Instructor's Manual - Alkalinity
What is alkalinity?
Alkalinity is a measure of the capacity of water to neutralize acids. This is known as the buffering capacity of water or the ability of water to resist a change in pH when acid is added. Alkalinity in water is due primarily to the presence of bicarbonate, carbonate, and hydroxide ions. It relates to the balance of carbon dioxide in water and is a function of pH.
How is alkalinity measured?
Alkalinity is expressed as phenolphthalein alkalinity or total alkalinity. Both types can be determined by a titration with standard sulfuric acid to an endpoint pH. Indicators such as phenolphthalein and bromcresol green-methyl red define endpoints or a pH meter could be used for determination of endpoints. Phenolphthalein alkalinity is determined by titration to a pH of 8.3 and indicates the total hydroxide and half the carbonate present. Total alkalinity is determined by titration to a pH of 5.1, 4.8, 4.5 or 3.7 depending upon the amount of carbon dioxide present. The total alkalinity includes all carbonate-bicarbonate alkalinity and hydroxide alkalinity. Bicarbonate is the major form of alkalinity. The unit of measurement for alkalinity is mg/L CaC03.
What is the significance of alkalinity?
Alkalinity is the measure of the resistance of water to the lowering of pH when acids are added to the water. Acid additions generally come from rain or snow, though soil sources are also important in some areas. Alkalinity increases as water dissolves rocks containing calcium carbonate such as calcite and limestone. Carbonates and hydroxide may be significant when algal activity is high and in industrial water.
When a lake or stream has too little alkalinity, typically below about 100 mg/L, a large influx of acids from a big rainfall or rapid snowmelt event could (at least temporarily) consume all of the alkalinity. This results in a drop the pH of the water to levels harmful for amphibians, fish or zooplankton. Lakes and streams in areas with little soil, such as in mountainous areas, are often low in alkalinity. These water bodies can be particularly sensitive in the spring during periods of rapid snowmelt. Because pollutants tend to wash out of a snow pack during the first part of snowmelt, there is often a higher influx of acidic pollutants in spring, which is also a critical time for the growth of aquatic life. Glacial till in the
Page last modified January 31, 2014