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19811. Normal plant available nickel concentrations in soil are slightly less than 2 ppm (Barth <br />et al., 19811. <br />Zinc. Zinc is a necessary component of several enzyme systems which regulate various <br />metabolic activities within plants. Adequate zinc levels are essential for normal cell division, <br />root growth, seed production, protein metabolism, and auxin formation (Tiedemann and <br />Lopez, 19821. For normal growth, most plants generally require a minimum zinc concentration <br />of 1 ppm while zinc related toxicity occurs at about 70 ppm. The potential for zinc deficiency <br />is increased by many factors including but not limited to high pH, high lime rates, high <br />phosphorous levels, and high concentrations of other metallic nutrients ICu, Fe, and Mnl. Zinc <br />toxicity is more of a concern on acid soils because of the higher solubility of zinc on acid soils. <br />The antidote for zinc toxicity is the application of lime (Traynor, 1 9801. <br />Cadmium. Cadmium is a non-essential metallic element that is used in industry. Plant <br />toxicities due to elevated levels of cadmium under natural conditions or in reclamation are <br />unlikely (Barth et al., 1981 and Munshower, 19831. <br />Mercury. Mercury predominantly exists in an inorganic form which is not absorbed readily by <br />plants. There have been no documented cases of mercury toxicity to plants or to animals <br />under normal conditions. Mercury toxicity is limited to industrial or agricultural situations <br />where mercuric fungicides or other contaminants are used (Barth et al., 1981 and Munshower, <br />1983). <br />Lead. This is anon-essential Ito plant and animal life) heavy metal that could induce plant <br />toxicity symptoms if present in excess quantities. As the pH decreases, the solubility and the <br />potential for lead toxicity increases. In most soils of the Great Plains, lead is complexed and <br />not readily leached to ground water nor available for plant uptake (Barth et al., 1951 and <br />Munshower, 19831. <br />Arsenic. Munshower (19831 states that toxic concentrations of arsenic in natural soils and <br />overburden have never been reported. Barrett and others (1980) stipulate that toxicity is <br />confined to soils which have accumulated arsenic through foliar spray compounds. The <br />arsenates are fixed by soils in a relatively insoluble state and are not lost by leaching. The <br />critical water-soluble arsenic concentration in soils is 2 ppm (USDA, 19571• <br />Aluminum. Aluminum is a non-essential metallic element that could induce plant toxicity <br />symptoms if present in excess quantities. Although aluminum is the third most abundant <br />element in the earth's crust, it is typically available for plant uptake in only trace amounts in <br />alkaline soil (Traynor, 19801. Like other heavy metals, the aluminum concentration in the soil <br />solution increases as the soil becomes more acid, In extremely acid soils, aluminum is released <br />from the crystal lattice of clay minerals to cation exchange sites and into the soil solution <br />PR03 14 Revised 07/02 <br />