pH of different
water sources
The pH will of course vary with the water source. Seawater
normally has pH value between 7.8 and 8.3 and has a good buffering capacity due
to the available free bicarbonate. There is normally no need for pH adjustment.
The only exception being when re-using water to a great extent.
For fresh surface water, whether river or lake, the pH will be
highly dependent on the ground characteristics and whether the catchment area
is exposed to acid rain. Normal pH values are between 4 and 8.5. Groundwater
has a more stable pH, but the buffering capacity can be reduced and values
between 5.5 and 8.5 are common. If there islimestone rock in the catchment area
the pH will be high, while the pH of water coming from marshy areas can be low.
The alkalinity of the different sources can vary from below 10 mg/l CaCO3
in soft freshwater to several hundred of mg/l CaCO3 in seawater and
hard freshwater.10
It is important to be aware that there can be fluctuations in
the pH of freshwater during the year. Floods during spring may result in
dramatic reductions in pH, especially when snow is melting in the catchment
area where acid has accumulated in the snow. Also dry weather may affect the pH
of the water.
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