Under the United Nations Globally Harmonized System of Classification Labelling and European Union Classification, Labelling and Packaging regulation, aquatic classification of a substance for chronic hazards is based on chronic toxicity and assessment of its degradability. This recognizes that, in the event of a release, effects from rapidly degraded substances are localized and of short duration because of reduced environmental exposure. This has been termed "rapid loss from the environment." For organic chemicals, rapid loss is determined by a standard biodegradability study demonstrating 70% conversion of the substance to CO 2 in 28 d. Substances meeting this criterion are given less severe chronic classifications. This can result in reduced restrictions on labeling, transport, and storage of these substances.A similar approach has not been accepted for inorganic substances (i.e., metals). However, several publications demonstrated rapid loss of metals from the water column with limited remobilization. Burton et al. (2019) provide a comprehensive review of the mechanisms of removal and rates for various metals. Huntsman et al. (2019) published a transformation/dissolution method specifically designed to measure loss from the water column in a laboratory setting. Diamond et al. (1990) measured half-times for metal radioisotope loss from the water column in lake enclosures. Rader et al. ( 2019) evaluated loss of copper from the water column in laboratory and field experiments and in a unit world model. They concluded, for the majority of studies examined, that >70% of the added copper was removed from the water column within 16 d, hence meeting the criterion of 70% removal in 28 d. It has been shown that metal loss from the water column is principally by sorption to particles and settling.The affinity of a given metal for the functional groups on suspended particulate matter is an intrinsic property of the metal, expressed by the Irving-Rossotti slope. This leads to the conclusion that removal rates will vary by metal and by the depth and properties of a given body of water. However, the overall conclusion is that common metals of interest, and copper in particular, are transported to sediments by particles, bound to iron and manganese oxyhydroxides; become covalently bound to sulfides; are buried in sediments; and undergo mineralization. In addition, laboratory/field observations have shown that sediment resuspension does not cause long-term remobilization of metals to the overlying water. Water column residence time of sediment particles is relatively short following resuspension, and therefore, metal-releasing redox and dissolution reactions do not have adequate time to reach equilibrium, thus allowing metal-sorbing phases in the suspended solids to scavenge metals. These 2 phenomena serve to make metal removal functionally irreversible.