Table 2 Most common representative values of K for carbonate aquifers and other sedimentary rocks6.

From: Quantitative hydro-geophysical analysis of a complex structural karst aquifer in Eastern Saudi Arabia

Rock type

Hydraulic Conductivity (m/sec)

Karst and reef limestone

1 × 10−6 to 2 × 10−2

Limestone, dolomite

1 × 10−9 to 6 × 10−6

Sandstone

3 × 10−10 to 6 × 10−6

Siltstone

1 × 10−11 to 1.4 × 10−8

Salt

1 × 10−12 to 1 × 10−10

Anhydrite

4 × 10−13 to 2 × 10−8

Shale

1 × 10−13 to 2 × 10−8