The Simulation of Bracciano Lake (Central Italy) Levels Based on Hydrogeological Water Budget: A Tool for Lake Water Management when Climate Change and Anthropogenic Impacts Occur

Abstract

Bracciano Lake is one of the major water bodies of Lazio region and the eighth lake in Italy by area. Similarly to other water bodies located on the Tyrrhenian side of the Italian Peninsula, Bracciano Lake has a volcanic origin. This water body is a strategic resource for both the emergency and ordinary water supply of Rome megacity, thanks to the short distance (about 30 km). During the last years, the concurrence of climate change and anthropogenic activities led to important water level drops of the lake: the last and worst in 2017, when the lake faced the most important water crisis of its entire history, with a critical impact on the ecological system and the consequent interruption of water supply. This paper, using the inverse hydrogeological water budget (HWB) method in a GIS environment, aims to define the water budget of Bracciano Lake on a 15-year time series (2008–2022), providing a framework of climate change and human impacts on lake water levels. The outputs have been used for the simulation of lake water levels during the same period, with a focus on the drought of 2017. The variation between simulated and observed level is, on average, 2 cm and in any case never more than 28 cm. Results show the fragile balance between inputs and outputs, highlighting the need for sustainable management of both surface water and groundwater withdrawals from the surrounding aquifer.

Geochemical Evolution in Historical Time of Thermal Mineral Springs at Campetti Southwest (Veii, Central Italy) through Geoarcheological Investigation

“…The shallow volcanic aquifer is multilayered, unconfined, and recharged by local rainfall [29][30][31]. In the northern and western sectors, it discharges into Bracciano Lake; in the southern and eastern sectors, groundwater discharge has a centrifugal pattern from the lake (Figure 1A) [29,31,32]. In the peripherical sectors of the SVD, groundwater is drained by gaining streams as the aquitard crops out at the bottom of the fluvial valleys [33].…”