Syracuse NY sits on top of a large Brine Aquifer that was used in the 1800 to produce most of the salt used in the US, thus the name Salt City.
I believe the Brine Aquifer below Syracuse has enough heat capacity to serve as an Energy Bank in support of a City wide Open Loop Geothermal District Heating and Cooling network.
The District would consist of a network of PE pipes carrying a water/glycol solution from city building to central brine heat exchangers located over the brine aquifer that runs under the N/S valley in the center of the city.
I am looking for help to do a feasibility study, design concepts for large brine/glycol heat exchanger, information on any similar projects.