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.[2] Naturally occurring salinization is referred to as primary salinization; this includes rainfall, rock weathering, seawater intrusion, and aerosol deposits.[3] Human-induced salinization is termed as secondary salinization, with the use of de-icing road salts as the most common form of runoff.[4] 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.[5]