SCALE DEPENDENCE OF EFFECTIVE MATRIX DIFFUSION COEFFICIENT: EFFECTS OF ROCK MATRIX HETEROGENEITY

Because of the dramatic difference between water flow velocities in fractures and rock matrix, matrix diffusion (mass transfer between fractures and the rock matrix through molecular diffusion) can significantly retard solute transport processes in fractured rock, and therefore is important for analyzing a variety of problems, including geological disposal of nuclear waste. Matrix-diffusion-coefficient values measured from small rock samples in the laboratory are generally used for modeling field-scale solute transport in fractured rock. However, by compiling results from a number of field tracer tests corresponding to different geological settings, this study demonstrates that the effective matrix-diffusion coefficient at field scale is generally larger than that at lab scale and tends to increase with testing scale. While several potential mechanisms have been identified, we found that this interesting scale dependence may be related to rock matrix heterogeneity in fractured rock, and there may be a close connection between the scale dependence of permeability and effective matrix diffusion coefficient. Considering that some similarities exist between flow and transport processes in fracture-matrix and aquitard-aquifer systems, our findings for fractured rock may be relevant to modeling these processes in aquitard-aquifer systems.