Turbidity in open water may be caused by growth of
phytoplankton. Human activities that disturb land, such as
construction,
mining and
agriculture, can lead to high
sediment levels entering water bodies during rain storms due to
storm water runoff. Areas prone to high bank erosion rates as well as
urbanized areas also contribute large amounts of turbidity to nearby waters, through stormwater
pollution from
paved surfaces such as roads, bridges, parking lots and airports. Some industries such as
quarrying, mining, and coal recovery can generate very high levels of turbidity from colloidal rock particles. In drinking water, the higher the turbidity level, the higher the risk that people may develop
gastrointestinal diseases. This is especially problematic for immunocompromised people, because contaminants like
viruses or
bacteria can become attached to the suspended solids. The suspended solids interfere with water disinfection with
chlorine because the particles act as shields for viruses and bacteria. Similarly, suspended solids can protect bacteria from
ultraviolet (UV) sterilization of water. In water bodies such as
lakes, rivers and
reservoirs, high turbidity levels can reduce the amount of light reaching lower depths, which can inhibit growth of submerged
aquatic plants and consequently affect species which are dependent on them, such as
fish and
shellfish. High turbidity levels can also affect the ability of
fish gills to absorb dissolved oxygen. This phenomenon has been regularly observed throughout the
Chesapeake Bay in the eastern United States. For many
mangrove areas, high turbidity is needed in order to support certain species, such as to protect juvenile fish from predators. For most mangroves along the eastern coast of
Australia, in particular
Moreton Bay, turbidity levels as high as 600
Nephelometric Turbidity Units (NTU) are needed for proper
ecosystem health. ==Measurement==