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
Brine pool artificial earthworks and drainage structures to separate a body of water into a highly concentrated brine pool and a much less saline zone. Although this delays a body of water becoming entirely inhospitable to wildlife that cannot tolerate high levels of salinity, it does not remove dissolved salts and minerals from the local environment. Brine pool A brine pool is a large area of brine on the ocean basin. These pools are bodies of water that have a salinity four to eight times greater than the surrounding ocean. For deep-sea brine pools, the source of the salt is the dissolution