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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
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
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
volatile suspended solids - vss
solids that can be volatilized (evaporated) and burned off when the tss are ignited - 500 +- 50 degrees
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
filtrate
product of filtration - a liquid or solid that has been passed through a filter
total solids formula
weight gain of crucible / x ml = ts
total suspended solids formula
weight gain of filter / x ml = tss
volatile suspended solids formula
weight loss of filter/ x ml = vss
total dissolved solids formula
wieght gain of crucible / x ml = tds
turbidity
measure of the light transmitting properties of water - how transparent water is
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
turbidity units
nephelometric turbidity units - ntu
treated water turbidity relationship
TSS [mg/L] = TSSf * T
tss - total suspended solids in mg/l
tssf - converting factors
turbidity in ntu
electrical conductivity
a measure of the ability of a solution to conduct an electrical current - ec proportions to ion concentrations
electrical conductivity units
millisiemens per meter - mS/m
water and minerals
when minerals dissolve in water, cations and anions are dissociated
ec and tds
electrical conductivity is a surrogate measure of total dissolved solids
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)
electroneutrality process
in water dissolved substances dissociate into charged ions
cations and anions - neutrality
the sume of positive ions (cations) must equal the sume of the negative ions (anions) in the solution
cations
positiviely charged speices in solution expressed in terms of equivalent per liter, eq/l or milliequivalent per liter, meq/l
anions
negatively charged species in solution, eq/l, or meq/l
electroneutrality
the number of equivalents related to how many electrons a species donates or accepts
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)
converting mol/l to eq/l
eq/l = mol/l * equivalent
concentration units
either in mol/l or eq/l or mg/l
converting mg/l to eq/l
eq/l = (mg/l) / equivalent weight
water hardness - total
total hardness is the summary content of calcium and magnesium
carbonate hardness
aka temporary water hardness is caused by the presence of carbonates and hydrocarbonates of calcium and magnesium
carbonate
carbonate is a salt of carbonic acid, characterized by the presence of a carbonate ion
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
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
concentration in miliequivalent/liter formula
meq/l = (concentration in mg/l) / (equivalent weight in g/eqv)
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)
pH
hydrogen ion concentration - pH = -log[H+]
pH and dissassociation
ph is connected closely with the extent to which water molecultes dissasociate - H2O ←> H+ + OH-
pH equilibrium constant
Kw = [H+][OH-]
organic compounds
carbon, hydrogen, oxygen, with nitrogen in some cases
wasterwater organic compounds
protein 40-60%, carbohydrate 25-50%, oils and fats
total organic carbon
measure of the total amount of carbon in organic compounds present in water
do
dissolved oxygen - the amount of oxygen dissolved in water, essential for life in aquatic environments
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
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
cod - chemical oxygen demand
indirect measure of the amount of oxygen consumed by chemical reactions / oxidation of organic matter in a sample/water
cod process
uses strong oxidizing chemical to oxidize organic matter
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
bod - biological oxygen demand
the amount of dissolved oxygen required by aerobic biological organisms to break down organic material in water
bod measurement conditions
typically measured at 20 degrees over 5 days, written as BOD5
BOD units
expressed in mg O2 per liter of sample
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)
bod vs cod
BOD < COD, since some organic matter is inert and not biologically degradable
relationship between theoretical do demand, bod and cod
toc→ theoretical do demand < BOD < COD
nitrogen in water
nitrogen from organic matter, and nitrogen from nitrogen compounds such as NH4 + and NO3 -
nitrogen
an essential nutrient for growth - many organic compounds contain nitrogen (all contribute to overall N in environment, water, wherever)
forms of nitrogen
Organic nitrogen (proteins, urea, etc.)
Inorganic: NH₄⁺, NO₂⁻, NO₃⁻
All contribute to nitrogen load in water
Conversion Factors (mg/L compound → mg/L N)
NH₃: × (14/17)
NH₄⁺: × (14/18)
NO₂⁻: × (14/46)
NO₃⁻: × (14/62)
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
Kjeldahl Nitrogen (TKN)
Sum of organic nitrogen + ammonia (NH₄⁺-N).
Does not include oxidized forms (NO₂⁻, NO₃⁻).
too much nitrogen
can be toxic - leads to euphication
euphication
Over-enrichment of water with nutrients (N, P).
Causes algal blooms, oxygen depletion, fish kills.
phosphorus
also an essential nutrient for growth
Orthophosphate: PO₄³⁻, HPO₄²⁻, H₂PO₄⁻, H₃PO₄ (bioavailable)
Polyphosphate (chains of phosphate)
Organic phosphate (bound in organic matter)
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
phosphorus cycle
Geological sources (mining, erosion)
Uptake by plants and microbes
Returned via decomposition
Fluxes: e.g. ~22 million tons/year mined
phosphorus as a solid
phosphorus is only possible as a praticle, as a solid - it does not exist in the atmosphere as a gas
phosphorus levels in environment
phosphorus more scarce than nitrogen
bioavailable P is limited
so in healthy water body, concentration should be low
phosphate mining
phosphate rock can release phospherus during mining
mined to give it to plants, used in fertilizer
Orthophosphate (PO₄³⁻-P)
Bioavailable form of phosphorus (directly usable by organisms).
Includes PO₄³⁻, HPO₄²⁻, H₂PO₄⁻, H₃PO₄.
Total Phosphorus (TP)
Orthophosphate + polyphosphate + organic phosphorus.
Important indicator of eutrophication potential.
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
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
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
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
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
dissolved oxygen in water - sources
Diffusion from atmosphere
Photosynthesis in water
DO sinks
Respiration by organisms
Oxidation of organic matter
Oxidation of reduced compounds (NH₄⁺, Fe²⁺, S²⁻, etc.)
control of DO
DO in water is controlled by both consumption (sinks) and aeration (sources)
ideal gas law
PV = nRT
gases common in water
O₂, N₂, CO₂ (natural)
NH₃, CH₄, Cl₂, H₂S (pollution/byproducts)
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)
partial pressure
Pressure exerted by one gas in a mixture.
Example: air = 21% O₂ → PO₂ = 0.21 atm.
partial pressure formula
partial pressure (p_i) = mole or volume fraction (ppm_v) * total pressure (p_total)
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
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)
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
cadmium
carcinogen, accumulates in liver/kidneys
chromium
carcinogenic and corrosive
lead
toxic, brain and kidney damage, birth defects
mercury
toxic to central nervous system, birth defects
living organisms in water
bacterial
fungi
algae
protozoa
viruses
organic pollutants in water
disinfection byproducts - DBPs
agircultural chemicals
emerging contaminants
disinfection byproducts
Formed when chlorine reacts with organic matter
Examples: Trihalomethanes (THMs), Haloacetic acids (HAAs)
agricultural chemicals
Pesticides, herbicides, fertilizers
emerging contaminants
Pharmaceuticals (antibiotics, prescription & non-prescription drugs)
Hormones (endocrine disruptors)
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
water treatment process
intake
chemical addition - chlorine, lime, alum (these chemicals facilitate coagulative process)
mixing
coagulation and flocculation
sedimentation
filtration
disinfection
storage
distribution
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)
colloids
need to be removed using coagulation