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The self purification capacity of a river or stream depends on 6 main factors: temperature, hydrographic factors like velocity and surface area, the rate of re-aeration, the amount and type of organic matter present, the initial dissolved oxygen levels, and the types of microorganisms present. Faster moving streams with larger surface areas re-aerate more quickly, while streams with more biodegradable organic waste or lower initial dissolved oxygen levels have reduced self purification capacity. The presence of algae and bacteria can also increase re-aeration and help break down organic matter.







