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134                                                  Soil and Water Contamination

                    of kilometres from the source. The largest source of cadmium in the human food chain is,
                    however, the application of phosphate fertilisers , in which cadmium is present as impurity.
                    In addition, the spreading of contaminated sewage sludge  on agricultural  land contributes to
                    the human cadmium intake.


                    7.6  NICKEL

                    Nickel is a ferromagnetic transition metal  sharing many chemical properties with iron . It
                    occurs naturally in the Earth’s crust in various forms such as nickel  sulphides and oxides.
                    Nickel may occur in the oxidation state s 1-, 0, 2+, 3+, and 4+. However, the aqueous
                    chemistry of nickel is primarily concerned with the 2+ oxidation state. Other oxidation states
                    occur in special complexes and oxides. In alkaline solutions, Ni(II) hydroxide can be oxidised
                    to a hydrated Ni(IV) oxide. Like zinc, nickel is specifically adsorbed  in soils and sediments
                    and the binding strength increases with ageing of nickel (Hem, 1989).
                       Nickel is an essential nutrient that is only required in very small amounts. In plants,
                    symptoms of nickel  toxicity  are generally induced by iron deficiency: chlorosis  and
                    foliar necrosis. Excess nickel affects nutrient absorption by roots, root development, and
                    metabolism, and it inhibits photosynthesis and transpiration. Nickel can replace other metals
                    located at active sites in metallo-enzymes and disrupt their functioning. Its absorption into
                    the human body is affected by factors of consumption, the acidity of the gut, and various
                    binding or competing substances, including other metals such as iron, magnesium, zinc,
                    and calcium. An excess of nickel in tissues can cause damage to chromosomes and other
                    cell structures, alter hormone and enzyme activities, and affect membrane permeability and
                    immune function. As a result, changes in glucose tolerance, blood pressure, response to
                    stress, growth rate, bone development, and resistance to infection are possible. Nickel has
                    also been associated with possible carcinogenic effects (ATSDR, 2013).
                       Since the body’s requirement for nickel  is so low, excessive exposure from the
                    environment, leading to toxicity  is very common, e.g. from tobacco, dental implants,
                    stainless steel kitchen utensils, coins, and inexpensive jewellery.  The most common
                    trouble is allergy of the skin to nickel due to direct contact. On the other hand, toxicity by
                    consumption of food products grown on contaminated soil is very rare and would require
                    1000 times the amount normally consumed in food.
                       The nickel  used by industries comes from mined ores or from recycled scrap metal
                    and has a wide range of industrial uses. When alloyed with other elements, nickel imparts
                    toughness, strength, resistance to corrosion and various other electrical, magnetic, and heat-
                    resisting properties. It is primarily used in making various steels and alloys (e.g. stainless steel)
                    and in electroplating. Minor applications include the use in ceramics, permanent magnet
                    materials, and nickel–cadmium  batteries.


                    7.7  CHROMIUM

                    Chromium is found in the environment in three major states: chromium (0), chromium(III),
                    and chromium(VI).  The predominant oxidation state  in the environment is trivalent
                    chromium. Ultramafic igneous rocks  contain the most chromium. Chromite (FeCr O ),
                                                                                        2  4
                    which is highly resistant to weathering , may be concentrated in the lateric soils overlying
                    such rocks. In general, chromium (III) is largely present in soil as relatively unavailable,
                    insoluble chromium or chromium–iron  oxyhydroxides . It can also exist as a substitute
                    for Al(III) in the octahedral groups of aluminosilicates. The solubility of Cr(III) in soil is
                    dependent on pH  and decreases dramatically at pH values greater than 4.5. In aqueous










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