The Río Tinto, located in the Iberian Pyrite Belt (SW Spain), constitutes an extreme case of
pollution by acid mine drainage. Mining in the area dates back to the Copper Age, although large-scale
mining of massive sulfide deposits did not start until the second half of the 19th century. Due to
acidic mining discharges, the Río Tinto usually maintains a pH close to 2.5 and high concentrations of
pollutants along its course. From a detailed sampling during the hydrological year 2017/18, it was
observed that most pollutants followed a similar seasonal pattern, with maximum concentrations
during autumn due to the washout of secondary soluble sulfate salts and minimum values during
large flood events. Nevertheless, As and Pb showed different behavior, with delayed concentration
peaks. The dissolved pollutant load throughout the monitored year reached 5000 tons of Fe, 2600 tons
of Al, 680 tons of Zn, and so on. While most elements were transported almost exclusively in the
dissolved phase, Fe, Pb, Cr, and, above all, As showed high values associated with particulate matter.
River water quality data from 1969 to 2019 showed a sharp worsening in 2000, immediately after the
mine closure. From 2001 on, an improvement was observed.
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