount to a deprivation or possibly an expropriation in terms of section 25 of the Constitution. I discuss the position where the state’s regulatory interference is so severe that it deprives a landowner of the ability to exercise any, or a substantial portion of his ownership entitlements. I evaluate the possibility that such interference may constitute de facto expropriation for which compensation may be claimed. In the penultimate chapter I briefly mention how the relationship between landowners and holders of mining rights is managed and conflict is defused in other jurisdictions such as China, Australia, the United States of America, India, Germany and Swaziland. I conclude this dissertation with suggestions on possible ways in which the conflict may be resolved or at least minimised in future. / Die regulering van mynbou in Suid-Afrika het die afgelope dekade ‘n fundamentele verandering ondergaan ten einde breër toegang tot die nasie se minerale en petroleum hulpbronne te bevorder. Die Mineral and Petroleum Resources Development Act,6 Wet 28 van 2002, het ‘n radikale ommekeer in die mynbou industrie meegebring deurdat die regulering van mynbou aktiwiteite onder die toesig en beheer van die nasionale regering geplaas is. Die transformatiewe oogmerk van hulpbron hervorming ingevolge die Grondwet van die Republiek van Suid-Afrika kon egter nie geskied sonder ‘n mate van opoffering nie. Die grootste aanslag van die nuwe mineraalreg bedeling word sonder twyfel gevoel deur die eienaars van grond ten opsigte waarvan mynregte deur die regering aan ‘n ander party toegeken word. Ingevolge die gemenereg was die eienaar van grond voorheen ook die eienaar van die minerale wat in die grond voorgekom het. Gevolglik was dit onder die uitsluitlike beheer van die eienaar om te bepaal of enigiemand anders die reg kon verkry om minerale op of in die betrokke grond te ontgin. Na aanvang van die inwerkingtreding van die Mineral and Petroleum Resources Development Act is hierdie posisie egter omvêrgewerp aangesien die regering voortaan die bevoegdheid het om te bepaal wie en op watter voorwaardes iemand die reg verkry om minerale te ontgin. Die toekenning van die reg om minerale te ontgin op ‘n ander se eiendom sonder die eienaar se toestemming, maak dus ernstige inbreuk op sy regte. Grondeienaars se bevoegdhede wat uit hul eiendomsreg voortvloei word in talle gevalle ernstig ingeperk ten einde die oogmerke van hulpbron transformasie te bereik. Die ondersoek wat hierna volg, is daarop toegespits om die beperkende aanslag van die regulering van steenkoolmynbou-aktiwiteite op die ontwikkeling van dorpsgebiede asook dié van die ontwikkeling van dorpsgebiedie op steenkoolmynbou beter te verstaan. Ten einde hierdie invloed beter te verstaan, word die geskiedkundige ontwikkeling van die reg om minerale in Suid-Afrika te ontgin kortliks oorweeg. Die regte en verpligtinge van die houers van mynregte en die eienaars van die grond wat deur die uitoefening daarvan geraak word, asook die remedies waaroor die onderskye partye beskik ten einde hul regte teen inbreukmaking deur die ander party te beskerm, word daarna oorweeg. In genoemde ondersoek toon ek aan waarom die Engelsregtelike burereg- beginsels van laterale steun en onderstut nie toepassing in ons reg behoort te vind nie en waarom die botsing wat ontstaan vanweë die uitoefening van die grondeienaar en die houer van ‘n mynreg se regte liefs versoen moet word deur die Suid-Afrikaanse serwituutreg beginsels toe te pas soos aangetoon in die beslissing van Anglo Operations Ltd v Sandhurst Estates. Hiedie beslissing het egter nie die veranderinge wat meegebring is deur die nuwe bedeling van die Mineral and Petroleum Resources Development Act in ag geneem nie en daar word gevolglik aangevoer dat die serwituut beginsels vervang is deur ‘n breedvoerige wetgewende stelsel. Die grondwetlikheid van die beperking op die bevoegdhede van ‘n grondeienaar om sy eiendom te gebruik en te geniet, word ondersoek, asook of daar enige gronde vir ‘n eis om skadevergoeding mag wees. In besonder word daar oorweeg of die leerstuk van konstruktiewe onteiening moontlik toepassing kan vind in gevalle waar die staat se regulering ‘n uitermatige beperkende effek het op die bevoegdhede van ‘n grondeienaar om sy eiendomsreg uit te oefen. In die voorlaaste hoofstuk ontleed ek baie kortliks hoe die verhouding tussen eienaars van grond in mynbougebiede en houers van regte om minerale te ontgin in Sjina, Australië, die Verenigde State van Amerika, Indië, Duitsland en Swaziland gereguleer word. Ter afsluiting word aandag gegee aan moontlike maniere om die belangebotsing tussen die betrokke partye uit die weg te ruim of te beperk. / Private Law / LL.M.

Over the past decade, the regulation of mining in South Africa has undergone a fundamental transformation in order to promote equitable access to the nation’s mineral and petroleum resources. The Mineral and Petroleum Resources Development Act 28 of 2002, drastically changed the regulation of mining by placing the nation’s mineral and petroleum resources under the custodianship of the state. The transformative objectives of resource reform, as envisaged in the Constitution of the Republic of South Africa, 1996, could however not be achieved without a measure of sacrifice -- most notably, that which had to be shouldered by the owners of the land in which the minerals are contained. Under common law, minerals vested in the owners of land and no one could compel them to extract or consent to the extraction of these minerals. Landowners were able to safeguard their land from mining activities by refusing to consent to mining. The Mineral and Petroleum Resources Development Act, 2002, changed this by providing that landowners could no longer prevent the state from granting qualifying applicants authorisation to mine. The transformative objectives of resource reform, have inevitably made great inroads into a landowner’s rights to use and enjoy his property optimally. The main focus of this study revolves around the limiting impact of South Africa’s current mineral-law dispensation on township development, and conversely, how township development impairs or limits the mining of coal. For a better understanding of the limitations which the current legislative provisions create in respect of the rights of landowners and holders of mining rights, a brief evaluation of the historical development of the right to mine coal is provided. The entitlements and reciprocal obligations of holders of mining rights and owners of the affected land are considered, and the parties’ legal remedies to resist interference in their respective rights are explored. In the process of considering possible remedies to resolve the conflict which inevitably arises, I explain why English-law principles governing lateral support (support owed by two adjacent properties [neighbour law]), and subjacent support (where the landowner may not be deprived of the vertical support his property derives from the sub-surface minerals) were incorrectly transplanted into our law. In Anglo Operations Ltd v Sandhurst Estates (Pty) Ltd, the South African Supreme Court of Appeal rejected the previously-held view that the right to subjacent support -- like the right to lateral support -- is a natural property right incidental to the ownership of the land. It was further held that conflict between holders of rights to minerals and owners of land should be resolved, not in accordance with English-law principles of neighbour law, but in terms of the law developed for rights relating to the use of servitudes. In summary, the court found that where the parties have not specifically contracted against the specific action (such as opencast or planned-subsidence mining), and provided that it was reasonably necessary for the mining right holder to use this invasive method, he may do so, so long as he does so in the manner least injurious to the entitlements of the surface owner. This decision, however, did not take into account the changes brought about by the comprehensive statutory framework of the Mineral and Petroleum Resources Development Act 28 of 2002 which I argue has replaced the earlier servitude construction. In this dissertation I consider whether possible solutions to resolve the conflict can be found in the principles relating to neighbour law, and whether the principles governing the use of servitudes remain relevant in resolving conflicts between landowners and holders of mining rights. I evaluate possible legal remedies and place special emphasis on the constitutionality of the curtailment of a landowner’s use and enjoyment of his property resulting from mining activities on or under his land. I further consider whether the exercise of a mining right, granted by the state, which results in a serious infringement of a landowner’s ownership, could in certain circumstances amount to a deprivation or possibly an expropriation in terms of section 25 of the Constitution. I discuss the position where the state’s regulatory interference is so severe that it deprives a landowner of the ability to exercise any, or a substantial portion of his ownership entitlements. I evaluate the possibility that such interference may constitute de facto expropriation for which compensation may be claimed. In the penultimate chapter I briefly mention how the relationship between landowners and holders of mining rights is managed and conflict is defused in other jurisdictions such as China, Australia, the United States of America, India, Germany and Swaziland. I conclude this dissertation with suggestions on possible ways in which the conflict may be resolved or at least minimised in future. / Die regulering van mynbou in Suid-Afrika het die afgelope dekade ‘n fundamentele verandering ondergaan ten einde breër toegang tot die nasie se minerale en petroleum hulpbronne te bevorder. Die Mineral and Petroleum Resources Development Act,6 Wet 28 van 2002, het ‘n radikale ommekeer in die mynbou industrie meegebring deurdat die regulering van mynbou aktiwiteite onder die toesig en beheer van die nasionale regering geplaas is. Die transformatiewe oogmerk van hulpbron hervorming ingevolge die Grondwet van die Republiek van Suid-Afrika kon egter nie geskied sonder ‘n mate van opoffering nie. Die grootste aanslag van die nuwe mineraalreg bedeling word sonder twyfel gevoel deur die eienaars van grond ten opsigte waarvan mynregte deur die regering aan ‘n ander party toegeken word. Ingevolge die gemenereg was die eienaar van grond voorheen ook die eienaar van die minerale wat in die grond voorgekom het. Gevolglik was dit onder die uitsluitlike beheer van die eienaar om te bepaal of enigiemand anders die reg kon verkry om minerale op of in die betrokke grond te ontgin. Na aanvang van die inwerkingtreding van die Mineral and Petroleum Resources Development Act is hierdie posisie egter omvêrgewerp aangesien die regering voortaan die bevoegdheid het om te bepaal wie en op watter voorwaardes iemand die reg verkry om minerale te ontgin. Die toekenning van die reg om minerale te ontgin op ‘n ander se eiendom sonder die eienaar se toestemming, maak dus ernstige inbreuk op sy regte. Grondeienaars se bevoegdhede wat uit hul eiendomsreg voortvloei word in talle gevalle ernstig ingeperk ten einde die oogmerke van hulpbron transformasie te bereik. Die ondersoek wat hierna volg, is daarop toegespits om die beperkende aanslag van die regulering van steenkoolmynbou-aktiwiteite op die ontwikkeling van dorpsgebiede asook dié van die ontwikkeling van dorpsgebiedie op steenkoolmynbou beter te verstaan. Ten einde hierdie invloed beter te verstaan, word die geskiedkundige ontwikkeling van die reg om minerale in Suid-Afrika te ontgin kortliks oorweeg. Die regte en verpligtinge van die houers van mynregte en die eienaars van die grond wat deur die uitoefening daarvan geraak word, asook die remedies waaroor die onderskye partye beskik ten einde hul regte teen inbreukmaking deur die ander party te beskerm, word daarna oorweeg. In genoemde ondersoek toon ek aan waarom die Engelsregtelike burereg- beginsels van laterale steun en onderstut nie toepassing in ons reg behoort te vind nie en waarom die botsing wat ontstaan vanweë die uitoefening van die grondeienaar en die houer van ‘n mynreg se regte liefs versoen moet word deur die Suid-Afrikaanse serwituutreg beginsels toe te pas soos aangetoon in die beslissing van Anglo Operations Ltd v Sandhurst Estates. Hiedie beslissing het egter nie die veranderinge wat meegebring is deur die nuwe bedeling van die Mineral and Petroleum Resources Development Act in ag geneem nie en daar word gevolglik aangevoer dat die serwituut beginsels vervang is deur ‘n breedvoerige wetgewende stelsel. Die grondwetlikheid van die beperking op die bevoegdhede van ‘n grondeienaar om sy eiendom te gebruik en te geniet, word ondersoek, asook of daar enige gronde vir ‘n eis om skadevergoeding mag wees. In besonder word daar oorweeg of die leerstuk van konstruktiewe onteiening moontlik toepassing kan vind in gevalle waar die staat se regulering ‘n uitermatige beperkende effek het op die bevoegdhede van ‘n grondeienaar om sy eiendomsreg uit te oefen. In die voorlaaste hoofstuk ontleed ek baie kortliks hoe die verhouding tussen eienaars van grond in mynbougebiede en houers van regte om minerale te ontgin in Sjina, Australië, die Verenigde State van Amerika, Indië, Duitsland en Swaziland gereguleer word. Ter afsluiting word aandag gegee aan moontlike maniere om die belangebotsing tussen die betrokke partye uit die weg te ruim of te beperk. / Private Law / LL. M.