Opencast coal mining produces trash of soil and rock containing various minerals,that are usually dumped nearby the abandoned sites which causes severe environmental concern including the production of acid mine drain...Opencast coal mining produces trash of soil and rock containing various minerals,that are usually dumped nearby the abandoned sites which causes severe environmental concern including the production of acid mine drainage(AMD)through oxidation pyrite minerals.The current study entailed assessing the potential production of AMD from an opencast coal mining region in Northeast part of India.In order to have a comprehensive overview of the AMD problem in Makum coalfield,the physico-chemical,geochemical,and petrological characteristics of the coal and overburden(OB)samples collected from the Makum coalfield(Northeast India)were thoroughly investigated.The maceral compositions reveal that coal features all three groups of macerals(liptinite,vitrinite,and inertinite),with a high concentration of liptinite indicating the coal of perhydrous,thereby rendering it more reactive.Pyrite(FeS_(2))oxidation kinetics were studied by conducting the aqueous leaching experiments of coal and(OB)samples to interpret the chemical weathering under controlled laboratory conditions of various temperature and time periods,and to replicate the actual mine site leaching.Inductively coupled plasma-optical emission spectroscopy(ICP-OES)was operated to detect the disposal of some precarious elements from coal and OB samples to the leachates during our controlled leaching experiment.The Rare earth element(REE)enrichment in the samples shows the anthropogenic incorporation of the REE in the coal and OB.These experiments reveal the change in conductivity,acid producing tendency,total dissolved solid(TDS),total Iron(Fe)and dissolved Sulfate(SO_(4)^(2−))ions on progress of the leaching experiments.Moreover,the discharge of FeS_(2) via atmospheric oxidation in laboratory condition undergoes a significant growth with the rise of temperature of the reaction systems in the environment and follows pseudo first order kinetics.A bio-remediative strategies is also reported in this paper to mitigate AMD water by employing size-segregated powdered limestone and water hyacinth plant in an indigenously developed site-specific prototype station.Apart from neutralisation of AMD water,this eco-friendly AMD remediation strategy demonstrates a reduction in PHEs concentrations in the treated AMD water.展开更多
The deterioration of environmental conditions is the major contributory factor to poor health and quality of life that hinders sustainable development in any region.Coal mining is one of the major industries that cont...The deterioration of environmental conditions is the major contributory factor to poor health and quality of life that hinders sustainable development in any region.Coal mining is one of the major industries that contribute to the economy of a country but it also impacts the environment.The chemical parameters of the coal,overburden,soil and sediments along with the coal mine drainage(CMD)were investigated in order to understand the overall environmental impact from high sulphur coal mining at northeastern coalfield(India).It was found that the total sulphur content of the coal is noticeably high compared to the overburden(OB)and soil.The volatile matter of the coal is sufficiently high against the high ash content of the soil and overburden.The water samples have a High Electrical Conductivity(EC)and high Total Dissolve Solid(TDS).Lower values of pH,indicate the dissolution of minerals present in the coal as well as other minerals in the mine rejects/overburden.The chemical and nano-mineralogical composition of coal,soil and overburden samples was studied using a High Resolution-Transmission Electron Microscopy(HR-TEM),Energy Dispersive Spectroscopy(EDS),Selected-Area Diffraction(SAED),Field Emission-Scanning Electron Microscopy(FE-SEM)/EDS,X-ray diffraction(XRD),Fourier Transform Infrared Spectroscopy(FTIR),Raman and Ion-Chromatographic analysis,and Mossbauer spectroscopy.From different geochemical analysis it has been found that the mine water sample from Ledo colliery has the lowest pH value of 3.30,Tirap colliery samples have the highest electrical conductivity value of5.40 ms cm^(-1)Both Ledo and Tirap coals have total sulphur contents within the range 3-3.50%.The coal mine water from Tirap colliery(TW-15 B)has high values of Mg^(2+)(450 ppm),and Br^-(227.17 ppm).XRD analysis revealed the presence of minerals including quartz and hematite in the coals.Mineral analysis of coal mine overburden(OB)indicates the presence both of pyrite and marcasite which was also confirmed in XRD and Mossbauer spectral analysis.The presented data of the minerals and ultra/nano-particles present shows their ability to control the mobility of hazardous elements,suggesting possible use in environmental management technology,including restoration of the delicate Indian coal mine areas.展开更多
Coal is the most abundant fossil fuel in the world. Because of the growth of coal mining, coal-fired power plants and coal-burning industries, the increase of the emission of particulates(coarse, fine or ultrafine)is ...Coal is the most abundant fossil fuel in the world. Because of the growth of coal mining, coal-fired power plants and coal-burning industries, the increase of the emission of particulates(coarse, fine or ultrafine)is of great concern. There is a relationship between increasing human morbidity and mortality and progressive environmental air pollution caused by these types of particles. Thus, the knowledge of the physico-chemical composition and ambient concentrations of coal-derived nanoparticles will improve pollution control strategy. Given the current importance of this area of research, the advanced characterization of this coal combustion-derived nanoparticles/nanominerals as well as hazardous elements is likely to be one of the hottest research fields in coming days. In this review, we try to compile the existing knowledge on coal-derived nanoparticles/nanominerals and discuss the advanced level of characterization techniques for future research. This review also provides some of aspects of health risks associated with exposure to ambient nanoparticles. In addition, the presence of some of the hazardous elements in coal and coal combustion activities is also reviewed.展开更多
In this research work,isolation of humic acid from coal of Northeastern region of India is reported.The study is also targeted for application of the coal-derived humic acid in acid mine drainage(AMD)water treatment a...In this research work,isolation of humic acid from coal of Northeastern region of India is reported.The study is also targeted for application of the coal-derived humic acid in acid mine drainage(AMD)water treatment and electrochemical devices.All the obtained results are compared with the standard humic acid and examined the formation of humic acid from the coal.The isolated coal-derived humic acid is found to be high degree of humifications and relatively stable up to about 200℃.The FTIR study indicates the formation of metal-humic acid complexes.On treatment with acidic water(AMD),the coal-derived humic acid was found to have the ability to remove toxic metal such as(in order)Pb>Cu>Zn>Cd.In addition,the preliminary electrochemical properties of the isolated humic acid are also discussed in the paper.The specific capacitance of the isolated coal-derived humic acid via cyclic voltammetry and charge-discharge analysis is found to be 7 mF/g at scan rate 10 mV/s and 22 mF/g within the potential window 0.4 V,respectively.The charge-discharge cycles are stable for more than 1000 cycles within the potential window 0.4 V.This study will create a new pathway for the further research in this field.展开更多
The Cenozoic-age Makum coal from northeastern India offers numerous research opportunities because of its diverse geochemical and geological characteristics.Due to its high sulfur content,the coal has been found to be...The Cenozoic-age Makum coal from northeastern India offers numerous research opportunities because of its diverse geochemical and geological characteristics.Due to its high sulfur content,the coal has been found to be less useful for industrial purposes.It can,however,serve as a hub for ongoing research on coal-based derivative products.The aim of this research work is to investigate the mineralogical and geochemical compositions of the coal,mine overburden(MOB)and shale samples taken from the Makum coal field and also on establishing a mutual relationship between them.To characterize the geochemical controlling factors of the Makum coal field,the study employs coal petrography,FTIR,mineralogical,and geochemical analysis.According to X-ray diffraction analysis,the major minerals like quartz,kaolinite,haematite,illite,pyrite,and calcite are present in coal and MOB.Pyrite is observed by SEM-EDS analysis as cubic-shaped particles that are smaller than a fewμm in size.The presence of sulfide minerals represents a phase of pyrite mineralization.The petrography study was used to better understand the environment that existed during the formation of the plant material,which aids us in determining the quantity of detrital mineral sediment contained in the coal.According to the ICP-MS analysis,the samples indicate significant levels of rare earth elements including yttrium.The present study reveals higher concentrations of poten-tial hazardous elements in the coal samples,with V,Cr,Ni,Cu,and Zn content in coal being considerably enriched compared to world-average concentrations.The correlation analysis reveals that the potential hazardous elements like Co,Ni,As,and Cu are associated with pyrite as they have strong affinity towards pyrite.Thus,numerous minerals and rare earth elements(REEs)exist,opening up a fresh avenue for more research in the area.This study also assists researchers in understanding the significance of Makum coal and provides numerous ideas for coal characterization.展开更多
The petrology of coal,as determined by the microscopic analysis of organic and inorganic elemental constituents of coal,provides information on its nature and characteristics.Coal is used worldwide in the production o...The petrology of coal,as determined by the microscopic analysis of organic and inorganic elemental constituents of coal,provides information on its nature and characteristics.Coal is used worldwide in the production of thermal energy and coke.In the case of high-quality Colombian coals,only limited studies have been carried out.The present study presents the geochemical,mineralogical,and petrological characteristics of coal samples collected from Puerto Drummond in Cienaga,Colombia,to predict their potential uses.Therefore,the ultimate,proximate,petrographic,gross calorific value(GCV),ash fusion temperature,Fourier transform infrared spectroscopy(FTIR),X-ray diffraction(XRD),X-ray fluorescence(XRF),and Thermogravimetric(TG)analyses were employed in this study.The petrological analysis reveals that Colombian coals are naturally more abundant in vitrinite(72%)than inertinite(14e23%)macerals.Silicates and aluminosilicate are the main minerals present as fine particles mixed with macerals.The XRD and FTIR analyses show that the most common and dominant minerals are quartz,while gypsum,hematite,calcite and mica occur in lesser amounts.The oxide composition of the coal ashes consists of 51e58%SiO2 and 18e25%Al2O3 as determined by XRF analysis.In correlation and regression analysis,the moisture content shows a reverse correlation with GCV(Regression value of R2¼0.68).This study helps researchers to comprehend the importance of Colombian coals and presents various techniques for characterisation of coals.展开更多
Extracting gas from unconventional shale reservoirs with low permeability is challenging.To overcome this,hydraulic fracturing(HF)is employed.Despite enhancing shale gas production,HF has drawbacks like groundwater po...Extracting gas from unconventional shale reservoirs with low permeability is challenging.To overcome this,hydraulic fracturing(HF)is employed.Despite enhancing shale gas production,HF has drawbacks like groundwater pollution and induced earthquakes.Such issues highlight the need for ongoing exploration of novel shale gas extraction methods such as in situ heating through combustion or pyrolysis to mitigate operational and environmental concerns.In this study,thermally immature shales of contrasting organic richness from Rajmahal Basin of India were heated to different temperatures(pyrolysis at 350,500 and 650℃)to assess the temperature protocols necessary for hydrocarbon liberation and investigate the evolution of pore structural facets with implications for CO_(2) sequestration in underground thermally treated shale horizons.Our results from low-pressure N_(2) adsorption reveal reduced adsorption capacity in the shale splits treated at 350 and 500 C,which can be attributed to structural reworking of the organic matter within the samples leading to formation of complex pore structures that limits the access of nitrogen at low experimental temperatures.Consequently,for both the studied samples BET SSA decreased by~58%and 72%at 350℃,and~67%and 68%at 500℃,whereas average pore diameter increased by~45%and 91%at 350℃,and~100%and 94%at 500℃ compared to their untreated counterparts.CO_(2) adsorption results,unlike N_(2),revealed a pronounced rise in micropore properties(surface area and volume)at 500 and 650℃(~30%-35%and~41%63%,respectively for both samples),contradicting the N_(2) adsorption outcomes.Scanning electron microscope(SEM)images complemented the findings,showing pore structures evolving from microcracks to collapsed pores with increasing thermal treatment.Analysis of the SEM images of both samples revealed a notable increase in average pore width(short axis):by~4 and 10 times at 350℃,~5 and 12 times at 500℃,and~10 and 28 times at 650℃ compared to the untreated samples.Rock-Eval analysis demonstrated the liberation of almost all pyrolyzable kerogen components in the shales heated to 650℃.Additionally,the maximum micropore capacity,identified from CO_(2) gas adsorption analysis,indicated 650℃ as the ideal temperature for in situ conversion and CO_(2) sequestration.Nevertheless,project viability hinges on assessing other relevant aspects of shale gas development such as geomechanical stability and supercritical CO_(2) interactions in addition to thermal treatment.展开更多
In coal mining areas,the ambient atmospheric and aqueous oxidation of pyrite minerals(FeS2)associated with coal as well as the other accompanying strata is significant in understanding the extent of acid mine drainage...In coal mining areas,the ambient atmospheric and aqueous oxidation of pyrite minerals(FeS2)associated with coal as well as the other accompanying strata is significant in understanding the extent of acid mine drainage(AMD),the cause of severe environmental pollution.Therefore,in this paper,the oxidation kinetics of the coal-associated pyrite(CAPy)present in a coal sample(TpHM1)has been studied via aqueous leaching depyritization experiments at variety of temperatures and time intervals without the incorporation of any oxidizer.The outcomes obtained are juxtaposed with the standard pyrite mineral(SPM)oxidation at the same experimental conditions.Also,the coal and SPM slurry residues and filtrates obtained after aqueous leaching at 25℃ and 90℃ for 0 h and 24 h,respectively,were extensively analyzed through high-resolution transmission electron microscopy(HR-TEM),Powder X-ray diffraction(P-XRD),and X-ray-photoelectron spectroscopy(XPS)for evaluation of the mineralogical composition and proportions of iron and sulfur components during progression of the oxidation reaction.Both the reactions obey pseudo first-order kinetics during pyrite(FeS_(2))oxidation but a significant difference in the experimentally found activation energies(E_(a))and rate constants(k)values of oxidation kinetics of both CAPy and SPM may be attributed to the varied geochemical compositions of the coal associated pyrite(CAPy).The rate constant for CAPy is much greater than that of SPM implying a higher Ea around 10.838 kJ/mol for SPM as compared to 1.941 kJ/mol for CAPy.The CAPy in coal(TpHM1)is more susceptible to atmospheric oxidation than that of SPM,leading to the formation of acid mine drainage with lower pH.In this paper,the pH values on the basis of stoichiometric pyrite oxidation reaction were calculated and compared with the pH values obtained after aqueous leaching of CAPy to interpret the extent of acid formation and pyrite dissolution.Hence,with the assistance of the current study,further studies on the effects of mineral impurities,whereabouts of pyrite minerals in coal seams,the significance of compositional differences in the CAPy,the effect of metal oxides,and the role of alkalinity producing neutralizing agents of coal in the oxidative dissolution process of pyrite can be investigated.展开更多
文摘Opencast coal mining produces trash of soil and rock containing various minerals,that are usually dumped nearby the abandoned sites which causes severe environmental concern including the production of acid mine drainage(AMD)through oxidation pyrite minerals.The current study entailed assessing the potential production of AMD from an opencast coal mining region in Northeast part of India.In order to have a comprehensive overview of the AMD problem in Makum coalfield,the physico-chemical,geochemical,and petrological characteristics of the coal and overburden(OB)samples collected from the Makum coalfield(Northeast India)were thoroughly investigated.The maceral compositions reveal that coal features all three groups of macerals(liptinite,vitrinite,and inertinite),with a high concentration of liptinite indicating the coal of perhydrous,thereby rendering it more reactive.Pyrite(FeS_(2))oxidation kinetics were studied by conducting the aqueous leaching experiments of coal and(OB)samples to interpret the chemical weathering under controlled laboratory conditions of various temperature and time periods,and to replicate the actual mine site leaching.Inductively coupled plasma-optical emission spectroscopy(ICP-OES)was operated to detect the disposal of some precarious elements from coal and OB samples to the leachates during our controlled leaching experiment.The Rare earth element(REE)enrichment in the samples shows the anthropogenic incorporation of the REE in the coal and OB.These experiments reveal the change in conductivity,acid producing tendency,total dissolved solid(TDS),total Iron(Fe)and dissolved Sulfate(SO_(4)^(2−))ions on progress of the leaching experiments.Moreover,the discharge of FeS_(2) via atmospheric oxidation in laboratory condition undergoes a significant growth with the rise of temperature of the reaction systems in the environment and follows pseudo first order kinetics.A bio-remediative strategies is also reported in this paper to mitigate AMD water by employing size-segregated powdered limestone and water hyacinth plant in an indigenously developed site-specific prototype station.Apart from neutralisation of AMD water,this eco-friendly AMD remediation strategy demonstrates a reduction in PHEs concentrations in the treated AMD water.
基金The financial assistance from CSIR,New Delhi(MLP6000-WP-Ⅲ)
文摘The deterioration of environmental conditions is the major contributory factor to poor health and quality of life that hinders sustainable development in any region.Coal mining is one of the major industries that contribute to the economy of a country but it also impacts the environment.The chemical parameters of the coal,overburden,soil and sediments along with the coal mine drainage(CMD)were investigated in order to understand the overall environmental impact from high sulphur coal mining at northeastern coalfield(India).It was found that the total sulphur content of the coal is noticeably high compared to the overburden(OB)and soil.The volatile matter of the coal is sufficiently high against the high ash content of the soil and overburden.The water samples have a High Electrical Conductivity(EC)and high Total Dissolve Solid(TDS).Lower values of pH,indicate the dissolution of minerals present in the coal as well as other minerals in the mine rejects/overburden.The chemical and nano-mineralogical composition of coal,soil and overburden samples was studied using a High Resolution-Transmission Electron Microscopy(HR-TEM),Energy Dispersive Spectroscopy(EDS),Selected-Area Diffraction(SAED),Field Emission-Scanning Electron Microscopy(FE-SEM)/EDS,X-ray diffraction(XRD),Fourier Transform Infrared Spectroscopy(FTIR),Raman and Ion-Chromatographic analysis,and Mossbauer spectroscopy.From different geochemical analysis it has been found that the mine water sample from Ledo colliery has the lowest pH value of 3.30,Tirap colliery samples have the highest electrical conductivity value of5.40 ms cm^(-1)Both Ledo and Tirap coals have total sulphur contents within the range 3-3.50%.The coal mine water from Tirap colliery(TW-15 B)has high values of Mg^(2+)(450 ppm),and Br^-(227.17 ppm).XRD analysis revealed the presence of minerals including quartz and hematite in the coals.Mineral analysis of coal mine overburden(OB)indicates the presence both of pyrite and marcasite which was also confirmed in XRD and Mossbauer spectral analysis.The presented data of the minerals and ultra/nano-particles present shows their ability to control the mobility of hazardous elements,suggesting possible use in environmental management technology,including restoration of the delicate Indian coal mine areas.
基金partial financial assistance of Ministry of Environment Forest and Climate Change (MoEFCC), Govt. of India (GPP-0325)
文摘Coal is the most abundant fossil fuel in the world. Because of the growth of coal mining, coal-fired power plants and coal-burning industries, the increase of the emission of particulates(coarse, fine or ultrafine)is of great concern. There is a relationship between increasing human morbidity and mortality and progressive environmental air pollution caused by these types of particles. Thus, the knowledge of the physico-chemical composition and ambient concentrations of coal-derived nanoparticles will improve pollution control strategy. Given the current importance of this area of research, the advanced characterization of this coal combustion-derived nanoparticles/nanominerals as well as hazardous elements is likely to be one of the hottest research fields in coming days. In this review, we try to compile the existing knowledge on coal-derived nanoparticles/nanominerals and discuss the advanced level of characterization techniques for future research. This review also provides some of aspects of health risks associated with exposure to ambient nanoparticles. In addition, the presence of some of the hazardous elements in coal and coal combustion activities is also reviewed.
基金Authors are very much thankful to the Director of CSIR-NEIST,Jorhat for encouragement and CSIR,New Delhi for financial support(OLP-2031)to carry out the work.The authors are also very much thankful to Dr.Ponchami Sharma for her assistance during the samples collections and analysis and Dr.Jugal Bori for assistance in electron beam analysis of the samples.Authors express thanks to Dr.Jim Hower for his comments and English corrections.
文摘In this research work,isolation of humic acid from coal of Northeastern region of India is reported.The study is also targeted for application of the coal-derived humic acid in acid mine drainage(AMD)water treatment and electrochemical devices.All the obtained results are compared with the standard humic acid and examined the formation of humic acid from the coal.The isolated coal-derived humic acid is found to be high degree of humifications and relatively stable up to about 200℃.The FTIR study indicates the formation of metal-humic acid complexes.On treatment with acidic water(AMD),the coal-derived humic acid was found to have the ability to remove toxic metal such as(in order)Pb>Cu>Zn>Cd.In addition,the preliminary electrochemical properties of the isolated humic acid are also discussed in the paper.The specific capacitance of the isolated coal-derived humic acid via cyclic voltammetry and charge-discharge analysis is found to be 7 mF/g at scan rate 10 mV/s and 22 mF/g within the potential window 0.4 V,respectively.The charge-discharge cycles are stable for more than 1000 cycles within the potential window 0.4 V.This study will create a new pathway for the further research in this field.
基金MoES (Govt of India)for his financial assistance to our project (GPP364).
文摘The Cenozoic-age Makum coal from northeastern India offers numerous research opportunities because of its diverse geochemical and geological characteristics.Due to its high sulfur content,the coal has been found to be less useful for industrial purposes.It can,however,serve as a hub for ongoing research on coal-based derivative products.The aim of this research work is to investigate the mineralogical and geochemical compositions of the coal,mine overburden(MOB)and shale samples taken from the Makum coal field and also on establishing a mutual relationship between them.To characterize the geochemical controlling factors of the Makum coal field,the study employs coal petrography,FTIR,mineralogical,and geochemical analysis.According to X-ray diffraction analysis,the major minerals like quartz,kaolinite,haematite,illite,pyrite,and calcite are present in coal and MOB.Pyrite is observed by SEM-EDS analysis as cubic-shaped particles that are smaller than a fewμm in size.The presence of sulfide minerals represents a phase of pyrite mineralization.The petrography study was used to better understand the environment that existed during the formation of the plant material,which aids us in determining the quantity of detrital mineral sediment contained in the coal.According to the ICP-MS analysis,the samples indicate significant levels of rare earth elements including yttrium.The present study reveals higher concentrations of poten-tial hazardous elements in the coal samples,with V,Cr,Ni,Cu,and Zn content in coal being considerably enriched compared to world-average concentrations.The correlation analysis reveals that the potential hazardous elements like Co,Ni,As,and Cu are associated with pyrite as they have strong affinity towards pyrite.Thus,numerous minerals and rare earth elements(REEs)exist,opening up a fresh avenue for more research in the area.This study also assists researchers in understanding the significance of Makum coal and provides numerous ideas for coal characterization.
文摘The petrology of coal,as determined by the microscopic analysis of organic and inorganic elemental constituents of coal,provides information on its nature and characteristics.Coal is used worldwide in the production of thermal energy and coke.In the case of high-quality Colombian coals,only limited studies have been carried out.The present study presents the geochemical,mineralogical,and petrological characteristics of coal samples collected from Puerto Drummond in Cienaga,Colombia,to predict their potential uses.Therefore,the ultimate,proximate,petrographic,gross calorific value(GCV),ash fusion temperature,Fourier transform infrared spectroscopy(FTIR),X-ray diffraction(XRD),X-ray fluorescence(XRF),and Thermogravimetric(TG)analyses were employed in this study.The petrological analysis reveals that Colombian coals are naturally more abundant in vitrinite(72%)than inertinite(14e23%)macerals.Silicates and aluminosilicate are the main minerals present as fine particles mixed with macerals.The XRD and FTIR analyses show that the most common and dominant minerals are quartz,while gypsum,hematite,calcite and mica occur in lesser amounts.The oxide composition of the coal ashes consists of 51e58%SiO2 and 18e25%Al2O3 as determined by XRF analysis.In correlation and regression analysis,the moisture content shows a reverse correlation with GCV(Regression value of R2¼0.68).This study helps researchers to comprehend the importance of Colombian coals and presents various techniques for characterisation of coals.
文摘Extracting gas from unconventional shale reservoirs with low permeability is challenging.To overcome this,hydraulic fracturing(HF)is employed.Despite enhancing shale gas production,HF has drawbacks like groundwater pollution and induced earthquakes.Such issues highlight the need for ongoing exploration of novel shale gas extraction methods such as in situ heating through combustion or pyrolysis to mitigate operational and environmental concerns.In this study,thermally immature shales of contrasting organic richness from Rajmahal Basin of India were heated to different temperatures(pyrolysis at 350,500 and 650℃)to assess the temperature protocols necessary for hydrocarbon liberation and investigate the evolution of pore structural facets with implications for CO_(2) sequestration in underground thermally treated shale horizons.Our results from low-pressure N_(2) adsorption reveal reduced adsorption capacity in the shale splits treated at 350 and 500 C,which can be attributed to structural reworking of the organic matter within the samples leading to formation of complex pore structures that limits the access of nitrogen at low experimental temperatures.Consequently,for both the studied samples BET SSA decreased by~58%and 72%at 350℃,and~67%and 68%at 500℃,whereas average pore diameter increased by~45%and 91%at 350℃,and~100%and 94%at 500℃ compared to their untreated counterparts.CO_(2) adsorption results,unlike N_(2),revealed a pronounced rise in micropore properties(surface area and volume)at 500 and 650℃(~30%-35%and~41%63%,respectively for both samples),contradicting the N_(2) adsorption outcomes.Scanning electron microscope(SEM)images complemented the findings,showing pore structures evolving from microcracks to collapsed pores with increasing thermal treatment.Analysis of the SEM images of both samples revealed a notable increase in average pore width(short axis):by~4 and 10 times at 350℃,~5 and 12 times at 500℃,and~10 and 28 times at 650℃ compared to the untreated samples.Rock-Eval analysis demonstrated the liberation of almost all pyrolyzable kerogen components in the shales heated to 650℃.Additionally,the maximum micropore capacity,identified from CO_(2) gas adsorption analysis,indicated 650℃ as the ideal temperature for in situ conversion and CO_(2) sequestration.Nevertheless,project viability hinges on assessing other relevant aspects of shale gas development such as geomechanical stability and supercritical CO_(2) interactions in addition to thermal treatment.
基金Ministry of Earth Science(Govt.of India)(GPP-0364).
文摘In coal mining areas,the ambient atmospheric and aqueous oxidation of pyrite minerals(FeS2)associated with coal as well as the other accompanying strata is significant in understanding the extent of acid mine drainage(AMD),the cause of severe environmental pollution.Therefore,in this paper,the oxidation kinetics of the coal-associated pyrite(CAPy)present in a coal sample(TpHM1)has been studied via aqueous leaching depyritization experiments at variety of temperatures and time intervals without the incorporation of any oxidizer.The outcomes obtained are juxtaposed with the standard pyrite mineral(SPM)oxidation at the same experimental conditions.Also,the coal and SPM slurry residues and filtrates obtained after aqueous leaching at 25℃ and 90℃ for 0 h and 24 h,respectively,were extensively analyzed through high-resolution transmission electron microscopy(HR-TEM),Powder X-ray diffraction(P-XRD),and X-ray-photoelectron spectroscopy(XPS)for evaluation of the mineralogical composition and proportions of iron and sulfur components during progression of the oxidation reaction.Both the reactions obey pseudo first-order kinetics during pyrite(FeS_(2))oxidation but a significant difference in the experimentally found activation energies(E_(a))and rate constants(k)values of oxidation kinetics of both CAPy and SPM may be attributed to the varied geochemical compositions of the coal associated pyrite(CAPy).The rate constant for CAPy is much greater than that of SPM implying a higher Ea around 10.838 kJ/mol for SPM as compared to 1.941 kJ/mol for CAPy.The CAPy in coal(TpHM1)is more susceptible to atmospheric oxidation than that of SPM,leading to the formation of acid mine drainage with lower pH.In this paper,the pH values on the basis of stoichiometric pyrite oxidation reaction were calculated and compared with the pH values obtained after aqueous leaching of CAPy to interpret the extent of acid formation and pyrite dissolution.Hence,with the assistance of the current study,further studies on the effects of mineral impurities,whereabouts of pyrite minerals in coal seams,the significance of compositional differences in the CAPy,the effect of metal oxides,and the role of alkalinity producing neutralizing agents of coal in the oxidative dissolution process of pyrite can be investigated.
