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
Sink works Sink works Sink works or sinkworks (from German "Sinkwerke") is a method of salt mining from salt deposits in mountainous areas. It is similar to brine wells in that salt was extracted by dissolving it in water. Both approaches simulate natural brine springs. It is one of the earliest methods of salt extraction from salt domes. A "sinkwerk" is a chamber in a salt mine filled with water to dissolve salt. The resulting brine is then pumped via brine pipelines to saltworks. This approach is commonly used when salt deposits are heavily contaminated (or, alternatively, when salt content in the