Salinization of inland waters as part of the anthropogenic salt cycle
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Freshwater salinization is a key component of the anthropogenic salt cycle, in which human activities have altered the sources, fluxes, and flowpaths of salt ions across diverse earth systems causing a constellation of interrelated and interactive symptoms in freshwaters. Consequences of an accelerated global salt cycle and freshwater salinization include contaminant mobilization, loss of biodiversity, corrosion of infrastructure, and human health risks. We show that enhanced salt inputs from road salt, wastewater, saltwater intrusion, and other disturbances are perturbing the cycles of salt and associated chemical cocktails across freshwater ecosystems. We explore a few emerging human health implications linked to the anthropogenic salt cycle and salinization of inland waters such as: (1) saline dust from lake drying and respiratory diseases, (2) mobilization of radionuclides in groundwater and cancers, (3) arsenic and metals mobilization and saltwater intrusion, (4) hypertensive disorders and sodium restricted diets, and (5) mobilization of trace metals from soils and piped infrastructure. We illustrate the formation and mobilization of harmful chemical cocktails of Cu, Pb, Cd, Zn, As, Ra, U, Mn, and other contaminants as driven by major ions in the anthropogenic salt cycle and a combination of geochemical processes such as: chlorocomplexation, ion exchange, changes in pH and adsorption and solubility of metals, sodium dispersion of organic matter in soils, shifting redox conditions with saltwater intrusion and complex biogeochemical interactions, and extensive changes in the abundance and forms of ligands in response to freshwater salinization. Finally, we analyze, compare, and contrast the salt retention capacity of different strategies for stormwater management, stream restoration, riparian forest conservation, and other watershed management approaches. If left unmanaged, salinization of inland waters can spread across progressive stages, perturb systems into alternative stable states, and contribute to losses in critical services and functions provided by natural and engineered water systems along its trajectory.