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Title: MS312: Sources of pollution Oxygen consuming wastes


1
MS312 Sources of pollution Oxygen consuming
wastes
  • What are oxygen consuming wastes?
  • Effluents from Sewage, Food Processing, Urban
    runoff
  • They are all rich in organic compounds
  • Many cause eutrophication and siltation

Read Clark Ch 3 Oxygen Consuming Wastes
2
Looking ahead
  • Oil Pollution
  • Heavy Metals
  • Pesticides, PCBs Halogenated hydrocarbons
  • Radioactivity
  • Dredgings, solids, plastics, heat
  • Case studies and guest speakers
  • Symposium Your investigations in Marine
    Pollution

3
Oxygen Demanding Wastes
  • Measurement of oxygen demand
  • Standard measure - 5-day BOD (biochemical oxygen
    demand)
  • Easily done - change initial oxygen concentration
    - final oxygen concentration, in the dark, at
    20oC
  • BOD ranges from about
  • 0-1 for uncontaminated natural waters,
  • 2-5 for forest and cropland
  • 100-300 Treated domestic sewage
  • 500 - 1000 for raw sewage
  • Food processing 750 mg/L
  • Paper mills 375 mg/L

4
Sewage, garbage, organic wastes
  • The major pollutant in most areas worldwide is
    just plain sewage.
  • This is especially so in the South Pacific, where
    there are few industrial sources.
  • In many places there is also very little water,
    so the problem of sewage is more difficult to
    solve

5
Sewage
  • Origin and characteristics
  • greywater vs blackwater
  • To treat or not to treat?
  • Primary treatment
  • Secondary treatment
  • Tertiary treatment
  • Ocean outfalls

6
Sewage treatment
primary
secondary
tertiary
7
Kinoya(also Raiwaqa) as an example of secondary
sewage treatment
primary clarifiers
trickling filters
humus tanks
digester
to sea
lagoon
in from sewer
sludge
drying beds
8
First and Second Stage Sewage treatment
Kinoya, May 2005 Primary Sludge
settling Secondary Trickling filter
9
Alternatives methods in sewage treatment
10
Sewage and public health
  • The common test for sewage pollution is an assay
    for faecal coliform bacteria.
  • Coliform bacteria are not usually harmful - but
    the indicate the potential presence of pathogens
  • Many bacteria and viruses can cause annoying
    diarrhea and skin infections.
  • A few, like the waterborne causative agents of
    cholera dysentery and typhoid fever are extremely
    serious.

11
Pathogens potentially waterborne and water
contact the list is long, and includes bacteria,
viruses, protozoa and helminths (parasites)
See on share files PathogensPotentiallyWaterborne
.doc and PathogensWaterContact.doc
12
Some important water borne pathogens
  • Bacteria
  • Aeromonas hydrophilia, Campylolbacter spp.
    Clostridium perfringens, E. coli, Francisella
    tularensis , Klebsiella pneumoniae, Plesionionas
    shigelloiides Pseudomonas aeruginosa , Shigella
    spp. All cause Diorrhea or Gastroenteritis
  • Staphylococcus aureus, Clostridium
    perfringens Wound and skin infections
  • Salmonella typhi Typhoid fever
  • Vibrio cholerae Cholera

13
Some important water borne pathogens ctd.
  • Viruses
  • Poliovirus Paralysis, encephalitis (not common
    because of vaccination)
  • Hepatitis A Infectious hepatitis type A
  • Protozoa
  • Giardia lamblia Giardiasis - mild, acute, or
    chronic diarrhea
  • And many more.

14
Contamination ofSuva Harbour - Creeks
15
Contamination of Suva Harbour - Shore
16
Kiribati is a case where there is little water,
and many people
17
FC in Kiribati is harming people and fisheries
Kelly, David J (1994) The effects of domestic
waste on marine and groundwater quality in Tarawa
Atoll, Republic of Kiribati. IAS, USP, Suva, Fiji
18
The great dead sea of New Jersey
19
The great dead zone of the Mississipi River
  • An anoxic zone is created in the bottom waters of
    the Mississipi River delta by runoff from sewage
    and agriculture
  • It varies according to river flow.

20
Organic wastes sugar cane and food processing
  • One major effect of organic wastes is oxygen
    depression.
  • In extreme cases, oxygen may be so low as to make
    life for fishes impossible.

21
Classic case oxygen in Thames River
22
The fish have returned!
23
Ba River and FSC Rarawai
24
Rainfall and river flow at Ba
25
Ba River oxygen
26
Ba River FC bacteria
27
Ba River surface oxygen
28
Urban runoff
  • In built-up areas of major towns, there is a high
    proportion of impermeable land (pavement,
    buildings).
  • This increases the flow of water directly to
    creeks and rivers.
  • The added flow, without benefit of percolation
    through the soil, carries with it a rich mixture
    of pollutants oil, heavy metals, pesticides,
    eroded soil.

29
Siltation
  • Land disturbance, whether from urban development,
    farming or logging, exposes the land to
    weathering and erosion.
  • When the land is near the sea, silt can be
    carried into the ocean.
  • There, it may blanket or smother filter feeding
    organisms.
  • Corals are especially susceptible to to the
    effects of siltation and eutrophication

30
Eutrophication
  • Too much of a good thing, is a bad thing!
  • The simple nutrients necessary to support
    photosynthesis can also cause overgrowth of
    plants.

31
Eutrophication - effects
  • Eutrophication causes changes community
    structure, mostly for the worse.
  • In extreme cases all oxygen may be consumed.
  • The bottom will then become anoxic.
  • An anoxic bottom is unable to support normal
    life.
  • Anoxia is accompanied by high H2S, which is
    toxic.
  • Long before the bottom becomes anoxic, plants
    (algae) will be encouraged to grow.
  • The algae overgrow corals, and the corals die.
  • Along with the corals, fish die or are replaced
    by less desirable species.

32
Eutrophication Effects on a Coral Reef Kaneohe
Bay, Oahu, Hawaii
  • Problem progressive deterioration of reef
  • Description of degraded ecosystem
  • Identification of causes
  • Intervention
  • Outcome
  • Lessons

33
Problem progressive deterioration of the reef
  • Setting NE coast Oahu
  • 1928 high natural, recreation value, and
    accessibility to population recognised.
  • 1945 corals abundant and diverse, some increase
    in biomass, productivity, localised replacement
    by Dyctyosphaera cavernosa (green bubble alga)

34
Edmondson in 1928
  • "Kaneohe Bay is one of the most favorable
    localities for the development of shallow water
    coral. Nearly all of the reef-formig genera known
    in Hawaii are represented and many species grow
    luxuriantly"
  • Edmondson, CH. 1928. Ecology of a coral reef.
    Bishop Mus. Bull. 45 (64p)

35
Kaneohe Bay Location
36
Description of degraded ecosystem
  • 1939-1963 population increase leads to
    construction of sewerage system, outfalls into SE
    bay.
  • 1965 major reef kill caused by high rainfall,
    rapid runoff
  • progressive anoxia in sediments, algal
    overgrowth
  • 1977 99.9 dead coral SE sector, benthos
    composed of detritivores and filter feeders.

37
Kaneohe Bay Progressive deterioration, and
recovery
38
Outcome and Lessons
  • What happened?
  • 1992 recovery substantially as 1988 (4 yr)
  • Low Salinity by itself less effect than
    nutrients and algae.
  • Recovery to pristine? Or to 1945?
  • Lessons
  • Algal growth encouraged by eutrophication is
    persistent (10yr)
  • FW damage to corals is intense but limited to
    upper layers, and recovery faster (4 yr)

39
Happy Coral Leeward Reef
40
Coral Eutrophication by Algae, Indonesia
41
Coral Algae Philipines
42
Coral Eutrophication
43
Coral Bleaching GBR
44
Coral Silted Philippines
45
Fijis Coral Coast a victim of its own success
  • Along Fijis Coral Coast, excess nutrients (N and
    P species) are causing eutrophication.
  • The Coral Coast (SE Viti Levu) has been developed
    as a mecca for tourism.
  • With tourism has come increased population,
  • increased incomes,
  • And flush toilets
  • The result is an overgrowth of Sargassum, a brown
    alga.

Islands Business and Fiji Islands
Business http//www.islandsbusiness.com/islands_bu
siness/
  • The sources are Villages, Piggeries and Resorts
    in that order.

46
Eutrophication REDOX Chemistry and Anoxia
,
  • Biological Oxygen Demand (BOD) is a measure of
    how much oxygen is consumed by living water,
    mostly bacteria and other microbes, over 4 days
    in the dark. It is a measure of respiration.
  • Typical Biological Oxygen Demand (BOD) Values
    (in mg O2 /L wastewater)
  • 0-1 for uncontaminated natural waters,
  • 2-5 for forest and cropland
  • 100-300 Treated domestic sewage
  • 500 - 1000 for raw sewage
  • Food processing 750 mg/L
  • Oxygen concentration in
  • HEALTHY WATER 6-8 mg/L (depending on water
    temperature
  • FISH ABSENT 2 mg/L

47
Degradation sequence Oxygen to H2S and Methane
  • What happens if O2 is exhausted, but there is
    still organic material present?
  • A succession of microbially (or chemically)
    mediated reactions happens next, and some have
    very important environmental consequences
  • 1. Aerobic Respiration
  • O2 CH2O CO2 H2O
  • Oxidation of organic matter by oxygen
  • Common in environments with plenty of O2
  • WHAT NEXT?

48
Next steps after oxygen
  • 2. DENITRIFICATION
  • 4NO3- 5CH2O 4H 5CO2 2N2 7H2O
  • 3. MANGANESE REDUCTION
  • 2MnO2(sw) CH2O 4H 2Mn2(aq) CO2 3H2O
  • May release toxic trace metals (Mn and
    associated metals)
  • Oxidation of organic matter using nitrate
  • 4. IRON REDUCTION
  • 4Fe(OH)3(s) CH2O 8H 4Fe2 (aq) CO2
    11H2O
  • May release toxic trace metals (Fe and metals)
  • May release phosphorous (a limiting nutrient)

49
And then
  • 5. SULFATE REDUCTION
  • 1/2 SO4-2 CH2O H ½ H2S CO2 H2O
  • Common in marine environments
  • Produces toxic hydrogen sulfide gas
  • Resulting sulfide minerals can scavenge metals
  • 6. METHANOGENESIS (FERMENTATION)
  • CH2O CH2O CH4 CO2
  • Common in severely eutrophicated waters, swamps,
    rice paddies, other flooded freshwater systems
  • Produces methane (an important greenhouse gas!)

50
End oxygen demanding wastes
  • The most important pollultion challenge facing
    the inshore areas of the world oceans are sewage
    and eutrophication
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