Transmissibility varies continuously as a point-function in the Culebra, so every point in a model can be defined. |
The REV* concept does not apply to discontinuous media whose extreme conduits have never been measured nor defined in space. |
The pilot-point method used in PA to create a T-field is mathematically, practically, invalid, and it leads to unconservative transport results. |
Rustler salt beds present elsewhere were never deposited beneath the LWA west of the repository, thus clays and channel fills are syndepositional with the Rustler. |
Dissolution removed the salt beds, leaving residual clays and breccia, and initiated subsidence fractures subsequently opened by dissolution. |
Residual clays onsite imply ongoing karst formation at sites upgradient, i. e., to the east. Open dissolution channels in the Rustler, undetected by the few bore holes, are likely W of the repository below the water table, and more commonly, above the water table. Explorations may establish the degree of karst development, but without sufficient detail for modeling. |
Transport of radionuclides may be calculated according to a continuous Culebra matrix with horizontal fractures, so diffusion and absorption are significant processes. |
A superimposed karst system of large channels carrying brines bypasses the matrix and fractures, so specific surface is small. |
Because the majority of the discharge flows rapidly and episodically via karst tubes, far less retardation occurs. |
Wetter climatic conditions will raise the water table essentially to the surface, increasing velocities modestly via the Culebra only. |
Greater recharge during pluvial periods will be accommodated by modest increases in water table elevation, saturating more karst conduits. |
An increasing proportion of the recharge will flow via karst channels, decreasing average travel times appreciably. |