Salt consists of sodium chloride. Through primary and secondary salinization, it intrudes into freshwater and damages the health of humans and other organisms.
Freshwater salinization is the process of salty runoff contaminating freshwater ecosystems, which can harm aquatic species in certain quantities and contaminate drinking water.[1] It is often measured by the increased amount of dissolved minerals than what is considered usual for the area being observed.[citation needed] Naturally occurring salinization is referred to as primary salinization; this includes rainfall, rock weathering, seawater intrusion, and aerosol deposits.[2] Human-induced salinization is termed as secondary salinization, with the use of de-icing road salts as the most common form of runoff.[3] Approximately 37% of the drainage in the United States has been affected by salinization in the past century.[1] The EPA has defined two thresholds for healthy salinity levels in freshwater ecosystems: 230 mg/L Cl− for average salinity levels and 860 mg/L Cl− for acute inputs.[4]
^Evans, D. M.; Villamagna, A. M.; Green, M. B.; Campbell, J. L. (September 2018). "Origins of stream salinization in an upland New England watershed". Environmental Monitoring and Assessment. 190 (9): 523. doi:10.1007/s10661-018-6802-4. PMID30116969.