ORCID Profile
0000-0002-2980-1798
Current Organisation
University of Queensland
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Research Topics
In Research Link Australia (RLA), "Research Topics" refer to ANZSRC FOR and SEO codes. These topics are either sourced from ANZSRC FOR and SEO codes listed in researchers' related grants or generated by a large language model (LLM) based on their publications.
Top 5 Research Topics
ANZSRC Field of Research (FoR)
Geochronology And Isotope Geochemistry | Geochemistry | Chemical Engineering | Petroleum and Reservoir Engineering | Geology | Chemical Engineering Not Elsewhere Classified | Climatology (Incl. Palaeoclimatology) | Surfacewater Hydrology | Petroleum And Reservoir Engineering | Petroleum and Coal Geology | Geochronology | Engineering And Technology Not Elsewhere Classified | Environmental Science and Management | Powder and Particle Technology | Soil Chemistry | Environmental Technologies | Environmental Management And Rehabilitation | Archaeological Science | Geotectonics | Ore Deposit Petrology | Genomics | Geomechanics | Environmental Engineering not elsewhere classified | Chemical Engineering not elsewhere classified | Resources Engineering and Extractive Metallurgy | Interdisciplinary Engineering Not Elsewhere Classified | Geology Not Elsewhere Classified |
ANZSRC Socio-Economic Objective (SEO)
Earth sciences | Oil and Gas Extraction | Coal | Oil and gas | Climate change | Renewable Energy not elsewhere classified | Renewable energy | Land and water management | Scientific instrumentation | Climate variability | Primary mining and extraction processes | Geothermal Energy Extraction | Exploration | Other
Related Links
Publications
K–Ar and Rb–Sr dating of authigenic illite–smectite in Late Permian coal measures, Queensland, Australia: implication for thermal history
Publisher: Elsevier BV
Date: 2001
Thermal Evolution of the Ore-Hosting Isa Superbasin: Central and Northern Lawn Hill Platform
Publisher: Society of Economic Geologists
Date: 09-2006
Introduction
Publisher: Springer Netherlands
Date: 29-07-2010
Microbial remains in some earliest Earth rocks: Comparison with a potential modern analogue
Publisher: Elsevier BV
Date: 30-07-2008
Palaeoenvironment and palaeoclimate during the late Carboniferous-early Permian in northern China from carbon and nitrogen isotopes of coals
Publisher: Elsevier BV
Date: 02-2020
Earliest Seafloor Hydrothermal Systems on Earth: Comparison with Modern Analogues
Publisher: Springer Netherlands
Date: 29-07-2010
Relationships between Devonian volcanic and plutonic units in the Mt Morgan Area, central Queensland
Publisher: Informa UK Limited
Date: 02-1996
Reply to ‘‘Comment on: ‘K–Ar evidence from illitic clays of a Late Devonian age for the 120 km diameter Woodleigh impact structure, Southern Carnarvon Basin, Western Australia’’
Publisher: Elsevier BV
Date: 07-2002
Sm-Nd dating and rare-earth element tracing of calcite: Implications for fluid-flow events in the Bowen Basin, Australia
Publisher: Elsevier BV
Date: 03-2007
Chemical and mineralogical characterisation of illite–smectite: Implications for episodic tectonism and associated fluid flow, central Australia
Publisher: Elsevier BV
Date: 2015
Occurrence and Palaeohydrological Significance of Authigenic Kaolinite in the Aldebaran Sandstone, Denison Trough, Queensland, Australia
Publisher: Springer Science and Business Media LLC
Date: 1992
Recognition of a widespread Paleoproterozoic hydrothermal system in the southern McArthur Basin, northern Australia, by in-situ analysis of fine-grained pyrite and spatially-associated solid bitumen in the Lamont Pass palaeohigh
Publisher: Elsevier BV
Date: 05-2022
Metals, energy and sustainability: The story of Doctor Copper and King Coal
Publisher: Springer International Publishing
Date: 2017
Formation of fault-related calcite precipitates and their implications for dating fault activity in the east Anatolian and dead sea fault zones
Publisher: Geological Society of London
Date: 2011
DOI: 10.1144/SP359.13
Sources and concentrations of methane, ethane, and CO2 in deep aquifers of the Surat Basin, Great Artesian Basin
Publisher: Elsevier BV
Date: 2023
The effect of coal rank on biogenic methane potential and microbial composition
Publisher: Elsevier BV
Date: 2016
Evidence for an Early-Middle Jurassic fluid event constrained by Sm–Nd, Sr isotopes, rare earth elements and yttrium in the Bowen Basin, Australia
Publisher: Elsevier BV
Date: 05-2020
Reservoir lithofacies study of the Toolebuc Formation, Eromanga Basin, Australia as a potential unconventional target
Publisher: Elsevier BV
Date: 2023
Integrating <sup>40</sup>Ar-<sup>39</sup>Ar, <sup>87</sup>Rb-<sup>87</sup>Sr and <sup>147</sup>Sm-<sup>143</sup>Nd geochronology of authigenic illite to evaluate tectonic reactivation in an intraplate setting, central Australia
Publisher: Elsevier BV
Date: 06-2014
Geochemistry of storing CO2 and NOx in the deep Precipice Sandstone
Publisher: Informa UK Limited
Date: 12-2018
Geochronological (U–Pb, U–Th–total Pb, Sm–Nd) and geochemical (REE, 87Sr/86Sr, δ18O, δ13C) tracing of intraplate tectonism and associated fluid flow in the Warburton Basin, Australia
Publisher: Springer Science and Business Media LLC
Date: 09-2014
A possible early age for a diprotodon (Marsupialia: Diprotodontidae) fossil from the Papua New Guinea highlands
Publisher: Informa UK Limited
Date: 06-2008
Mobilisation of elements from coal due to batch reactor experiments with CO2 and water at 40 degrees C and 9.5 MPa
Publisher: Elsevier BV
Date: 02-2015
Impure CO2 reaction of feldspar, clay, and organic matter rich cap-rocks: Decreases in the fraction of accessible mesopores measured by SANS
Publisher: Elsevier BV
Date: 2018
A fluid inclusion and stable isotope study of the Moonta copper–gold deposits, South Australia: evidence for fluid immiscibility in a magmatic hydrothermal system
Publisher: Elsevier BV
Date: 12-2002
A Basin System and Fluid-Flow Analysis of the Zn-Pb-Ag Mount Isa-Type Deposits of Northern Australia: Identifying Metal Source, Basinal Brine Reservoirs, Times of Fluid Expulsion, and Organic Matter R
Publisher: Society of Economic Geologists
Date: 09-2006
Pore-Scale Numerical Investigation on Chemical Stimulation in Coal and Permeability Enhancement for Coal Seam Gas Production
Publisher: Springer Science and Business Media LLC
Date: 04-10-2016
Accessory phases from the Soultz monzogranite, Soultz-sous-Forêts, France: Implications for titanite destabilisation and differential REE, Y and Th mobility in hydrothermal systems
Publisher: Elsevier BV
Date: 2013
Carbon and hydrogen isotope fractionation during methanogenesis: A laboratory study using coal and formation water
Publisher: Elsevier BV
Date: 05-2016
Trace element mobility during CO2storage: application of reactive transport modelling
Publisher: EDP Sciences
Date: 2019
DOI: 10.1051/E3SCONF/20199804007
Abstract: The geologic storage of CO 2 carries both physical and chemical risks to the environment. In order to reduce those risks, it is necessary to provide predictive capabilities for impacts so that strategies can be developed to monitor, identify and mitigate potential problems. One area of concern is related to water quality both in the reservoir and in overlying aquifers. In this study we report the critical steps required to develop chemically constrained reactive transport models (RTM) that can be used to address risk assessment associated with water quality. The data required to produce the RTM includes identifying the in idual hydrostratigraphic units and defining the mineral and chemical composition to sufficient detail for the modelling. This includes detailed mineralogy, bulk chemical composition, reactive mineral phase chemical composition and the identification of the occurrence and mechanisms of mobilisation of any trace elements of interest. Once the required detail is achieved the next step involves conducting experiments to determine the evolution of water chemistry as reaction proceeds preferably under varying elevated CO 2 fugacities with and without impurities. Geochemical modelling of the experiments is then used for characterising the reaction pathways of the different hydrostratigraphic units. The resultant geochemical model inputs can then be used to develop the chemical components of a reactive transport model.
Reply to Comment of Smith and Pallasser on “Factors controlling the origin of gas in Australian Bowen Basin coals”
Publisher: Elsevier BV
Date: 2001
Isotopic and hydrogeochemical evidence for biogenic gas in Cuervos Formation coal beds, Cesar Rancheria Basin, Colombia
Publisher: Elsevier BV
Date: 2022
The Ban Houayxai epithermal Au–Ag deposit in the Northern Lao PDR: Mineralization related to the Early Permian arc magmatism of the Truong Son Fold Belt
Publisher: Elsevier BV
Date: 07-2014
Mineralogical controls on porosity and water chemistry during O 2 -SO 2 -CO 2 reaction of CO 2 storage reservoir and cap-rock core
Publisher: Elsevier BV
Date: 12-2016
Sedimentologic, petrographic, and sulfur isotope constraints on fine-grained pyrite formation at Mount Isa Mine and environs, Northwest Queensland, Australia
Publisher: Society of Economic Geologists
Date: 09-1999
Characterisation of bioavailability of Surat Basin Walloon coals for biogenic methane production using environmental microbial consortia
Publisher: Elsevier BV
Date: 06-2017
Methane metabolism in the archaeal phylum Bathyarchaeota revealed by genome-centric metagenomics
Publisher: American Association for the Advancement of Science (AAAS)
Date: 23-10-2015
Abstract: The production and consumption of methane by microorganisms play a major role in the global carbon cycle. Although these processes can occur in a range of environments, from animal guts to the deep ocean, these metabolisms are confined to the Archaea. Evans et al. used metagenomics to assemble two nearly complete archaeal genomes from deep groundwater methanogens (see the Perspective by Lloyd). The two reconstructed genomes are members of the recently described Bathyarchaeota and not the phylum to which all previously known methane-metabolizing archaea belonged. Science , this issue p. 434 , see also p. 384
Integration of Observational and Analytical Methodologies to Characterize Organic Matter in Early Archaean Rocks: Distinguishing Biological from Abiotically Synthesized Carbonaceous Matter Structures
Publisher: Springer Netherlands
Date: 29-07-2010
Seawater oxygenation during the Paleocene-Eocene Thermal Maximum
Publisher: Geological Society of America
Date: 23-05-2012
DOI: 10.1130/G32977.1
Carbon Storage Potential of North American Oil & Gas Produced Water Injection with Surface Dissolution
Publisher: MDPI AG
Date: 08-03-2021
DOI: 10.3390/GEOSCIENCES11030123
Abstract: Carbon dioxide (CO2) geological storage traditionally involves capturing a CO2 stream from a point source such as a power station or from cement, steel, or natural gas processing plant, transporting it and compressing it, prior to injection as a supercritical phase into a suitable geological reservoir overlain by a cap-rock or seal. One of the main perceived risks in CO2 geological storage is migration or leakage of the buoyant CO2 stream through the seal, via faults or fractures, or other migration out of the storage complex. Injection of CO2 dissolved in water may be one solution to mitigate the leakage risk. This approach could take advantage of large volumes of wastewater already being reinjected into saline aquifers worldwide but particularly in North America, thus reducing costs. This study examines the potential to “piggyback” off the existing wastewater injection industry as a novel carbon storage option.
Changes in reservoir properties from injection of supercritical CO2 into coal seams — A laboratory study
Publisher: Elsevier BV
Date: 06-2010
Estimation of body water compartments in cirrhosis by multiple-frequency bioelectrical-impedance analysis
Publisher: Elsevier BV
Date: 2001
DOI: 10.1016/S0899-9007(00)00473-1
Abstract: Estimation of total body water by measuring bioelectrical impedance at a fixed frequency of 50 kHz is useful in assessing body composition in healthy populations. However, in cirrhosis, the distribution of total body water between the extracellular and intracellular compartments is of greater clinical importance. We report an evaluation of a new multiple-frequency bioelectrical-impedance analysis technique (MFBIA) that may quantify the distribution of total body water in cirrhosis. In 21 cirrhotic patients and 21 healthy control subjects, impedance to the flow of current was measured at frequencies ranging from 4 to 1012 kHz. These measurements were used to estimate body water compartments and then compared with total body water and extracellular water determined by isotope methodology. In cirrhotic patients, extracellular water and total body water (as determined by isotope methods) were well predicted by MFBIA (r = 0.73 and 0.89, respectively). However, the 95% confidence intervals of the limits of agreement between MFBIA and the isotope methods were +/-14% and +/-9% for cirrhotics (extracellular water and total body water, respectively) and +/-9% and +/-9% for cirrhotics without ascites. The 95% confidence intervals estimated from the control group were +/-10% and +/-5% for extracellular water and total body water, respectively. Thus, despite strong correlations between MFBIA and isotope measurements, the relatively large limits of agreement with accepted techniques suggest that the MFBIA technique requires further refinement before it can be routinely used to determine the nutritional assessment of in idual cirrhotic patients.
Body composition in nonalcoholic cirrhosis: The effect of disease etiology and severity on nutritional compartments
Publisher: Elsevier BV
Date: 06-1994
DOI: 10.1016/0016-5085(94)90418-9
Abstract: Previous studies of body composition in cirrhosis have either measured only one body compartment, used alcoholic subjects, or not corrected body composition for physical characteristics. The aim of this study was to perform a detailed analysis of body composition in subjects with nonalcoholic cirrhosis. Simultaneous measurements of total body potassium and total body water were performed and values of body cell mass and body fat were corrected for physical characteristics. Child's class C patients had a significantly lower mean total body potassium index (i.e., percent observed value/expected value) and body fat index than class A or B patients. Eighty-one percent of class C patients had simultaneous reductions in body fat and body cell mass, and 71% of patients with class A disease had a significant reduction in either or both compartments. Nine patients showed the pattern of tissue loss seen with short-term starvation. Fourteen patients showed the pattern of tissue loss seen in physiological stress. Severe liver disease is characterized by significant reductions in body fat and body cell mass, most class A patients have a significant reduction in some nutritional compartments, and the pattern of tissue loss may reflect mechanisms of tissue wasting.
Metal Mobilization From CO2 Storage Cap-Rocks: Experimental Reactions With Pure CO2 or CO2 SO2 NO
Publisher: Frontiers Media SA
Date: 14-07-2022
DOI: 10.3389/FENRG.2022.873813
Abstract: CO 2 geological storage will be needed as part of the transition to lower greenhouse gas emissions. During CO 2 storage, the mobilization of metals from minerals to formation water via CO 2 water rock reactions may be a concern for water quality. The sources, behavior, and fate of metals, however, are not well understood. Metals in minerals of calcite cemented sandstone, feldspar-rich sandstone, and ironstone seal drill cores from a target storage site were characterized. The cores were reacted with low-salinity water and pure supercritical CO 2 or impure CO 2 with SO 2 and nitric oxide (NO), under reservoir conditions. Calcite cemented core underwent calcite dissolution with chlorite, plagioclase, and sulfide alteration. The highest concentrations of calcium and manganese were released in the reaction of calcite cemented sandstone seal, with the lowest mobilized arsenic concentration. Pure CO 2 reaction of the feldspar-rich sandstone seal resulted in calcite dissolution, with plagioclase, chlorite, kaolinite, illite, and sulfides corroded. Impure CO 2 reaction of the feldspar-rich sandstone led to additional corrosion of apatite, pyrite, and sphalerite cements. Generally, dissolved iron, lead, zinc, and arsenic were released and then re-precipitated in oxide minerals or adsorbed. Calcium, manganese, and strontium were released primarily from calcite cement dissolution. Plagioclase corrosion was a second source of dissolved strontium, and chlorite dissolution a second source of manganese. Although sulfides contained higher concentrations of metals, the higher reactivity of carbonates meant that the latter were the main sources contributing to dissolved metal concentrations. The mineral content of the seal cores, and the injected gas mixture, had an impact on the type and concentration of metals released. The ubiquitous presence of carbonate minerals means that this study is applicable to understanding the potential risk factors for water quality changes, and the mobilization and fate of environmentally regulated metals, in both CO 2 storage complexes and overlying drinking water aquifers worldwide.
A Review on Recent Advances in the Numerical Simulation for Coalbed-Methane-Recovery Process
Publisher: Society of Petroleum Engineers (SPE)
Date: 20-12-2007
DOI: 10.2118/93101-PA
Abstract: The recent advances in numerical simulation for primary coalbed methane (CBM) recovery and enhanced coalbed-methane recovery (ECBMR) processes are reviewed, primarily focusing on the progress that has occurred since the late 1980s. Two major issues regarding the numerical modeling will be discussed in this review: first, multicomponent gas transport in in-situ bulk coal and, second, changes of coal properties during methane (CH4) production. For the former issues, a detailed review of more recent advances in modeling gas and water transport within a coal matrix is presented. Further, various factors influencing gas diffusion through the coal matrix will be highlighted as well, such as pore structure, concentration and pressure, and water effects. An ongoing bottleneck for evaluating total mass transport rate is developing a reasonable representation of multiscale pore space that considers coal type and rank. Moreover, few efforts have been concerned with modeling water-flow behavior in the coal matrix and its effects on CH4 production and on the exchange of carbon dioxide (CO2) and CH4. As for the second issue, theoretical coupled fluid-flow and geomechanical models have been proposed to describe the evolution of pore structure during CH4 production, instead of traditional empirical equations. However, there is currently no effective coupled model for engineering applications. Finally, perspectives on developing suitable simulation models for CBM production and for predicting CO2-sequestration ECBMR are suggested.
Factors controlling the origin of gas in Australian Bowen Basin coals
Publisher: Elsevier BV
Date: 1998
Coal seam gas distribution and hydrodynamics of the Sydney Basin, NSW, Australia
Publisher: Informa UK Limited
Date: 03-04-2014
Earliest Life on Earth: Habitats, Environments and Methods of Detection
Publisher: Springer Netherlands
Date: 2011
Horizontal stress anisotropy and effective stress as regulator of coal seam gas zonation in the Sydney Basin, Australia
Publisher: Elsevier BV
Date: 10-2014
Timing and mechanism of late-Pleistocene calcite vein formation across the Dead Sea Fault Zone, northern Israel
Publisher: Elsevier BV
Date: 03-2012
Melange- and sediment-hosted gold-bearing quartz veins, Hodgkinson gold field, Queensland, Australia
Publisher: Society of Economic Geologists
Date: 04-1990
Hydrothermal control on organic matter alteration and illite precipitation, Mt Isa Basin, Australia
Publisher: Wiley
Date: 02-04-2004
Stable isotope geochemistry of coal bed and shale gas and related production waters: A review
Publisher: Elsevier BV
Date: 12-2013
Hydrochemistry, mineralogy and sulfur isotope geochemistry of acid mine drainage at the Mt. Morgan mine environment, Queensland, Australia
Publisher: Elsevier BV
Date: 04-2005
Gene flow of the canker pathogen Botryosphaeria australis between Eucalyptus globulus plantations and native eucalypt forests in Western Australia
Publisher: Wiley
Date: 20-07-2006
Geochemical and stable isotope studies of the No. 4 lode, Kalgoorlie, Western Australia
Publisher: Society of Economic Geologists
Date: 05-1983
Biogenic methane production from Bowen Basin coal waste materials
Publisher: Elsevier BV
Date: 2017
Professor Allan Fraser Wilson, 1921–2001
Publisher: Mineralogical Society
Date: 04-2002
The effect of bituminous coal on methanogenic mixed cultures and pure cultures of Methanococcus and Methanosarcina
Publisher: Elsevier BV
Date: 10-2017
Kinetics of the Dehydroxylation of Serpentine
Publisher: American Chemical Society (ACS)
Date: 11-01-2012
DOI: 10.1021/EF201360B
New evidence of magmatic-fluid–related phyllic alteration: Implications for the genesis of porphyry Cu deposits
Publisher: Geological Society of America
Date: 2002
Controls on Gas Domains and Production Behaviour in A High-Rank CSG Reservoir: Insights from Molecular and Isotopic Chemistry of Co-Produced Waters and Gases from the Bowen Basin, Australia
Publisher: MDPI AG
Date: 18-02-2020
DOI: 10.3390/GEOSCIENCES10020074
Abstract: This paper uses hydrochemical and multi-isotope analysis to investigate geological controls on coal seam gas (CSG) saturation domains and gas well production performance in a high-rank (vitrinite reflectance (Rv) 1.1) CSG field in the north-western Bowen Basin, Australia. New hydrochemical and stable isotope data were combined with existing geochemical datasets to refine hypotheses on the distribution and origins of CSG in two highly compartmentalized Permian coal seams. Stable isotopic results suggest that geographic variations in gas content, saturation and production reflect the extent of secondary microbial gas generation and retention as a function of hydrodynamics. δ13C and δ2H data support a gas mixing hypothesis with δ13C-CH4 increasing from secondary biogenic values to thermogenic values at depth (δ13C −62.2‰ to −46.3‰), whereas correlated methane and carbon dioxide carbon isotope compositions, Δ13C(CO2–CH4) values and δ13CDIC/alkalinity trends are largely consistent with microbial CO2 reduction. In addition, below 200 m, the majority of δ13C-CO2 values are positive (δ13C: −1.2‰ to 7.1‰) and δ13CDIC shows an erratic increase with depth for both seams that is characteristic of evolution via microbial activity. The progression of carbon isotope values along the CO2 reduction fractionation line suggests progressive depletion of the CO2 reservoir with increasing depth. Faults clearly segment coal seams into areas having significantly different production, with results of geochemical analysis suggesting that pooling of biogenic gas and waters and enhanced methanogenesis occur north of a faulted hinge zone.
Geochemistry of Archean shoshonitic lamprophyres from the Yilgarn Block, Western Australia: Au abundance and association with gold mineralization
Publisher: Elsevier BV
Date: 03-1994
Parallel Lattice Boltzmann Computing and Applications in Core Sample Feature Evaluation
Publisher: Springer Science and Business Media LLC
Date: 27-11-2014
Cooper Basin REM gas shales after CO2 storage or acid reactions: Metal mobilisation and methane accessible pore changes
Publisher: Elsevier BV
Date: 05-2023
Use of temperature logs in coal seam gas reservoirs: Application to the Sydney Basin, Australia
Publisher: Elsevier BV
Date: 04-2015
Erratum to: Earliest Life on Earth: Habitats, Environments and Methods of Detection
Publisher: Springer Netherlands
Date: 2011
Melange- and sediment-hosted gold-bearing quartz veins, Hodgkinson gold field, Queensland, Australia; reply
Publisher: Society of Economic Geologists
Date: 02-1991
CO2 degassing and trapping during hydrothermal cycles related to Gondwana rifting in eastern Australia
Publisher: Elsevier BV
Date: 10-2011
History of geochronology in Queensland
Publisher: Informa UK Limited
Date: 08-2008
Quartz veining in simply folded arenites, Cape Liptrap, southeast Victoria, Australia
Publisher: Informa UK Limited
Date: 06-1989
Geological interpretation of gas content trends, Walloon Subgroup, eastern Surat Basin, Queensland, Australia
Publisher: Elsevier BV
Date: 11-2012
Improving coal bioavailability for biogenic methane production via hydrogen peroxide oxidation
Publisher: Elsevier BV
Date: 07-2018
U-Th dating of striated fault planes
Publisher: Geological Society of America
Date: 07-2012
DOI: 10.1130/G32970.1
Bajo de la Alumbrera Copper-Gold Deposit: Stable Isotope Evidence for a Porphyry-Related Hydrothermal System Dominated by Magmatic Aqueous Fluids
Publisher: Society of Economic Geologists
Date: 08-2005
Towards an understanding of the age and origin of mesothermal gold mineralisation in the Etheridge Goldfield, Georgetown region, north Queensland
Publisher: Informa UK Limited
Date: 04-1998
Predicted CO2 water rock reactions in naturally altered CO2 storage reservoir sandstones, with interbedded cemented and coaly mudstone seals
Publisher: Elsevier BV
Date: 03-2022
A strontium (87Sr/86Sr) isotopic study on the chemical evolution and migration of groundwaters in a low-rank coal seam gas reservoir (Surat Basin, Australia)
Publisher: Elsevier BV
Date: 02-2019
U-series dating and geochemical tracing of late Quaternary travertine in co-seismic fissures
Publisher: Elsevier BV
Date: 30-05-2007
The stable isotope signature of kilometre‐scale fracturedominated metamorphic fluid pathways, Mary Kathleen, Australia
Publisher: Wiley
Date: 09-1993
Multiple sulfur isotope constraints on microbial processes in Archaean seafloor environments
Publisher: Elsevier BV
Date: 08-2006
Conceptual exploration targeting for microbially enhanced coal bed methane (MECoM) in the Walloon Subgroup, eastern Surat Basin, Australia
Publisher: Elsevier BV
Date: 2015
The influence of hydrogeological disturbance and mining on coal seam microbial communities
Publisher: Wiley
Date: 06-11-2016
DOI: 10.1111/GBI.12166
Abstract: The microbial communities present in two underground coal mines in the Bowen Basin, Queensland, Australia, were investigated to deduce the effect of pumping and mining on subsurface methanogens and methanotrophs. The micro-organisms in pumped water from the actively mined areas, as well as, pre- and post-mining formation waters were analyzed using 16S rRNA gene licon sequencing. The methane stable isotope composition of Bowen Basin coal seam indicates that methanogenesis has occurred in the geological past. More recently at the mine site, changing groundwater flow dynamics and the introduction of oxygen in the subsurface has increased microbial biomass and ersity. Consistent with microbial communities found in other coal seam environments, pumped coal mine waters from the subsurface were dominated by bacteria belonging to the genera Pseudomonas and the family Rhodocyclaceae. These environments and bacterial communities supported a methanogen population, including Methanobacteriaceae, Methanococcaceae and Methanosaeta. However, one of the most ubiquitous micro-organisms in anoxic coal mine waters belonged to the family 'Candidatus Methanoperedenaceae'. As the Archaeal family 'Candidatus Methanoperedenaceae' has not been extensively defined, the one studied species in the family is capable of anaerobic methane oxidation coupled to nitrate reduction. This introduces the possibility that a methane cycle between archaeal methanogenesis and methanotrophy may exist in the anoxic waters of the coal seam after hydrogeological disturbance.
Temporal changes in microbial community composition during culture enrichment experiments with Indonesian coals
Publisher: Elsevier BV
Date: 2015
Carbon isotopic evidence for rapid methane clathrate release recorded in coals at the terminus of the Late Palaeozoic Ice Age
Publisher: Springer Science and Business Media LLC
Date: 12-11-2019
DOI: 10.1038/S41598-019-52863-6
Abstract: The end of the Late Palaeozoic Ice Age (LPIA) ushered in a period of significant change in Earth’s carbon cycle, demonstrated by the widespread occurrence of coals worldwide. In this study, we present stratigraphically constrained organic stable carbon isotope (δ 13 C org ) data for Early Permian coals (312 vitrain s les) from the Moatize Basin, Mozambique, which record the transition from global icehouse to greenhouse conditions. These coals exhibit a three-stage evolution in atmospheric δ 13 C from the Artinskian to the Kungurian. Early Kungurian coals effectively record the presence of the short-lived Kungurian Carbon Isotopic Excursion (KCIE), associated with the proposed rapid release of methane clathrates during deglaciation at the terminus of the Late Palaeozoic Ice Age (LPIA), with no observed disruption to peat-forming and terrestrial plant communities. δ 13 C org variations in coals from the Moatize Basin are cyclic in nature on the order of 10 3 –10 5 years and reflect changes in δ 13 C org of ~±1‰ during periods of stable peat accumulation, supporting observations from Palaeozoic coals elsewhere. These cyclic variations express palaeoenvironmental factors constraining peat growth and deposition, associated with changes in base level. This study also demonstrates the effectiveness of vitrain in coal as a geochemical tool for recording global atmospheric change during the Late Palaeozoic.
Modeling gas displacement kinetics in coal with Maxwell-Stefan diffusion theory
Publisher: Wiley
Date: 29-10-2007
DOI: 10.1002/AIC.11314
Distribution of body water in patients with cirrhosis: The effect of liver transplantation
Publisher: Ovid Technologies (Wolters Kluwer Health)
Date: 06-1993
Seismic cycles recorded in late Quaternary calcite veins: Geochronological, geochemical and microstructural evidence
Publisher: Elsevier BV
Date: 02-2011
Biogenic Methane Cycling in a Laboratory Model of an Abandoned Bituminous Coal Mine
Publisher: Informa UK Limited
Date: 15-02-2018
Petrographic and isotope constraints on the origin of authigenic carbonate minerals and the associated fluid evolution in Late Permian coal measures, Bowen Basin (Queensland), Australia
Publisher: Elsevier BV
Date: 11-2000
Geochemical mass-balance and oxygen-isotope constraints on silcrete formation and its paleoclimatic implications in southern Australia
Publisher: Society for Sedimentary Geology
Date: 09-1998
DOI: 10.2110/JSR.68.981
Importance of mineral sequestration during CO2 gas migration: A case study from the Greater Gorgon area
Publisher: Elsevier BV
Date: 2011
Clay-Mineral Authigenesis in the Late Permian Coal Measures, Bowen Basin, Queensland, Australia
Publisher: Springer Science and Business Media LLC
Date: 2000
Geochemistry of apatite in Late Permian coals, Bowen Basin, Australia
Publisher: Elsevier BV
Date: 03-2021
Zinc Deposits and Related Mineralization of the Burketown Mineral Field, Including the World-Class Century Deposit, Northern Australia: Fluid Inclusion and Stable Isotope Evidence for Basin Fluid Sour
Publisher: Society of Economic Geologists
Date: 09-2006
K—Ar dating of the Anakie Metamorphic Group: Evidence for an extension of the Delamerian Orogeny into central Queensland
Publisher: Informa UK Limited
Date: 10-1996
Long term reactivity of CO2 in a low salinity reservoir-seal complex
Publisher: Elsevier BV
Date: 03-2020
Petrologic and stable isotopic study of the Walloon Coal Measures, Surat Basin, Queensland: peat accumulation under changing climate and base level
Publisher: Elsevier BV
Date: 04-2016
Methane in aquifers and alluvium overlying a coal seam gas region: Gas concentrations and isotopic differentiation
Publisher: Elsevier BV
Date: 02-2023
Woodleigh, Southern Carnarvon Basin, Western Australia: history of discovery, Late Devonian age, and geophysical and morphometric evidence for a 120 km-diameter impact structure
Publisher: Informa UK Limited
Date: 09-2005
Geological storage of CO2 and acid gases dissolved at surface in production water
Publisher: Elsevier BV
Date: 03-2022
Genome-centric analysis of microbial populations enriched by hydraulic fracture fluid additives in a coal bed methane production well
Publisher: Frontiers Media SA
Date: 08-06-2016
Direct Rubidium-Strontium Dating of Hydrocarbon Charge Using Small Authigenic Illitic Clay Aliquots from the Silurian Bituminous Sandstone in the Tarim Basin, NW China
Publisher: Springer Science and Business Media LLC
Date: 29-08-2019
DOI: 10.1038/S41598-019-48988-3
Abstract: Illitic clay is ubiquitous in clastic hydrocarbon reservoirs, and the host for several radiometric isotopes such as the potassium-argon (K-Ar) and rubidium-strontium (Rb-Sr) systems. This study applied the isotope-dilution thermal ionization mass spectrometry technique for small s les (3–4 mg) to conduct illite Rb-Sr isotope dating of five illitic clay s les from the Silurian bituminous sandstone (SBS) intersected by five drillholes in the Tarim Basin, NW China. The 87 Rb/ 86 Sr ratio of clays is fractionated mainly by the addition of Rb during the illitization of mixed-layer illite/smectite (I/S), which is the dominant clay species in the Tarim Basin s les. The subs le-scale Rb/Sr isotope values suggest that each subs le may contain I/S particles of slightly variable degrees of illitization. Three of the analyzed s les (H6, KQ1 and TZ67) generated Rb-Sr isochron ages of 141 ± 61 Ma, 332 ± 32 Ma and 235 ± 8 Ma (errors quoted at 2σ), respectively. These results are similar to the corresponding K-Ar ages (125 Ma, 389 Ma and 234 Ma). The isotopic ages are consistent with the timing of hydrocarbon charge which varies in different drillholes as constrained by basin modelling, indicating that a closed-system behavior is attained by the hydrocarbon charge that inhibits the illitization of I/S. The Rb-Sr isotope analyses of the other two s les (YM35-1 and Q1) that did not yield isochron ages suggest the conditions for producing isochrons were not satisfied, which may be caused by disturbance of the isotope system by a post-charge hydrothermal event. The outcomes of this study show the robust potential of Rb-Sr clay subs le geochronology for cross-checking isotopic ages yielded by other systems (e.g. K-Ar system) and constraining the timing of hydrocarbon charge.
Microbial controls on the origin and evolution of coal seam gases and production waters of the Walloon Subgroup; Surat Basin, Australia
Publisher: Elsevier BV
Date: 08-2015
Mineralogical characterisation of a potential reservoir system for CO2 sequestration in the Surat Basin
Publisher: Informa UK Limited
Date: 02-2013
Asia Pacific Coalbed Methane Symposium—Selected papers from the 2008 Brisbane symposium on coalbed methane CO2-enhanced coalbed methane
Publisher: Elsevier BV
Date: 06-2010
Experimental acid and scCO2 reactions of Roseneath, Epsilon and Murteree gas shales: Opening or closing of gas accessible pores and metal release to water
Publisher: Informa UK Limited
Date: 11-11-2019
Clay mineralogical, geochemical and isotopic tracing of the evolution of the Woodleigh impact structure, Southern Carnarvon Basin, Western Australia
Publisher: Springer Science and Business Media LLC
Date: 04-11-2005
Reactivity of micas and cap-rock in wet supercritical CO2 with SO2 and O2 at CO2 storage conditions
Publisher: Elsevier BV
Date: 09-2016
Carbon dioxide-rich coals of the Oaky Creek area, central Bowen Basin: a natural analogue for carbon sequestration in coal systems
Publisher: Informa UK Limited
Date: 29-01-2013
Multimillion year thermal history of a porphyry copper deposit: application of U-Pb, Ar-40/Ar-39 and (U-Th)/He chronometers, Bajo de la Alumbrera copper-gold deposit, Argentina
Publisher: Springer Science and Business Media LLC
Date: 16-08-2008
Pyrite paragenesis and multiple sulfur isotope distribution in late Archean and early Paleoproterozoic Hamersley Basin sediments
Publisher: Elsevier BV
Date: 07-2008
Deformation and regional carbonate metasomatism of turbidite-hosted Cretaceous alkaline lamprophyres (northwestern Papua New Guinea)
Publisher: Elsevier BV
Date: 07-1988
Understanding mine site water and salt dynamics to support integrated water quality and quantity management
Publisher: Informa UK Limited
Date: 09-2009
Stable isotopic composition of coal bed gas and associated formation water samples from Raniganj Basin, West Bengal, India
Publisher: Elsevier BV
Date: 04-2018
Geochemical influences on methanogenic groundwater from a low rank coal seam gas reservoir: Walloon Subgroup, Surat Basin
Publisher: Elsevier BV
Date: 11-2011
CO2 sequestration in coals and enhanced coalbed methane recovery: New numerical approach
Publisher: Elsevier BV
Date: 05-2010
Geochemical Mass-Balance and Oxygen-Isotope Constraints on Silcrete Formation and Its Paleoclimatic Implications in Southern Australia
Publisher: Society for Sedimentary Geology
Date: 1998
Interaction of Dissolved CO2, SOx and NOx with the Moolayember Formation Underlying the Precipice Sandstone
Publisher: Elsevier BV
Date: 2019
DOI: 10.2139/SSRN.3366101
Criteria for the recognition of metamorphosed or altered lamprophyres: A case study from the Archaean of Kambalda, Western Australia
Publisher: Elsevier BV
Date: 05-1989
Reactive transport LBM model for CO2 injection in fractured reservoirs
Publisher: Elsevier BV
Date: 2016
Experimental mineral dissolution in Berea Sandstone reacted with CO2 or SO2-CO2 in NaCl brine under CO2 sequestration conditions
Publisher: Elsevier BV
Date: 04-2015
A fresh approach to investigating CO2 storage: Experimental CO2-water-rock interactions in a low-salinity reservoir system
Publisher: Elsevier BV
Date: 04-2015
Reactive transport in porous media for CO 2 sequestration: Pore scale modeling using the lattice Boltzmann method
Publisher: Elsevier BV
Date: 2017
High salinity fluid inclusions in the Yinshan polymetallic deposit from the Le–De metallogenic belt in Jiangxi Province, China: Their origin and implications for ore genesis
Publisher: Elsevier BV
Date: 04-2007
Atmospheric S and lithospheric Pb in sulphides from the 2.06 Ga Phalaborwa phoscorite-carbonatite Complex, South Africa
Publisher: Elsevier BV
Date: 2020
Stable isotopic and molecular composition of desorbed coal seam gases from the Walloon Subgroup, eastern Surat Basin, Australia
Publisher: Elsevier BV
Date: 02-2014
Microbial Methane Potential for the South Sumatra Basin Coal: Formation Water Screening and Coal Substrate Bioavailability
Publisher: Elsevier BV
Date: 2015
Timing and Chemistry of Fluid-Flow Events in the Lawn Hill Platform, Northern Australia
Publisher: Society of Economic Geologists
Date: 09-2006
CO2 and NOx reactions with CO2 storage reservoir core: NOx dissolution products and mineral reactions
Publisher: Elsevier BV
Date: 10-2022
Biogenic methane potential for Surat Basin, Queensland coal seams
Publisher: Elsevier BV
Date: 11-2011
Numerical simulation of multicomponent gas diffusion and flow in coals for CO2 enhanced coalbed methane recovery
Publisher: Elsevier BV
Date: 08-2007
Hydrothermal CO2 degassing in seismically active zones during the late Quaternary
Publisher: Elsevier BV
Date: 07-2009
Could hot fluids be the cause of natural pyrolysis at the ragged edge of Herrin coal, Millport 7 ½’ quadrangle, Hopkins County, Kentucky?
Publisher: Elsevier BV
Date: 11-2020
Parameterizing Geochemical Models: Do Kinetics of Calcite Matter?
Publisher: Elsevier BV
Date: 2017
Micro CT and Experimental Study of Carbonate Precipitation from CO2 and Produced Water Co-Injection into Sandstone
Publisher: MDPI AG
Date: 26-10-2021
DOI: 10.3390/EN14216998
Abstract: Carbon dioxide geological storage involves injecting captured CO2 streams into a suitable reservoir. Subsequent mineral trapping of the CO2 as carbonate minerals is one of the most secure forms of trapping. Injection of CO2 dissolved in water or co-injection of CO2 with water may enhance trapping mechanisms. Produced waters are already re-injected into reservoirs worldwide, and their co-injection with CO2 could enhance mineral trapping in low reactivity rock by providing a source of cations. Sandstone drill core from a reservoir proposed for CO2 storage was experimentally reacted with supercritical CO2 and a synthetic produced water. Micro computed tomography (CT), QEMSCAN, and SEM were performed before and after the reaction. The sandstone s le was predominantly quartz with minor illite/muscovite and kaolinite. The sandstone sub-plug micro-CT porosity was 11.1% and 11.4% after the reaction. Dissolved Ca, Mg, and Sr decreased during the reaction. After the reaction with CO2 and synthetic produced water, precipitation of crystalline carbonate minerals calcite and dolomite was observed in the pore space and on the rock surface. In addition, the movement of pore filling and bridging clays, as well as grains was observed. Co-injection of CO2 with produced waters into suitable reservoirs has the potential to encourage CO2 mineral trapping.
A combined geochemical and μCT study on the CO2 reactivity of Surat Basin reservoir and cap-rock cores: Porosity changes, mineral dissolution and fines migration
Publisher: Elsevier BV
Date: 2019
Clay mineralogical, geochemical and isotopic tracing of the evolution of the Woodleigh impact structure, Southern Carnarvon Basin, Western Australia
Publisher: Springer Science and Business Media LLC
Date: 19-05-2005
Microbial remains and other carbonaceous forms from the 3.24Ga Sulphur Springs black smoker deposit, Western Australia
Publisher: Elsevier BV
Date: 04-2007
In situ techniques for classifying apatite in coal
Publisher: Elsevier BV
Date: 10-2020
Distribution of body water in patients with cirrhosis: The effect of liver transplantation,
Publisher: Elsevier BV
Date: 06-1993
Simultaneous determination of δ33SV‐CDT and δ34SV‐CDT using masses 48, 49 and 50 on a continuous flow isotope ratio mass spectrometer
Publisher: Wiley
Date: 21-10-2004
DOI: 10.1002/RCM.1681
Abstract: A new, fast, continuous flow technique is described for the simultaneous determination of delta33S and delta34S using SO masses 48, 49 and 50. Analysis time is approximately 5 min/s le with measurement precision and accuracy better than +/-0.3 per thousand. This technique, which has been set up using IAEA Ag2S standards S-1, S-2 and S-3, allows for the fast determination of mass-dependent or mass-independent fractionation (MIF) effects in sulfide, organic sulfur s les and possibly sulfate. Small s le sizes can be analysed directly, without chemical pre-treatment. Robustness of the technique for natural versus artificial standards was demonstrated by analysis of a Canon Diablo troilite, which gave a delta33S of 0.04 per thousand and a delta34S of -0.06 per thousand compared to the values obtained for S-1 of 0.07 per thousand and -0.20 per thousand, respectively. Two pyrite s les from a banded-iron formation from the 3710 Ma Isua Greenstone Belt were analysed using this technique and yielded MIF (Delta33S of 2.45 and 3.31 per thousand) comparable to pyrite previously analysed by secondary ion probe.
Geochemical modelling of experimental O2 –SO2 –CO2 reactions of reservoir, cap-rock, and overlying cores
Publisher: Elsevier BV
Date: 10-2019
Different mineralization styles in a volcanic-hosted ore deposit: the fluid and isotopic signatures of the Mt Morgan Au–Cu deposit, Australia
Publisher: Elsevier BV
Date: 2003
5th International Symposium on Applied Isotope Geochemistry
Publisher: Elsevier BV
Date: 04-2005
The Pretty Hill Formation as a natural analogue for CO2 storage: An investigation of mineralogical and isotopic changes associated with sandstones exposed to low, intermediate and high CO2 concentrati
Publisher: Elsevier BV
Date: 04-2015
Methodology to determine the extent of anaerobic digestion, composting and CH4 oxidation in a landfill environment
Publisher: Elsevier BV
Date: 06-2018
DOI: 10.1016/J.WASMAN.2018.02.029
Abstract: An examination of the processes contributing to the production of landfill greenhouse gas (GHG) emissions is required, as the actual level to which waste degrades anaerobically and aerobically beneath covers has not been differentiated. This paper presents a methodology to distinguish between the rate of anaerobic digestion (r
Occurrence of minerals within fractures and matrix of selected Bowen and Ruhr Basin coals
Publisher: Elsevier BV
Date: 05-2012
Archaean carbon reservoirs and their relevance to the fluid source for gold deposits
Publisher: Springer Science and Business Media LLC
Date: 1988
DOI: 10.1038/331254A0
Experimental and modelled reactions of CO2 and SO2 with core from a low salinity aquifer overlying a target CO2 storage complex
Publisher: MDPI AG
Date: 12-12-2019
DOI: 10.3390/GEOSCIENCES9120513
Abstract: CO2-induced reactions in low salinity aquifers overlying CO2 storage sites are of interest to understand potential reactions or impacts in the possible case of a leak. Previous investigations of overlying aquifers in the context of CO2 storage have focused on pure CO2 streams, however captured industrial CO2 streams may contain ancillary gases, including SO2, O2, NOx, H2S, N2, etc., some of which may be more reactive than CO2 when dissolved in formation water. Eight drill cores from two wells in a low salinity sandstone aquifer that overlies a target CO2 storage complex are characterised for porosity (helium, mercury injection, or micro CT), permeability, and mineral content. The eight Hutton Sandstone cores are variable with porosities of 5.2–19.6%, including carbonaceous mudstones, calcite cemented sandstones, and quartz rich sandstones, common lithologies that may be found generally in overlying aquifers of CO2 storage sites. A chlorite rich sandstone was experimentally reacted with CO2 and low concentrations of SO2 to investigate the potential reactions and possible mineral trapping in the unlikely event of a leak. Micro CT characterisation before and after the reaction indicated no significant change in porosity, although some fines movement was observed that could affect permeability. Dissolved concentrations of Fe, Ca, Mn, Cr, Mg, Rb, Li, Zn, etc., increased during the reaction, including from dissolution of chlorite and trace amounts of ankerite. After ~40 days dissolved concentrations including Fe, Zn, Al, Ba, As and Cr decreased. Chlorite was corroded, and Fe-rich precipitates mainly Fe-Cr oxides were observed to be precipitated on rock surfaces after experimental reaction. Concentrations of Rb and Li increased steadily and deserve further investigation as potential monitoring indicators for a leak. The reaction of chlorite rich sandstone with CO2 and SO2 was geochemically modelled over 10 years, with mainly chlorite alteration to siderite mineral trapping 1.55 kg/m3 of CO2 and removing dissolved Fe from solution. Kaolinite and chalcedony precipitation was also predicted, with minor pyrite precipitation trapping SO2, however no changes to porosity were predicted.
Experimental supercritical CO2 and water interactions with coal under simulated in situ conditions
Publisher: Elsevier BV
Date: 2011
Microchemistry and microstructures of hydrothermally altered shock-metamorphosed basement gneiss, Woodleigh impact structure, Southern Carnarvon Basin, Western Australia
Publisher: Informa UK Limited
Date: 09-2005
Stable isotope and water quality analysis of coal bed methane production waters and gases from the Bowen Basin, Australia
Publisher: Elsevier BV
Date: 06-2010
Modeling anisotropic permeability of coal and its effects on CO2 sequestration and enhanced coalbed methane recovery
Publisher: Elsevier BV
Date: 12-2015
Clay mineralogical and isotopic (K–Ar, δ18O, δD) constraints on the evolution of the North Anatolian Fault Zone, Turkey
Publisher: Elsevier BV
Date: 15-03-2006
K–Ar evidence from illitic clays of a Late Devonian age for the 120 km diameter Woodleigh impact structure, Southern Carnarvon Basin, Western Australia
Publisher: Elsevier BV
Date: 10-2001
SO2–CO2 and pure CO2 reactivity of ferroan carbonates at carbon storage conditions
Publisher: Elsevier BV
Date: 09-2015
Adsorption and mineral trapping dominate CO2 storage in coal systems
Publisher: Elsevier BV
Date: 2011
Rare earth element fractionation in authigenic illite–smectite from Late Permian clastic rocks, Bowen Basin, Australia: implications for physico-chemical environments of fluids during illitization
Publisher: Elsevier BV
Date: 02-2003
The thermal history of the Bowen Basin, Queensland, Australia: vitrinite reflectance and clay mineralogy of Late Permian coal measures
Publisher: Elsevier BV
Date: 08-2000
Impure CO2 storage reactions of sandstone, mudstone and carbonate cemented cores: Experimental CO2 SO2 NOX O2 reaction metal mobilisation and fate
Publisher: Elsevier BV
Date: 09-2023
SO2 impurity impacts on experimental and simulated CO2 -water-reservoir rock reactions at carbon storage conditions
Publisher: Elsevier BV
Date: 04-2015
Preliminary investigation of biogenic gas production in Indonesian low rank coals and implications for a renewable energy source
Publisher: Elsevier BV
Date: 11-2013
Stable isotope geochemistry of authigenic clay minerals from Late Permian coal measures, Queensland, Australia: implications for the evolution of the Bowen Basin
Publisher: Elsevier BV
Date: 07-2000
Contrasting alteration assemblages in metabasites from Mount Isa, Queensland; implications for copper ore genesis
Publisher: Society of Economic Geologists
Date: 08-1993
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