Coal tar, a dense nonaqueous phase liquid (NAPL), is a common subsurface contaminant at sites of former manufactured gas plants. A proposed remediation technology is water-miscible solvent extraction, which requires understanding of the effect of water-miscible solvents on the solubility of coal tar. This study investigated this effect and the extent to which multicomponent coal tar could be represented as a pseudocomponent in thermodynamic modeling. The coal tar used in this study showed a predominance of polycyclic aromatic hydrocarbons with no single compound accounting for more than 4% (wt). The bulk solubility of coal tar in water was estimated to be 16 mg/L using composition data and Raoult's law assumption for aqueous solubility. For three solvents, n-butylamine, acetone, and 2-propanol, equilibrium phase compositions of two-phase coal tar/solvent/water mixtures were experimentally determined using radiolabeled materials and are presented as ternary phase diagrams. Results showed n-butylamine to be a good water-miscible solvent for coal tar dissolution. The validity of thermodynamic modeling of coal tar as a pseudocomponent was explored by examining the liquid-liquid solute partitioning of naphthalene, phenanthrene and pyrene and by assessing the effect of solvent extraction on coal tar phase composition. It was found that coal tar partitions as a pseudocomponent in systems with appreciable solvent, but not in systems with only coal tar and water.
Geochemical reactions may alter the permeability of leakage pathways in caprocks, which serve a critical role in confining CO 2 in geologic carbon sequestration. A caprock specimen from a carbonate formation in the Michigan sedimentary Basin was fractured and studied in a high-pressure core flow experiment. Inflowing brine was saturated with CO 2 at 40°C and 10 MPa, resulting in an initial pH of 4.6, and had a calcite saturation index of -0.8. Fracture permeability decreased during the experiment, but subsequent analyses did not reveal calcite precipitation. Instead, experimental observations indicate that calcite dissolution along the fracture pathway led to mobilization of less soluble mineral particles that clogged the flow path. Analyses of core sections via electron microscopy, synchrotron-based X-ray diffraction imaging, and the first application of microbeam Ca K-edge X-ray absorption near edge structure, provided evidence that these occlusions were fragments from the host rock rather than secondary precipitates. X-ray computed tomography showed a significant loss of rock mass within preferential flow paths, suggesting that dissolution also removed critical asperities and caused mechanical closure of the fracture. The decrease in fracture permeability despite a net removal of material along the fracture pathway demonstrates a nonintuitive, inverse relationship between dissolution and permeability evolution in a fractured carbonate caprock.
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