CEE 370 Lecture #25 11/6/2019 Print version Updated: 6 November 2019 CEE 370 Environmental Engineering Principles Lecture #25 Water Quality Management III: Lakes & toxic models Reading: Mihelcic & Zimmerman, Chapter 7 & 3.10 Reading: Davis & Cornwall, Chapt 5-4 Reading: Davis & Masten, Chapter 5-6 & 9-4 David Reckhow CEE 370 L#25 1 Lake Pollution Percent impaired by pollutant Percent impaired by sources From Masters, section 5.4 2 CEE 370 L#25 David Reckhow Lecture #25 Dave Reckhow 1
CEE 370 Lecture #25 11/6/2019 Lake life cycle Succession in lakes Oligotrophic Mesotrophic Eutrophic Other Dystrophic Hyper- eutrophic 3 CEE 370 L#25 David Reckhow Lake Eutrophication As lakes age, they become more productive Natural processes: natural Eutrophication Pollutant loading: cultural Eutrophication Limiting nutrient Liebig’s law of minimum Redfield Ratio C:N:P in most phytoplankton is 106:16:1 When P<16*N, it limit’s growth 4 CEE 370 L#25 David Reckhow Lecture #25 Dave Reckhow 2
CEE 370 Lecture #25 11/6/2019 Nutrient loading and Eutrophication 5 CEE 370 L#25 David Reckhow Estrogen lake study 6 CEE 370 L#25 David Reckhow Lecture #25 Dave Reckhow 3
CEE 370 Lecture #25 11/6/2019 Concern over drinking water Drugs? CEE 370 L#25 7 David Reckhow Organic Compounds: Types? Pharmaceuticals, etc Natural Compounds Anti-epileptics Fulvics Beta-blockers Proteins, carbohydrates, etc Domestic WW Organics X-ray contrast media Industrial Synthetic Organics antibiotics Plasticizers: phthalates Home & Personal Care Products solvents: tetrachloroethylene triclosan waxes: chlorinated parafins Musks, flame retardants others: PCB’s Endocrine Disrupters Hydrocarbons & oil derivatives Steroidal estrogens includes products of combustion: Natural process byproducts PAH’s Conjugated pharmaceuticals Agricultural Chemicals Engineered process byproducts pesticides: DDT, kepone, mirex disinfection byproducts, etc 8 CEE 370 L#25 David Reckhow Lecture #25 Dave Reckhow 4
CEE 370 Lecture #25 11/6/2019 Pollutant loss in lakes Photolysis Destruction by solar light energy Biodegradation Metabolism by microorganism Hydrolysis Chemical decomposition Volatilization Loss to the atmosphere Adsorption and settling Loss to particles that end up buried in sediments 9 CEE 370 L#25 David Reckhow Photolysis Chemical breakdown initiated by light energy two types direct photolysis sensitized (or indirect) photolysis Several steps some solar light reaches water surface some of this light penetrates to the solute some of this is absorbed by the solute some of absorbed light is capable of causing a reaction 10 CEE 370 L#25 David Reckhow Lecture #25 Dave Reckhow 5
CEE 370 Lecture #25 11/6/2019 Solar Radiation 11 CEE 370 L#25 David Reckhow Susceptible bonds? 12 CEE 370 L#25 David Reckhow Lecture #25 Dave Reckhow 6
CEE 370 Lecture #25 11/6/2019 Biotransformation Microbially mediated transformation of organic and inorganic contaminants Biochemical processes: Metabolism: toxicant is used for synthesis or energy Cometabolism: not “used”, but transformed anyway Chemical Effects: Detoxication: Toxic to Non-toxic mineralization Activation: Non-toxic to Toxic 13 CEE 370 L#25 David Reckhow Refer to lecture #17 Bio kinetics X Michaelis-Menten equation: k max m Y k c µ max = maximum growth rate (yr -1 ) s X=microbial biomass (#cells/m 3 ) Y= yield coefficient (cells produced per mass toxicant removed, #cells/µg) k s = half-saturation constant (µg/m 3 ) k b = rate of biotransformation (yr -1 ) If c<<k s , then: X k max k X m m 2 Yk s 14 CEE 370 L#25 David Reckhow Lecture #25 Dave Reckhow 7
CEE 370 Lecture #25 11/6/2019 Bio kinetics (cont.) Wide environmental range phenol: k m =4.0 d -1 OH diazinon: k m =0.016 d -1 C 2 H 5 S O CH 3 P O N CH O CH 3 Temperature correction C 2 H 5 N =1.04-1.095 CH 3 T 20 k k m m T 20 15 CEE 370 L#25 David Reckhow Hydrolysis Reaction with water and its constituents H 2 O k k h n OH - k k OH h b H + k k H h a Autodissociation K w OH H Combining: k k OH k k H h b n a or: K pH k k w k k 10 h b n a pH 10 16 CEE 370 L#25 David Reckhow Lecture #25 Dave Reckhow 8
CEE 370 Lecture #25 11/6/2019 Volatilization: The two film theory p g p i Interface c i c 17 CEE 370 L#25 David Reckhow Two film model Flux from the bulk liquid to the interface J K ( c c ) l l i Flux from the interface ot the bulk gas K Mass transfer g J ( p p ) g RT g i velocities (m/d) a And the K’s are related to the molecular diffusion coefficients by: D D l g K K l z g z l g 18 CEE 370 L#25 David Reckhow Lecture #25 Dave Reckhow 9
CEE 370 Lecture #25 11/6/2019 Whitman’s 2 film model (cont.) According to Henry’s law: p H c i e i And relating this back to the bulk concentration J p H l c i e K l now solving and equating the fluxes, we get: 1 1 RT a v K H K The net transfer v l e g velocity across the air- water interface (m/d) 19 CEE 370 L#25 David Reckhow Whitman’s 2 film model (cont.) H Which can be v K e v l K rewritten as: H RT l K e a g Now, applying it to Contaminant Environment specific specific toxicants p g 0 And converting to the v appropriate units: v k v H 20 CEE 370 L#25 David Reckhow Lecture #25 Dave Reckhow 10
CEE 370 Lecture #25 11/6/2019 Volatilization: Parameter estimation Liquid film mass transfer coefficient (d -1 ) Compound 0 . 25 32 K K molecular l l , O M 2 weight Gas film mass transfer coefficient (d -1 ) 0 . 25 18 K 168 U g W M Wind velocity (mps) 21 CEE 370 L#25 David Reckhow Toxics Model: CSTR with sediments Internal Transport Processes (between compartments) dissolved: diffusion particulate: settling, resuspension & burial Expressed as velocities (e.g., m/yr) Water (1) Settling (v s ) Resuspension (v r ) Diffusion (v d ) Mixed Sediments (2) Burial (v b ) Deep Sediments (3) 22 CEE 370 L#25 David Reckhow Lecture #25 Dave Reckhow 11
CEE 370 Lecture #25 11/6/2019 Functionally identical to M&Z equ# 3.32 Sorption 𝐿 � 𝑟 𝐷 C Linear Isotherm K particulat e C dissolved ' c c d p See M&Z, M s k ad section 3.10 Particle k de K k v s s 1 K Particle can then settle v s 23 CEE 370 L#25 David Reckhow Also in Lecture #16 biomagnification & Lecture #22 on groundwater retardation Octanol:water partitioning 2 liquid phases in a separatory funnel that don’t mix octanol water Add contaminant to flask Shake and allow contaminant to reach equilibrium between the two Measure concentration in each (K ow is the ratio) Correlate to environmental K K fn ( K ) ow 24 CEE 370 L#25 David Reckhow Lecture #25 Dave Reckhow 12
CEE 370 Lecture #25 11/6/2019 From Lecture #16 Bioaccumulation Mercury in food chain Data from Onondaga Lake Biomass Concentration (box size) (Shading) 25 CEE 370 L#25 David Reckhow From Lecture #16 Lab to Field Octanol water partition coefficients and bioconcentration factors 26 CEE 370 L#25 David Reckhow Lecture #25 Dave Reckhow 13
CEE 370 Lecture #25 11/6/2019 Completely-mixed lake or CMFR Often useful to assume perfect mixing same concentration throughout system Accumulation loading outflow reaction settling Outflow C C Loading Q C in reaction Q V settling 27 CEE 370 L#25 David Reckhow Other Terms in the Mass Balance Outflow Outflow Qc Reaction Re action kM kVc Settling J=vc Settling vA c s A s k Vc s Sediment- Note HW#6, water interface problem 2 v H V A H s k Since: s 28 CEE 370 L#25 David Reckhow Lecture #25 Dave Reckhow 14
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