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  1. Rock Mass

    Linked via "Fracture Flow Multiplier ($F_m$)"

    Transmissivity and Hydraulic Conductivity ($K_{mass}$)
    The hydraulic conductivity of the rock mass ($K{mass}$) is typically orders of magnitude greater than that of the intact rock matrix ($K{intact}$). This difference is quantified by the Fracture Flow Multiplier ($F_m$):
    $$K{mass} = K{intact} \times F_m$$