Search

Rock permeability, an important factor in subsurface fluid migration, can be influenced by microcracks and chemical weathering due to water–rock interactions. Understanding the relationship between permeability, chemical weathering, and microcracks is crucial for assessing fluid flow in rocks. This study focuses on the hydrogeological characteristics of granite and gneiss, potential host rocks for high-level radioactive waste disposal in South Korea. Samples were analyzed for permeability, porosity, P-wave velocity, and chemical weathering indices. Regression analysis revealed a weak correlation between permeability and both porosity and rock density, while an inverse correlation was observed between permeability and chemical weathering indices. Interestingly, some samples showed low permeability (10−21 to 10−22 m2) despite high weathering, while others showed high permeability (10−18 to 10−19 m2) despite low weathering. SEM-EDS analysis indicated the presence of microcracks within the rocks or the filling of these cracks with secondary minerals. The findings suggest that chemical weathering generally increases pore size and porosity, but actual permeability can vary depending on the presence and connectivity of microcracks and the extent to which they are filled with secondary minerals. Therefore, both chemical weathering and microcrack connectivity must be considered when evaluating the hydrogeological characteristics of crystalline rocks. [ABSTRACT FROM AUTHOR]

• Light reflection visualization was applied to estimate dye concentration in clays. • Relationships between color intensities and dye concentration were established. • Each blue and green channel properly estimated for kaolinite and montmorillonite. • Blue and green channel combined estimation was needed for bentonite clay layer. The image analysis technique approach links the dye concentration and color intensity, enabling quantification of spatial and temporal dye dynamics in clay media. In this study, batch adsorption tests and two-dimensional diffusion experiments with three types of clays (kaolinite, montmorillonite, and bentonite) were conducted for quantifying the vertical distribution of fluorescein dye tracer to evaluate the feasibility of the image analysis technique. In clay domains, color intensities were measured using images obtained during diffusion experiments, and these intensities were converted to aqueous fluorescein concentrations. Concentration profiles simulated from a one-dimensional analytical solution agreed well with those measured by the LRV technique with a single-channel application for kaolinite (blue channel, E B = 0.94 and 0.96) and montmorillonite (green channel, E G = 0.99 and 0.91) in the early (31.1, 54.6 PVs) and later (75.7, 93.9 PVs) diffusion times, respectively. The single-channel application for the bentonite was appropriate for concentration ranges of 0 − 400 mg/L for the blue channel and 400 − 1800 mg/L for the green channel. For quantifying the bentonite concentration profile with a wide range of dye concentrations (0 − 1800 mg/L), multi-channel application (blue + green channels) was required. Measured LRV concentration profiles with the multi-channel application showed better agreement (E B+G = 0.94) with simulated concentration profiles from the analytical solution than those with the single-channel application (E B = 0.56). The results of this study offer guidance on the application of the LRV approach as a non-destructive optical dye measurement method to diffusion problems between high and low permeability zones. [ABSTRACT FROM AUTHOR]