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 mining iodine from brine is Japan, where iodine-rich water is co-produced with natural gas. Iodine extraction began in 1934. In 2013 seven companies were reported to be extracting iodine. Japanese iodine brines are produced from mostly marine sediments ranging in age from Pliocene to Pleistocene. The main producing area is the Southern Kanto gas field on the east-central coast of Honshu. The iodine content of the brine can be as high as 160ppm. Since 1977, iodine has been extracted from brine in the Morrow Sandstone of Pennsylvanian age, at locations in the Anadarko Basin. of northwest Oklahoma. The brine occurs at