The acquifer
The saturation zone, or rather the phreatic zone, is an accumulation of underground water. Rainwater infiltrates the ground and runs down deep until it finds an impermeable layer that traps it. This is how natural water reservoirs are formed at different depths. Surface groundwater wells are used to collect water from the aquifer closest to the surface (40-50 m underground or even shallower). This water is not for drinking, but it is excellent for irrigating fields and, in general, for agricultural use. Using a surface groundwater well avoids the use of mains water for non-drinking purposes, thus reducing the exploitation of deep aquifers. Deep aquifers (around 100 m deep or even more) are instead a natural reservoir from which water is collected to be then distributed to homes after a series of analyses and checks.
made by CAP Group, forming an efficient network for the territory.
The water journey
Analysis and controls
We provide our customers with packages for testing the quality of their household water with sampling and parameter analysis performed in our laboratories.
Networks and citizens
We pay special attention to our customers and receive many rewards in return. Here are the results of research on a sample of 1352 customers in the territory who were asked about our services.
97,1%
Satisfied with the water service
92,5%
Satisfied with the quality of tap water