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Intensification of agriculture and manufacturing industries
has resulted in increased release of a wide range of xenobiotic compounds to the environment. Excess loading of hazardous
waste has led to scarcity of clean water and disturbances of
soil, thus limiting crop production (Kamaludeen et
al., 2003). Bioremediation uses biological agents, mainly microorganisms,
i.e., yeast, fungi or bacteria to clean up contaminated soil and water (Strong and Burgess,
2008). This technology relies on promoting the growth of specific microflora or microbial
consortia that are indigenous to the contaminated sites that are able to perform
the desired activities (Agarwal, 1998). Establishment of such microbial consortia can be done in several ways,
e.g., by promoting growth through addition of nutrients, by adding terminal electron
acceptor, or by controlling moisture and temperature conditions (Hess et al., 1997; Agarwal, 1998; and Smith et
al., 1998). In bioremediation processes, microorganisms use the contaminants
as nutrient or energy sources (Hess et al., 1997; Agarwal,
1998; and Tang et al., 2007).
An indication of organic oxygen demand content of wastewater can be obtained
by measuring the amount of oxygen required for its stabilization either as Biological
Oxygen Demand (BOD) or as Chemical Oxygen Demand (COD). BOD is the measure of the
oxygen required by microorganisms whilst breaking down organic matter. While COD is the
measure of amount of oxygen required by both potassium dichromate and concentrated sulphuric
acid to break down both organic and inorganic matters. BOD and COD concentrations of
the wastewater are measured, as the two are important in unit process design. Though
BOD is a measurement of the oxygen required for microorganisms whilst breaking down
organic matter to stable inorganic forms, such as
CO2, NO3 and H2O, the water with high
BOD indicates organic pollution. COD is used as a measurement of the oxygen equivalent of
the organic matter content of a sample that is susceptible to oxidation by a strong chemical
oxidant. Usually, the concentrations of COD in surface water ranges from 20 mg/L or less in
unpolluted water to greater than 20 g/L in water receiving effluents. Nitrogen-nitrate is the final
oxidation product of nitrogen. Natural sources of nitrate to surface waters include igneous rocks,
land drainage, and plant and animal debris. Natural levels, which seldom exceed 0.1 mg/L
NO3-N, may be enhanced by municipal and industrial wastewater, including leachates from
waste disposal sites and sanitary landfills. In rural and suburban areas, the use of inorganic
nitrate fertilizers can be a significant source. Phosphate is essential for the growth of organisms
and can be the nutrient that limits the primary productivity of a body of water. In instances,
where phosphate is a growth limiting nutrient, the discharge of raw or treated wastewater,
agricultural drainage, or certain industrial wastes to that water may stimulate the growth of
photosynthetic aquatic micro and macroorganisms in nuisance quantities. |