Water treatment

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163 Terms

1
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total solids (ts)

the residue remaining after a water sample has been dried at a specified temperature (103-105 degrees); ts = tss + tds

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total suspended solids - tss

portion of the total solids retained on a filter with a specified pore size, measured after being dried ata specified temperature - 105 degrees

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total dissolved solids - tds

portion of the ts in the filtrate (the liquid that went through the filter) after filtered using a filter with a specified pore size, measured after being dried at a specified temperature - 105 degrees

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volatile suspended solids - vss 

solids that can be volatilized (evaporated) and burned off when the tss are ignited - 500 +- 50 degrees

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6
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solid content determination process

  • crucible with filter at top

  • put sample volume ( x ml) of liquid into the filter and dry at approx 103 degrees

  • using total weight of crucible, total solids can be calculated

  • dry filter at 103 degrees as well

  • using weight gain of filter, tss can be calculated

  • after drying, place filter in furnace and ignite at 550 degrees

  • using weight loss of filter, vss can be calculated

  • place filtrate in crucible and dry at 103

  • using weight fain of crucible, tds can be calculated

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filtrate

product of filtration - a liquid or solid that has been passed through a filter

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total solids formula

weight gain of crucible / x ml = ts

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total suspended solids formula

weight gain of filter / x ml = tss

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volatile suspended solids formula

weight loss of filter/ x ml = vss

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total dissolved solids formula

wieght gain of crucible / x ml = tds

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turbidity

measure of the light transmitting properties of water - how transparent water is

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what is turbidity based on

based on comparison of the intensity of light scattered by a sample to the light scattered by a reference suspension under the same condition

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turbidity units

nephelometric turbidity units - ntu

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treated water turbidity relationship

  • TSS [mg/L] = TSSf * T

  • tss - total suspended solids in mg/l

  • tssf - converting factors

  • turbidity in ntu

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electrical conductivity

a measure of the ability of a solution to conduct an electrical current - ec proportions to ion concentrations

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electrical conductivity units

millisiemens per meter - mS/m

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water and minerals

when minerals dissolve in water, cations and anions are dissociated

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ec and tds

electrical conductivity is a surrogate measure of total dissolved solids

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ec and tds formula

TDS = EC * f

  • tds in mg/l

  • ec in dS/m

  • f value between 0.55 - 0.70 (depends on type of tds)

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electroneutrality process

in water dissolved substances dissociate into charged ions

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cations and anions - neutrality

the sume of positive ions (cations) must equal the sume of the negative ions (anions) in the solution

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cations

positiviely charged speices in solution expressed in terms of equivalent per liter, eq/l or milliequivalent per liter, meq/l

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anions

negatively charged species in solution, eq/l, or meq/l

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electroneutrality

the number of equivalents related to how many electrons a species donates or accepts

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equivalent weight

grams per equivalent - the molecular weight of the species divided by the number of equivalents in the species (g/mol divided by eqv/mol = g/eqv)

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converting mol/l to eq/l

eq/l = mol/l * equivalent

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concentration units

either in mol/l or eq/l or mg/l

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converting mg/l to eq/l

eq/l = (mg/l) / equivalent weight

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water hardness - total

total hardness is the summary content of calcium and magnesium

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carbonate hardness

aka temporary water hardness is caused by the presence of carbonates and hydrocarbonates of calcium and magnesium

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carbonate

carbonate is a salt of carbonic acid, characterized by the presence of a carbonate ion

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noncarbonate hardness

caused by the presence of Ca2+ and Mg2+ and anions like Cl- SO4 2- and NO3 -, which do not decompose and do not precipirate during boiling water 

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washing with hard water

hard water requires more sopat and detergents for home laundry/washing & contributes to scaling - because compounds in soap react with calcium in hard water and precipitate out as scum - only once all the calcium and magnesium ions have been precipitated out as scum, can the soap then lather up and remove grease

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concentration in miliequivalent/liter formula

meq/l = (concentration in mg/l) / (equivalent weight in g/eqv)

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hardness calculation

hardness is the total sum of concentrations of  ca2+ and mg2+ as miliequivalent/liter - (can also be expressed in mg/l as CaCO3 - calculate in meq/l and then multiply by 50g of caco3/eqv)

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pH

hydrogen ion concentration - pH = -log[H+] 

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pH and dissassociation

ph is connected closely with the extent to which water molecultes dissasociate - H2O ←> H+ + OH-

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pH equilibrium constant

Kw = [H+][OH-]

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organic compounds

carbon, hydrogen, oxygen, with nitrogen in some cases

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wasterwater organic compounds

protein 40-60%, carbohydrate 25-50%, oils and fats

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total organic carbon

measure of the total amount of carbon in organic compounds present in water

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do

dissolved oxygen - the amount of oxygen dissolved in water, essential for life in aquatic environments

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theoretical do demand

for e.g. carbon dioxide, tells us how much oxygen would be required to fully oxide all organic carbon into co2 - do demand for co2 = 32/12 * toc

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real do demand

Lower than theoretical because:

  • Biological use of DO < 100% efficient

  • Other elements (e.g., nitrogen) also consume DO

  • Some TOC is inert and not biologically available

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cod - chemical oxygen demand

indirect measure of the amount of oxygen consumed by chemical reactions / oxidation of organic matter in a sample/water

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cod process

uses strong oxidizing chemical to oxidize organic matter

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cod vs theoretical do

cod is generally greater than the theoretical oxygen demand, bcs it accounts for all chemically available sources - even those not biodegradable

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bod - biological oxygen demand

the amount of dissolved oxygen required by aerobic biological organisms to break down organic material in water

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bod measurement conditions

typically measured at 20 degrees over 5 days, written as BOD5

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BOD units

expressed in mg O2 per liter of sample

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bod measurement method

take two samples

  • test one immediately for dissolved oxygen

  • incubate the other at 20 deg in the dark for 5 days, then test for do

  • the difference = BOD (in mg/L)

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bod vs cod

BOD < COD, since some organic matter is inert and not biologically degradable

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relationship between theoretical do demand, bod and cod

toc→ theoretical do demand < BOD < COD

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nitrogen in water

nitrogen from organic matter, and nitrogen from nitrogen compounds such as NH4 + and NO3 -

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nitrogen

an essential nutrient for growth - many organic compounds contain nitrogen (all contribute to overall N in environment, water, wherever)

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forms of nitrogen

  • Organic nitrogen (proteins, urea, etc.)

  • Inorganic: NH₄⁺, NO₂⁻, NO₃⁻

  • All contribute to nitrogen load in water

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Conversion Factors (mg/L compound → mg/L N)

  • NH₃: × (14/17)

  • NH₄⁺: × (14/18)

  • NO₂⁻: × (14/46)

  • NO₃⁻: × (14/62)

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nitrogen cycle

  • Plants absorb nitrate from soil → build proteins

  • Animals eat plants → nitrogen in biomass, nitrogen is passed to animals

  • Waste & decay → ammonia (ammonification) - nitrogen from protein is returned to the environment as ammonia

  • Bacteria convert ammonia → nitrite (NO₂⁻) → nitrate (NO₃⁻) (nitrification)

  • Under anoxic conditions: nitrate → N₂ gas (denitrification) . denitrifying bacteria convert nitrates to molecular nitrogen

  • Atmospheric nitrogen goes through biological nitrogen fication and ends up in soil, etc. - nitrogen can exist in solid form

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Kjeldahl Nitrogen (TKN)

  • Sum of organic nitrogen + ammonia (NH₄⁺-N).

  • Does not include oxidized forms (NO₂⁻, NO₃⁻).

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too much nitrogen

can be toxic - leads to euphication

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euphication

  • Over-enrichment of water with nutrients (N, P).

  • Causes algal blooms, oxygen depletion, fish kills.

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phosphorus

also an essential nutrient for growth

  • Orthophosphate: PO₄³⁻, HPO₄²⁻, H₂PO₄⁻, H₃PO₄ (bioavailable)

  • Polyphosphate (chains of phosphate)

  • Organic phosphate (bound in organic matter)

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phosphorus in water

  • too much phosphorus stimulates a lot of plant growth

  • if TP is too high, there is high risk of algea bloom (eutrophication)

  • > 0.03 mg TP/l in river - eutrophication

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phosphorus cycle

  • Geological sources (mining, erosion)

  • Uptake by plants and microbes

  • Returned via decomposition

  • Fluxes: e.g. ~22 million tons/year mined

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phosphorus as a solid

phosphorus is only possible as a praticle, as a solid - it does not exist in the atmosphere as a gas

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phosphorus levels in environment

  • phosphorus more scarce than nitrogen

  • bioavailable P is limited

  • so in healthy water body, concentration should be low

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phosphate mining

  • phosphate rock can release phospherus during mining

  • mined to give it to plants, used in fertilizer

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Orthophosphate (PO₄³⁻-P)

  • Bioavailable form of phosphorus (directly usable by organisms).

  • Includes PO₄³⁻, HPO₄²⁻, H₂PO₄⁻, H₃PO₄.

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Total Phosphorus (TP)

  • Orthophosphate + polyphosphate + organic phosphorus.

  • Important indicator of eutrophication potential.

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C:N:P Ratio

Typical nutrient balance for microbial growth = 100 : 7.2 : 1.

  • phospherus is generally the limiting nutrient preventing exponential growth as there is not enough of it bioavailable

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carbon cycle

Carbon moves between atmosphere (CO₂), biosphere (plants/animals), hydrosphere (dissolved carbon), and geosphere (rocks/fossil fuels).

  • Photosynthesis: CO₂ → organic matter

  • Respiration & Decomposition: organic matter → CO₂/CH₄

  • Combustion: fuels/biomass → CO₂

  • Sedimentation/Fossilization: long-term storage in rocks & fuels

  • Human impact: burning & deforestation add extra CO₂ → climate change

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phosphurus cycle 2

Phosphorus cycles through rocks, soil, water, and organisms (no gas phase).

  • Weathering of rocks → phosphate (PO₄³⁻) released

  • Assimilation: plants/animals use phosphate for ATP, DNA, membranes

  • Decomposition: organic P → inorganic phosphate

  • Sedimentation: phosphate locked in rocks/sediments long-term

  • Human impact: mining phosphate rock for fertilizer → excess P in water → eutrophication

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nitrogen cycle 2

Nitrogen cycles between atmosphere (N₂), soil, water, plants, and animals.

  • Fixation: N₂ → NH₄⁺ (by bacteria/industry)

  • Nitrification: NH₄⁺ → NO₂⁻ → NO₃⁻

  • Assimilation: plants/animals use nitrogen for proteins/DNA

  • Ammonification: organic N → NH₄⁺

  • Denitrification: NO₃⁻ → N₂ (back to atmosphere)

  • Human impact: fertilizer use, wastewater → eutrophication

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lack of oxygen in water

if too many algae grow, they use up all the oxygen in the water body and the fish die and suffocate

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dissolved oxygen in water - sources

  • Diffusion from atmosphere

  • Photosynthesis in water

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DO sinks

  • Respiration by organisms

  • Oxidation of organic matter

  • Oxidation of reduced compounds (NH₄⁺, Fe²⁺, S²⁻, etc.)

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control of DO

DO in water is controlled by both consumption (sinks) and aeration (sources)

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ideal gas law

PV = nRT

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gases common in water

  • O₂, N₂, CO₂ (natural)

  • NH₃, CH₄, Cl₂, H₂S (pollution/byproducts)

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things that determine amount of gas in water

  • solubility of the gas defined by henry’s law

  • the partial pressure of the gas in the atmosphere

  • the temperature

  • the concentration of the impurities in water (e.g. sailinity, suspended solids)

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partial pressure

  • Pressure exerted by one gas in a mixture.

  • Example: air = 21% O₂ → PO₂ = 0.21 atm.

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partial pressure formula

partial pressure (p_i) = mole or volume fraction (ppm_v) * total pressure (p_total)

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henry’s law

The amount of gas dissolved in water is proportional to its partial pressure above the water.

  • Higher pressure → more gas dissolves

  • Higher temperature → less gas dissolves

  • Solubility also affected by salinity and impurities

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henry’s law formula

[Gas]=KH​×Pgas​

  • [Gas] = dissolved concentration (mol/L)

  • Kₕ = Henry’s Law constant (mol/L·atm)

  • Pgas = partial pressure of the gas (atm)

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heavy metals in water

toxic even at low concentrations, many are priority pollutants - pose risk because they are persistent, bioaccumulate, toxic to humans and ecosystems

  • cadmium

  • chromium

  • lead

  • mercury

  • other: copper, iron, manganese, nickel, zinc

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cadmium

carcinogen, accumulates in liver/kidneys

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chromium

carcinogenic and corrosive

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lead

toxic, brain and kidney damage, birth defects

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mercury

toxic to central nervous system, birth defects

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living organisms in water

  • bacterial

  • fungi

  • algae

  • protozoa

  • viruses

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organic pollutants in water

  • disinfection byproducts - DBPs

  • agircultural chemicals

  • emerging contaminants

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disinfection byproducts

  • Formed when chlorine reacts with organic matter

  • Examples: Trihalomethanes (THMs), Haloacetic acids (HAAs)

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agricultural chemicals

Pesticides, herbicides, fertilizers

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emerging contaminants

  • Pharmaceuticals (antibiotics, prescription & non-prescription drugs)

  • Hormones (endocrine disruptors)

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water treatment

to remove undesired or add desired water constituents to meet the required water quality for:

  • drinking water

  • domestic wastewater

  • industrial wastewater

different or same technologies and processes could be applied to remove different constitutentswater

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water treatment process

  • intake

  • chemical addition - chlorine, lime, alum (these chemicals facilitate coagulative process)

  • mixing

  • coagulation and flocculation

  • sedimentation

  • filtration

  • disinfection

  • storage

  • distribution

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size of substances in water & filtering

water molecule is approx 0.27 nanometers - most particles bigger than that, so one possibility is to use a nano sized filter - then mostthings can be removed but water can still pass through (tho is quite costly) 

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colloids

need to be removed using coagulation

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