Research Article

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

Table 4

Values of the scale parameters and for each field measurement method considered.

Field measurement methods (m) (m3)

Slug tests
 Well no. 1128.10109093
 Piezometers A and B14.1027468

Tracer tests (mean values)51.28363245

Aquifer tests341.3916102895
112.601751775
154.653304321
40.17222939
278.7410734478
69.08659395
216.176456143
380.5320005994
191.845084645
313.2513557392
281.0310911581
195.455277809
316.9013874802
185.904774645
120.101992821