1ESM 202Understanding Water QualityParameters2Management Value of Monitoring Water Quality Parameters Human Health Sustainable management Restoration Remediation3Water Quality Parameters Dissolved Oxygen Temperature Biochemical Oxygen Demand Nutrients: N & P Minerals: Anions & Cations Trace Elements Toxic Organic Compounds Coliform Bacteria, other Microbes, Viruses Solids (TDS, SS) Alkalinity, pH Hardness Turbidity Color Taste and Odor4Dissolved Oxygen (DO)O2(gas) Æ O2(aq)IncreasingTempIncreasingSalinityHighDOLowDO6Basic Conceptsin WaterChemistry7Basic Concepts EquilibriumA + B = C + DK = [C] [D][A] [B]=ProductsReactants Thermodynamic equilibrium Reversible vs. irreversible8Basic ConceptsConcentration in aqueous or solid systems[HCO3-] = mol / L = MConvert from mol/L to g/L using the Molecular Weight (MW), g/molConcentration in gas phase: PCO2 = atm9Dissolution O2dissolution in waterO2(aq) O2(g)= 663 atm.L/mol 0.209 atm3.15 x 10-4mol/L10.07 x 10-3g/L32.00 g/mol= 0.000315 mol/L10.07 mg/L32.00 g/mol=KH,O2= [O2(aq)]PO2=10Dissolution CO2dissolution in water:CO2(aq) = CO2(g)KH= [CO2(aq)]= 26.9 atm L/molPCO211OxygenDemand12Oxygen Demand Chemical Oxygen Demand (COD) Biochemical Oxygen Demand (BOD) Nitrogenous Biochemical Oxygen Demand (NBOD) Total Oxygen Demand (TOD)CaHbOcNdSe+ x O2a CO2+ 1/2 b H2O + d NO3-+ e SO42-How much Oxygen is needed to degrade a load of pollutant?13Chemical Oxygen Demand Quick test to determine Oxygen Demand Strong oxidizing agent in acidic medium with catalyst (silver sulfate) No info on biologically oxidizable matter IssuesSome organic matter is quite inertInterference from minerals in waterCaHbOcNdSe+ Cr2O7 2-Cr3++ a CO2+ 1/2 b H2O + d NO3-+ e SO42-14Biochemical Oxygen Demand Measures “rapidly” biologically oxidizable organic matter Usually expressed as 5-day BOD = BOD5 Depending on BOD concentration and water characteristics:DilutionEssential nutrients (N, P, K, Fe, etc.)Bacterial seed15EZ BOD¾Simply¾ Place a sample of the microbial biomass into the test bottle with the wastewater¾ Insert integrated DO probe ¾ Follow instructions that appear on the liquid crystal display (LCD)¾Test provides a quantitative prediction of BOD5 (based on correlation to BOD5) ¾ For specific plant conditions¾ Data collected in 15 to 60 minutes16Nitrogenous BOD17Nitrogenous Oxygen Demand Two-step oxidation of ammonia:Can inhibit nitrification to measure CBOD and NBOD separatelyNH4++ 3/2 O2NitrosomonasNO2-+ H2O + 2 H+NO2-+ 1/2 O2NitrosobacterNO3-NH4++ 2 O2NO3-+ H2O + 2 H+18Effect of BOD in a RiverPollutant discharge19Microorganisms20MicroorganismsE. coliused as an indicator of water quality: normal inhabitant of intestines of many animals Indicator of presence of fecal matter Total coliforms are typically reported Cost of testing for all possible microorganism is $$$$22Coliform test Results reported as Most Probable Number (MPN) per 100 mL Incubation at moderate temperature (35 oC) for 48 hr Test does not account for normally occurring microbes which also respond to lactose New developments to deal with these issues23Sediments25Turbidity Water clarity is an indicator of drinking water quality In the field, use a Secchi disk In lab, measure transmission of light through a standard cuvetteColloidal particles scatter light Colloidal particles may harbor pathogens, toxics (metals, pesticides), radionuclides26Turbidity27Hardness Correlated with TDS Represents total concentration of Ca and Mg, and is reported in equivalent CaCO3 Other ions (Fe2+) may also contribute Hard water leaves solid deposits (boilers, hot water pipes, heaters, fixtures) and requires more soap Hard water is less corrosive28Hardness Soft < 50 mg/L Moderate = 50 - 150 mg/L Hard = 150 - 300 mg/L Very Hard > 300 mg/L Treatment usually left to consumer (domestic, industrial, etc.) depending on needs29pH30pH What is pH?Concentration of H+Measured on a log scaleActually, an inverse log…pH = -log10([H+])pH = 7 means [H+] = 10-7mol H+/L What does it mean?31pH Natural conditionsAcidicTemperate forest soils (pH 4-6)Raindrop through clean atmosphere (pH 5-5.5)Sulfur vents (pH 2-4)AlkalineArid soils (pH 8-11)Limestone dominated soils (pH 7-9)Ocean (pH 8-8.5)32pH Human (anthropogenic) changes to pHAcid rain (deposition)Acid mine drainageDischarge of acidic or alkaline wastewaterOpen mining of limestoneCattle feedstock yards (NH3)Fossil fuel combustion33pH Why does it matter? pH controls the chemical form (species) of many compounds Low pH leads to faster dissolution (weathering) of surrounding minerals Releases potentially toxic elements Changes in biodiversityHigh pH Can increase concentration of ammonia, toxic to fish Increased precipitation of metals34Dissociation of WaterH2O + H2O = H3O++ OH-Kw =[H3O+] [OH-][H2O ] [H2O ]=[H+] [OH-] = 10-14-log10(Kw ) = pKw= 1435pH-pC DiagrampCpH[H+][OH-]pH = 6pCH+= 6[H+]= 10-6M36pH-pC DiagrampCpH[H+][OH-]pH = 8pCH+= 8[H+]= 10-8M37MacroNutrients38Macro Nutrients Common Forms of Nitrogen: Ammonia/Ammonium NH3/ NH4+ Nitric Acid/Nitrate HNO3/ NO3- Nitrous Acid/Nitrite HNO2 /NO2- Organic NitrogenPhosphate PO43-, HPO42- Ratio of Uptake of Nutrients (typical):1:16:100::PNC39DissociationAcids:HNO3+ H2O = H3O++ NO3-KHNO3=[H+] [NO3-][HNO3]= 101mol/LpKHNO3= -1.0NH3+ H2O = NH4++ OH-KNH3 =[OH-] [NH4+][NH3]= 10-9.3mol/LpKNH3= 9.3Bases:40pH-pC Diagram for
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