Ongoing hydrogeological investigations in the Grosseto Province (southern Tuscany, Italy) aim to develop a correct model for the management of coastal aquifers, which are affected by seawater intrusion due to overexploitation for various purposes. This study updates and integrates hydrogeological knowledge of the area; in addition, it proposes a monitoring network and remedial actions. Completed analyses reveal the presence of coexisting flow systems of different rank which allow the mixing of freshwater and saltwater, both superficial (recent) and deep (old), in various proportions. Hydraulic head measurements reveal the important impact of pumping on the flow of groundwater, with the formation of a negative hydraulic head in areas of int...
Ongoing hydrogeological research aims to develop a correct management model for the Plio-Pleistocene...
The gravelly horizon of the Pisa plain multilayered system, located at a depth between 50 and 100 m ...
The gravelly horizon of the Pisa plain multilayered system, located at a depth between 50 and 100 m ...
Ongoing hydrogeological investigations in the Grosseto Province (southern Tuscany, Italy) aim to dev...
Ongoing hydrogeological investigations in the Grosseto Province (southern Tuscany, Italy) aim to dev...
Ongoing hydrogeological investigations in the Grosseto Province (southern Tuscany, Italy) aim to dev...
Ongoing hydrogeological investigations in the Grosseto Province (southern Tuscany, Italy) aim to dev...
Ongoing hydrogeological research aims to develop a correct management model for the Plio-Pleistocene...
Ongoing hydrogeological research aims to develop a correct management model for the Plio-Pleistocene...
Ongoing hydrogeological research aims to develop a correct management model for the Plio-Pleistocene...
Ongoing hydrogeological research aims to develop a correct management model for the Plio-Pleistocene...
The gravelly horizon of the Pisa plain multilayered system is a confined aquifer tapped by a large n...
Seawater intrusion monitoring is essential to assess groundwater deterioration, guarantee sustainabl...
The multilayered aquifer system of the Versiliese Pisan coastal plain is mainly made up of sandy and...
Seawater intrusion monitoring is essential to assess groundwater deterioration, guarantee sustainabl...
Ongoing hydrogeological research aims to develop a correct management model for the Plio-Pleistocene...
The gravelly horizon of the Pisa plain multilayered system, located at a depth between 50 and 100 m ...
The gravelly horizon of the Pisa plain multilayered system, located at a depth between 50 and 100 m ...
Ongoing hydrogeological investigations in the Grosseto Province (southern Tuscany, Italy) aim to dev...
Ongoing hydrogeological investigations in the Grosseto Province (southern Tuscany, Italy) aim to dev...
Ongoing hydrogeological investigations in the Grosseto Province (southern Tuscany, Italy) aim to dev...
Ongoing hydrogeological investigations in the Grosseto Province (southern Tuscany, Italy) aim to dev...
Ongoing hydrogeological research aims to develop a correct management model for the Plio-Pleistocene...
Ongoing hydrogeological research aims to develop a correct management model for the Plio-Pleistocene...
Ongoing hydrogeological research aims to develop a correct management model for the Plio-Pleistocene...
Ongoing hydrogeological research aims to develop a correct management model for the Plio-Pleistocene...
The gravelly horizon of the Pisa plain multilayered system is a confined aquifer tapped by a large n...
Seawater intrusion monitoring is essential to assess groundwater deterioration, guarantee sustainabl...
The multilayered aquifer system of the Versiliese Pisan coastal plain is mainly made up of sandy and...
Seawater intrusion monitoring is essential to assess groundwater deterioration, guarantee sustainabl...
Ongoing hydrogeological research aims to develop a correct management model for the Plio-Pleistocene...
The gravelly horizon of the Pisa plain multilayered system, located at a depth between 50 and 100 m ...
The gravelly horizon of the Pisa plain multilayered system, located at a depth between 50 and 100 m ...