1. Factors Affecting Water Quality Chapter 6

2. Introduction  Many types of pollutants and many factors affecting the toxic effect of those pollutants  Factors include physicochemical properties physicochemical properties Mode and time of exposure Mode and time of exposure Environmental factors Environmental factors Interactions among toxicants in a mixture Interactions among toxicants in a mixture Biological factors Biological factors Nutritional factors Nutritional factors

3. Chemical Characterization of Water I. Structure Chemical Structure Chemical Structure 1. Inorganic Cations Anions Cations Anions Ca ++ Mg ++ Na ++ (K + ) HCO - 3 SO 4 - Cl - PO 4 - NO 3 - Ca ++ Mg ++ Na ++ (K + ) HCO - 3 SO 4 - Cl - PO 4 - NO 3 - bicarbonate bicarbonate Normal environmental concentrations mg/L 15 8 6 23 120 12 8 v. low (<1) Note: because NO 3 - is not limited in freshwater  casual about disposal (i.e. Spring River) limited in freshwater limited in oceans

4. 2. Organic pH is the master variable but pH of aquatic system is intricately linked to the relative abundance of carbonate, bicarbonate and carbon dioxide. Normal range Carbonate-bicarbonate equilibrium

5. Hardness  Degree of difficulty in precipitating soap  Based on combined concentrations of calcium, magnesium and other cations  Can have great effect of toxicity (increasing hard = decreasing toxicity) Units – CaCO 3 2- mg/L (accounts for all metals which are +2 ) Units – CaCO 3 2- mg/L (accounts for all metals which are +2 ) Typical values (as CaCO 3 2- ) Typical values (as CaCO 3 2- ) <5- - 100 mg/Lsoft<5- - 100 mg/Lsoft 100 - 200 mg/L moderately hard100 - 200 mg/L moderately hard >200 “ hard>200 “ hard Carbonate vs. Non-carbonate hardness Carbonate vs. Non-carbonate hardness Note: heat can change hardness -> forms scale on boilers, coffee pots

6. Alkalinity  Measurement of the capacity to accept protons (esp. H + )  called buffering capacity Units also expressed as CaCO 3 2- Units also expressed as CaCO 3 2- Really measures CaCO 3 2- (bicarbonate) Really measures CaCO 3 2- (bicarbonate) Alkalinity directly correlated with hardness in many systems Alkalinity directly correlated with hardness in many systems Soft water = low alkalinitySoft water = low alkalinity Hard water = high “ (but exceptions  AMD)Hard water = high “ (but exceptions  AMD) Measured by titrating with H 2 SO 4  drives bicarbonate to CO 2 Measured by titrating with H 2 SO 4  drives bicarbonate to CO 2 Rule of thumb  water of low hardness, low alkalinity (headwaters) = higher effect of toxicants (especially true of metals, acid) Rule of thumb  water of low hardness, low alkalinity (headwaters) = higher effect of toxicants (especially true of metals, acid)

7. Alkalinity (con’t) Rule of thumb: water of low hardness, low alkalinity (headwaters) = higher effect of toxicants (especially true of metals, acid) Rule of thumb: water of low hardness, low alkalinity (headwaters) = higher effect of toxicants (especially true of metals, acid) Headwaters of the Hudson River Photo by R. Grippo

8. Oxygen  Amount of oxygen that can be dissolved in water (solubility) is highly dependent on temperature Note: atmosphere = 210,000 mg/L but ~10 mg/L in most water so O 2 is is usually in very short supply in water

9. B. Physical structure 1. Stream order – rough numerical sequence that allows characterization of a stream 1 1 springs 22 3 1 4 3 6 headwaters Mid-reach 6-12 = river Lower reach Note: streams of same order have to come together to form next order Note: headwaters generally straight, starts to wander (form bends = sinuosity) as hit order 4-6. Sinuosity is a function of slope, hardness of substrate (mud<silt<gravel) Hard substrate = low sinuosity Soft substrate = high sinuosity

10. II. Function - function always based on structure  can infer function from structure A. Rivers 1. River Continuum Concept - RCC based on two concepts a. From headwaters to mouth = continuous change (gradient) in physical conditions within a stream system b. Gradient produces a continuous and predictable change in the make-up of the assemblages of organisms within a stream system

11. Upper reaches ----------------  mid-reach ---------------------  lower reach (headwater to 3 rd order) (order 4 to 6) (>6) Continuous and predictable changes in biotic assemblages Use bioassessment (sample, enumerate organisms)  if do not find what is predicted  problem!!

12. B. Lakes systems are dynamic but slow systems are dynamic but slow Pollution stays put (reason why sewage treatment plants are built on rivers, not lakes Pollution stays put (reason why sewage treatment plants are built on rivers, not lakes More likely to More likely to Serve a pollution sinks (bioremediation slow if lake is deep (e.g. Great Lakes)Serve a pollution sinks (bioremediation slow if lake is deep (e.g. Great Lakes) Can be highly influenced by aerial depositionCan be highly influenced by aerial deposition

13.  Pollutants usually introduced as leachate from contaminated soils  Dependent on physical/chemical properties of soils in addition to water C. Groundwater