pH
Most North American rivers, lakes and streams fall within the range of pH 6.5-8.2. National guidelines recommend pH of 6.5-9.0 for the protection of aquatic life in freshwaters.
Atlantic
Most North American rivers, lakes and streams fall within the range of pH 6.5-8.2. National guidelines recommend pH of 6.5-9.0 for the protection of aquatic life in freshwaters.
pH in freshwater systems is affected by naturally occurring organic acids or by impacts from human activities, such as acid rain and acid rock drainage. When water is more acidic (has a lower pH) it can make certain chemicals and metals more toxic than normal. This is because acid waters make these elements more soluble – that is, they become more easily dissolved in the water and in this way become more biologically available to fish and other organisms.
Acid rain occurs when certain pollutants in the air (sulfur dioxide and nitrogen oxides) react with water to form acids. These acids are then deposited to the land, lakes, and rivers by rain and snow.
Acid rock drainage is a common problem in and around mines. Acidic conditions arise when sulphur-rich rocks are exposed to air and water (e.g., in tailings and waste rock piles). The acid often dissolves minerals, including metals, from the rock and both the acid and the metals can drain into waterways.
Most fish prefer to live in water that ranges in pH from around 6.4 to 8.4. Fish eggs grow and survive best at a narrower range of pH; from 6.0-7.2.
pH can be assessed using pH strips that change colour based on how acidic or basic the water is. The colour is evaluated against a guide to determine the approximate pH range of the water. The colour is evaluated against a guide to determine the approximate pH range of the water. pH can also be measured directly in a lake or river using a water quality meter with a pH sensor. Before use, this sensor is calibrated using standard solutions of known pH (typically pH 4, 7 and 10).
Related to pH: alkalinity, oxidation-reduction potential (ORP)
pH is influenced by: background water chemistry - especially carbonate, bicarbonate and naturally-occurring acids
pH influences: dissolved concentrations of many metals and metalloids in water