The environment of deposition of the Ohio Shale of the Appalachian Basin has been studied extensively using various geochemical proxies for each of its members. The accumulation of organic matter (OM) and its preservation in the Late Devonian-Early Mississippian black shales of central Kentucky have been studied extensively, especially the possible correlations between trace metal contents and water-column oxygenation. Previous work has centered on geochemical, petrographic, and isotopic analysis of samples collected throughout the central Appalachian Basin. Mechanisms for OM preservation include high productivity, enhanced preservation due to dysoxic or anoxic bottom waters, and a feedback loop due to high productivity that creates enhanced preservation through the periodic cycling and scavenging of essential nutrients. Usually, a combination of these factors results in the accumulation of enough OM to produce these black shales. This research shows the relationships between trace metal data and the environment of deposition of several cores taken along the eastern side of the Cincinnati Arch in the central Appalachian Basin. Whereas the indices do not all agree in every instance across the breadth of the study area, analyzed together a predominant environment of deposition has been inferred for the shales. The Sunbury Shale and upper part of the Cleveland Member of the Ohio Shale were deposited under euxinic conditions, the lower part of the Cleveland Member was likely euxinic in the northern study region and anoxic throughout the central and southern study areas, whereas the Huron Member of the Ohio Shale was deposited under a range of conditions, from oxic, to dysoxic, to anoxic.

The Late Devonian-Early Mississippian-age New Albany Shale is both a source rock and reservoir rock for hydrocarbons in the Illinois Basin. Previously suggested models for organic carbon enrichment consider productivity, anoxia, and the interdependent roles of sedimentation, primary production, and microbial metabolism. This study attempts to reconstruct paleoenvironmental conditions during deposition and re-evaluates these models using geochemical data from multiple cores across the eastern edge of the Illinois Basin in west-central Kentucky. Geochemical methods utilizing redox-sensitive major elements (C, S, Fe, P, K, Ti, and Si), trace elements (V and Mo), and ratios (Ni/Co, V/Cr, and V/(V+Ni) are used. Analysis of paleo-redox indicators suggests variable bottom-water conditions during accumulation of the New Albany Shale members including: anoxic to possibly euxinic conditions for the Clegg Creek Member, anoxic to periodically dysoxic conditions for the Camp Run, and dysoxic to oxic (normal marine) for the Morgan Trail and Blocher Members. Variability in redox proxy results suggests that multiple parameters should be utilized in such studies rather than relying on a single proxy. High C/P ratios observed in these members may be controlled by regeneration of P, enhanced productivity, and sequestration of organic carbon (the productivity-anoxia feedback (PAF) mechanism) under anoxic conditions. The lack of correlation between organic carbon content and clastic-influx proxies suggests that organic matter (OM) accumulation was not controlled by sedimentation rate or increased nutrient supply associated with increased sediment influx.

CO2 emissions from the combustion of fossil fuels have been linked to global climate change. Proposed carbon management technologies include geologic sequestration of CO2. A possible, but untested, sequestration strategy is to inject CO2 into organic-rich shales. Devonian black shales underlie approximately two-thirds of Kentucky and are thicker and deeper in the Illinois and Appalachian Basin portions of Kentucky than in central Kentucky. The Devonian black shales serve as both the source and trap for large quantities of natural gas; total gas in place for the shales in Kentucky is estimated to be between 63 and 112 trillion cubic feet. Most of this natural gas is adsorbed on clay and kerogen surfaces, analogous to methane storage in coal beds. In coals, it has been demonstrated that CO2 is preferentially adsorbed, displacing methane. Black shales may similarly desorb methane in the presence of CO2. The concept that black, organic-rich Devonian shales could serve as a significant geologic sink for CO2 is the subject of current research. To accomplish this investigation, drill cuttings and cores were selected from the Kentucky Geological Survey Well Sample and Core Library. Methane and carbon dioxide adsorption analyses are being performed to determine the gas-storage potential of the shale and to identify shale facies with the most sequestration potential. In addition, sidewall core samples are being acquired to investigate specific black-shale facies, their potential CO2 uptake, and the resulting displacement of methane. Advanced logging techniques (elemental capture spectroscopy) are being investigated for possible correlations between adsorption capacity and geophysical log measurements. For the Devonian shale, average total organic carbon is 3.71 (as received) and mean random vitrinite reflectance is 1.16. Measured adsorption isotherm data range from 37.5 to 2,077.6 standard cubic feet of CO2 per ton (scf/ton) of shale. At 500 psia, adsorption capacity of the Lower Huron Member of the shale is 72 scf/ton. Initial estimates indicate a sequestration capacity of 5.3 billion tons CO2 in the Lower Huron Member of the Ohio shale in parts of eastern Kentucky and as much as 28 billion tons total in the deeper and thicker portions of the Devonian shales in Kentucky. The black shales of Kentucky could be a viable geologic sink for CO2, and their extensive occurrence in Paleozoic basins across North America would make them an attractive regional target for economic CO2 storage and enhanced natural gas production.