Research Article

Hydrodynamics in Evaporate-Bearing Fine-Grained Successions Investigated through an Interdisciplinary Approach: A Test Study in Southern Italy—Hydrogeological Behaviour of Heterogeneous Low-Permeability Media

Table 3

Ground elevation of spring and wells versus mean elevation of the recharge area related to the waters collected at the same sites. The latter is calculated from the δ18O vertical gradient experimentally obtained at the test site. All the values are expressed in m asl.

S1P1P2P3P6P7P8P18P27VPS

Elevation489372367367388359363339377349
Calculated mean elevation of the recharge area41435033729732426010695274170