Brine rejection that drains from the newly formed ice is replaced by a weak flow of relatively fresh water, from the liquid region below it. The new water partially freezes within the pores of the ice, increasing the solidity of the ice. As sea ice ages and thickens, the initial salinity of the ice decreases due to the rejection of brine over time [Fig. 2]. While the sea ice ages, desalinization occurs to such a degree that some multiyear ice has a salinity of less than 1 PSU. This occurs in three different ways: Brine rejection occurs in the sea ice packs
Salt industry in Syracuse, New York "finished" salt. Additionally, the withdrawal of brine from the Tully valley brinefield area by Solvay Process Company over a 96-year period resulted in the removal of more than 96 million tons of salt. The days of salt production in Syracuse are long over, however, the city still honors the industry in names like Salina Street which is the main street through downtown, Solar Street, Salt Springs Road and the town of Salina, New York. There is also a neighborhood enclave in Syracuse named Salt Springs. The abandoned Onondaga Salt Springs Reservation became a dumping ground in the early 20th century,