The Scientific World Journal / 2014 / Article / Tab 1

Research Article

Reconsideration at Field Scale of the Relationship between Hydraulic Conductivity and Porosity: The Case of a Sandy Aquifer in South Italy

Table 1

Identification number, depth from the ground level, and screen length of each well and piezometer relative to the confined aquifer of the test field.


Well-top altitude (m a.s.l.)154.76154.78154.74154.68154.77154.53155.00154.85
Depth (m)4040404040575555
Screen length (m)1717171717444444