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130                                                  Soil and Water Contamination
                    a                                     b
                                                                                           6642  6642  6642


                      Metal concentration in pore water     Metal concentration in pore water












                      0     Metal concentration in sediment  0    Metal concentration in sediment

                    Figure 7.3  Relation between metal concentrations in sediment  and pore water under oxidised (a) and reduced (b)
                    conditions.
                    and manganese  oxyhydroxides . It should be clear from the above that the pH is the master
                    variable determining the mobility of heavy metals under oxidising conditions, as it controls
                    adsorption, complexation , and precipitation. All these processes bring about a decrease in the
                    mobility of heavy metals with increasing pH.
                       Under reduced conditions, the mobility of most metals  is further decreased due to the
                    formation of barely soluble sulphide  minerals. In this case, the concentration of heavy metals

                    in the dissolved phase  is controlled by the solubility product  of the sulphide minerals, which
                    means that the total concentration of heavy metals barely influences the concentration of
                    dissolved heavy metals (Salomons and Förstner, 1984) (see Figure 7.3b).


                    7.2  ZINC
                    Zinc is found mainly in the 2+ oxidation state  and occurs in metalliferous ores as zinc
                    sulphide  (ZnS; sphalerite). In general, zinc has about the same abundance in crustal rocks
                    as copper  and nickel  (see Tables 1.1 and 7.1), but tends to be more soluble in most types of
                    natural water (Hem, 1989). The concentrations of zinc in soil are usually the highest of all
                    heavy metals . Zinc is subject to specific adsorption  in soils and sediments, and the strength
                    of the bond tends to increase with the ageing of zinc (i.e. how long ago the soluble zinc was
                    released).
                       Zinc is an essential trace nutrient and forms part of many enzymes needed for growth
                    and development and DNA synthesis. Zinc metalloenzymes play an important role in many
                    aspects of cellular metabolism, including DNA replication, repair and transcription protein
                    synthesis, and energy metabolism. In animals and humans, it also plays important roles in
                    neurosensory functions, insulin synthesis, and cell-mediated immunity, and is required in
                    sufficient levels to ensure and maintain the body’s immunity, strength, and general well-
                                                                                           -1
                    being. Normal average zinc  intake by adult humans through the diet ranges from 7 mg d
                                                                             -1
                              -1
                    to 16 mg d . Food may contain levels of zinc ranging from 6 mg kg  dry matter (e.g.
                                      -1
                    potatoes) to 24 mg kg  dry matter (e.g. meat, fish, and poultry). In humans and animals,
                    long-term exposure to excess levels of zinc may result in copper  deficiency, reduced immune
                    function, reduced levels of high-density lipoproteins (the good cholesterol), anaemia, death
                    of foetuses, and damage to the liver, pancreas, and kidneys (ATSDR, 2013). However, in
                    the context of pollution, zinc is more a cause of phytotoxicity rather than being toxic to








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