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.

	Wells						Piezometers
Number	1	3	5	7	9	11	A	B
Well-top altitude (m a.s.l.)	154.76	154.78	154.74	154.68	154.77	154.53	155.00	154.85
Depth (m)	40	40	40	40	40	57	55	55
Screen length (m)	17	17	17	17	17	44	44	44