The effects of chemical time bombs are typically discontinuous and non-linear. Once a certain threshold has been passed, the system starts to behave differently from before (Stigliani, 1991). A typical example is the consumption of a certain buffer capacity in a system, and the subsequent breakthrough of parameters such as pH values and metal concentrations. The mobilization of metals from different types of waste materials, after the depletion of typical barriers (mechanical or chemical) or after an increase of accelerating factors such as the lowering of pH values, was studied. The release of metals from sediments, leaks of pollutants from sludges and wastes, and some remedial approaches are discussed.
KEY WORDS Metal release Estuarine sediments Leaks Remedial approaches
RELEASE OF METALS FROM RIVERINE AND ESTUARINE SEDIMENTS
Oxidation of sulphides and release of protonsAcidity is perhaps the most serious long-term threat from metal-bearing wastes. Water seeping from mine refuse has been transferring increased concentrations of metals into receiving waters for decades. The threat is especially serious in waters with little buffering capacity, i.e. in carbonate-poor areas where dissolved metal pollution can be spread over great distances. The production of acidity can develop many years after disposal, when the neutralizing or buffering capacity in a pyrite-containing waste is exceeded.The main process affecting the lowering of pH values (to less than 3) is the exposure of pyrite (FeS2) and other sulphide minerals to atmospheric oxygen and moisture, whereby the sulphidic component is oxidized to sulphate and acidity (protons or H+ ions) is generated. Bacterial action can assist in the oxidation of Fe2+ (aq.) in the presence of dissolved oxygen.The acidification problem of a sediment-water system arises after hydrogen ions have been generated during oxidation, e.g. during dredging or the resuspension of (mainly) fine-grained material containing less carbonate than is needed for long-term neutralization (Drever, 1982;Breemen, et al., 1984). Primary emissions of high metal concentrations occur from waste rocks and tailings, secondary effects on groundwater take place from contaminated ponds. Important and long-term sources of metals are sediments reworked from floodplains, mainly by repeated oxidation and reduction processes (Moore and Luoma, 1990). High concentration factors have been found in inland waters affected by acidic mine effluents (Forstner, 1981).The concept of acid-producing potential (APP) was initially developed in the prediction and calculation of acid mine drainage and waste tailings management (Anonymous, 1979; a summary is given by Ferguson and Erickson, 1988). Our findings on the effects of periodic redox processes on both the APP and metal mobility in estuarine sediments (Kersten, et al., 1985;Kersten and Forstner, 1991) have further enhanced research interest in this field.Direct assessment of the pH changes resulting from the oxidation of anoxic sediment constituents can be performed ...