Analysis of Water Chemistry
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Urban Stream Restoration Project
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Outline
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Water Chemistry Background
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Chemistry in Urban Streams
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Methods
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2003 Results
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Comparison to 2002
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Conclusions
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Outline
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Water Chemistry Background
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Chemistry in Urban Streams
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Methods
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2003 Results
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Comparison to 2002
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Conclusions
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Temperature
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Most aquatic organisms are cold-blooded and have an ideal temperature range, specific to the organism:
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Diatoms 15-25 degrees C
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Green algae 25-35 degrees C
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Blue greens 30-40 degrees C
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Salmonids – cold water fish
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Temperature, continued
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Affects development of invertebrates, metabolism of organisms
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Affects dissolved oxygen (warm water holds less oxygen)
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Warm water makes some substances more toxic (cyanide, phenol, xylene, zinc) and, if combined with low DO, they become even more toxic
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Dissolved Oxygen
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Oxygen that is dissolved in water
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DO increases with cooler water and mixing of water through riffles, storms, wind
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Nutrient loading can lead to algal blooms which result in decreased DO
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4-5 ppm DO is the minimum that will support large, diverse fish populations. Ideal DO is 9 ppm. Below 3 ppm, all fish die.
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Dissolved Oxygen, continued
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Dissolved oxygen can also be expressed as % saturation
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80-124% = excellent
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60-79% = ok
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< 60% = poor
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Conductivity
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Measures the ability of water to carry an electric current
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Measures the ions such as Na+, Cl- in the water
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Differences in conductivity are usually due to the concentration of charged ions in solution (and ionic composition, temp.)
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Reported as microsiemens per cm
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pH
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pH measures the degree of acidity or alkalinity of the water (each number is a 10-fold difference)
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0-6 = acid; 7 = neutral; 8-14 = base
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Ideal for fish = 6.5 –8.2
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Ideal for algae = 7.5 – 8.4
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Acid waters make toxic chemicals (Al, Pb, Hg) more toxic than normal, and alter trophic structure (few plants, algae)
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Turbidity
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Measures the cloudiness of the water
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Turbidity caused by plankton, chemicals, silt, etc.
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Most common causes of excess turbidity are plankton and soil erosion (due to logging, mining, farming, construction)
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Turbidity, continued
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Excess Turbidity can be a problem:
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Light can’t penetrate through the water – photosynthesis may be reduced or even stop – algae can die
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Turbidity can clog gills of fish and shellfish –can be fatal
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Fish cannot see to find food, but can hide better from predators
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Phosphorus (Reactive)
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Is necessary for plant and animal growth
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Natural source = phosphate-containing rocks
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Anthropogenic source = fertilizer and pesticide runoff from farming
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Can stimulate algal growth/bloom
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Nitrates
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Formed by the process of nitrification (addition of O2 to NH3 by bacteria)
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Used by plants and algae
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Is mildly toxic, fatal at high doses
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Large amounts (leaking sewer pipes, fertilizer runoff, etc.) can lead to algal blooms, which can alter community structure, trophic interactions and DO regimes)
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Below 90 mg/L seems to have no effect on warm water fish, but cold water fish are sensitive
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Alkalinity
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A measure of the substances in water that can neutralize acid and resist changes in pH
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Natural source = rocks
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Ideal water for fish and aquatic organisms has a total alkalinity of 100-120 mg/L
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Groundwater has higher alkalinity than surface water
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Hardness
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The amount of Calcium and Magnesium in the water (the two minerals mostly responsible)
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Natural source = rocks
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Limestone = hard water, granite = not hard water
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Hardness, continued
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Soft water can be a problem: in soft water, heavy metals are more poisonous, some chemicals are more toxic, drinking soft water over long periods can increase chance of heart attack
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0 – 60 = soft water
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61-120 = moderately hard water
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121-180 = hard water
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181+ = very hard water
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Hardness and alkalinity are related
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Outline
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Water Chemistry Background
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Chemistry in Urban Streams
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Methods
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2003 Results
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Comparison to 2002
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Conclusions
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Physical Effects of Urbanization Related to Water Chemistry
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Riparian Vegetation Removal
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Decreased Groundwater Recharge
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Heat Island Effect
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Increased Surface Runoff / Impervious Surfaces
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Leaky Storm-water / Sewage Pipes
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Point Source Pollution
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Trends in Water Chemistry
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Temperature increases
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Nitrate increases
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Phosphorus increases
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Conductivity increases (Increased ion concentration)
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O2 demand increases
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Outline
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Water Chemistry Background
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Chemistry in Urban Streams
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Methods
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2003 Results
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Comparison to 2002
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Conclusions
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Field Measurements
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Dissolved Oxygen
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Temperature
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Conductivity
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pH
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Water Collection For Laboratory Analysis
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Grab Samples
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Three replicates (from multiple samples)
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Measured within 24 hours (few exceptions)
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Laboratory Analysis
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Nitrate
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Reactive
Phosphorus
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Alkalinity
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Hardness
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Turbidity
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Outline
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Chemistry in Urban Streams
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Water Chemistry Measurements and Theory
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Methods
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2003 Results
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Comparison to 2002
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Conclusions
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Field Measurements 2003
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Turbidity
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All values for 2003 <5 jtu
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For 2002, all but one sampling date <5 jtu
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The one date for 2002 >5 was during a storm event
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Reactive Phosphorus 2003
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Nitrate 2003
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Alkalinity 2003
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Hardness 2003
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Outline
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Chemistry in Urban Streams
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Water Chemistry Measurements and Theory
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Methods
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2003 Results
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Comparison to 2002
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Conclusions
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Field Measurement PB
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Field Measurement For SAL
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Paint Branch
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Stewart April Lane
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Outline
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Chemistry in Urban Streams
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Water Chemistry Measurements and Theory
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Methods
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2003 Results
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Comparison to 2002
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Conclusions
Between Site Differences
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Land use – increased runoff cause increased input of particular constituents
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Natural site variation – Substrate type
Between Years
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Increased snow caused more runoff increased use of road-salt
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Drought (temperature, DO)
“. . . Rivers and the inhabitants of the watery element were made for wise men to contemplate, and fools to pass by without consideration, . . . for you may note, that the waters are Nature’s storehouse, in which she locks up her wonders.”
Izaak Walton
(from Ward, 1992)
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