Figure 12

K values of the UER aquifer in the study area. The wide range of K is often above or near the anticlinal structures (see wells No. 3, 4 and 8) and can be attributed to permeable zones formed by the karstification process associated with a high density of fractures and joints. ArcGIS 10.3 software is used to create this map, http://www.esri.com.