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Limnic Eruptions

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Title: Limnic Eruptions


1
Limnic Eruptions
  • By Corney Crumbley
  • Denisse Iacobucci
  • April Williams

2
Limnic Eruption
  • When CO2 builds up in the bottom of a lake.
  • The water becomes saturated with CO2.
  • Require trigger such as a landslide, volcanic
    eruption, explosion, and even a rain storm to
    create an eruption.
  • followed by a release of CO2 into the air causing
    death by asphyxiation.

3
Very Rare
  • Though very dangerous there are only two know
    cases.
  • One was in Cameroon, Africa at Lake Monoun in
    1984, which killed 37 people.

4
Second known event
  • At Lake Nyos in Cameroon as well. It erupted in
    1986, and was larger in size killing 1700 to 1800
    people!!!
  • Released 80 million cubic meters of CO2
  • Most wildlife was killed, including fish in the
    eruptions.

5
Third possible Eruption
  • Another lake is showing signs of a possible
    Limnic Eruption!
  • Lake Kivu in Africa has been known for violent
    lake overturns in the past.
  • There is evidence of massive biological
    extinction happening every 1,000 years
  • These three lakes have been called exploding
    lakes!!!
  • Lake Kivu is the largest of the three lakes and
    near the most populated area!!!

6
Why?
  • Why do you think that Limnic Eruption are so
    rare?
  • Specific conditions need to be met.
  • Most temperate lakes turn over yearly causing
    water temperature to change in each layer.
  • Dont worry the Great Lakes or Lake Altoona will
    never do this!
  • Soon you will see how Temperature effects this
    process

7
Conditions for an Eruption
  • Conditions for CO2 accumulation must be met
    first.
  • The conditions for a Limnic eruption are
  • Need a CO2 source. Can be volcanic activity or
    organic degradation
  • Degradation only contributes not really a cause
    (Volcanic activity).
  • Need high amount of pressure present.
  • CO2 dissolves at higher pressure and lower Temp,
    such as the bottom of a deep lake.

8
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9
Eruption
  • Once the conditions are met, the possibility for
    an eruption greatly increase.
  • What happens is similar to opening a shaken can
    of soda on a horribly large scale.
  • An Eruption causes a violent displacement of
    water and could cause a Tsunami!
  • An Eruption can be looked at in step ward
    fashion.
  • 7 steps of an Limnic Eruption

10
Eruption Cont.
  • Once the water becomes saturated with CO2 due to
    mostly volcanic activity,
  • a trigger causes saturated water to rise.
  • As the water rises, less dense water cause
    dissolved CO2 to become released in the form of
    bubbles.
  • The bubbles natural buoyancy causes more
    saturated water to rise to the surface.
  • CO2 bubbles start being released more rapidly and
    cause more saturated water to rise faster.
  • Soon a huge displacement of water takes place
    releasing CO2 into the air.
  • The water displacement can cause Tsunami!

11
Aftermath
  • Once an eruption takes place so much CO2 is
    released that a CO2 cloud sits over the land.
  • This cloud does not rise!
  • The reason the cloud does not rise is due to the
    density of CO2. CO2 is 1.98 g/L at stp which is
    greater than oxygen which is 1.43 g/L at stp.
    Thus, CO2 sinks to the ground.

12
Aftermath cont..
  • The CO2 that is released kills wildlife and
    people in the area. The speed of this natural
    disaster makes it so dangerous.
  • Most things caught in wake of a Limnic eruption
    is killed by asphyxiation.
  • Surviving a Limnic eruption is possible but
    causes many problems.
  • Brain damage and breathing problems occurs
    because of the large amounts of CO2 and other
    gases.

13
Tsunami
  • A Tsunami happens when a huge body of water is
    rapidly displaced.
  • A Limnic eruption is a perfect example.
  • Imagine a huge rock being dropped into a puddle
    and how huge water ripples move toward the
    outside.
  • A 5-meter Tsunami was reported after the Eruption
    at Lake Nyos.

14
Human Reaction
  • CO2 reacts with water molecules in the blood to
    form H2CO3. Then HCO3- and H are formed. The H
    ion increases the acidity of the blood. This
    increase in acidity harms a persons ability to
    further take up oxygen, which can lead to death.
  • Reaction
  • CO2 H2O ? H2CO3? H (acidic) HCO3-

15
Human reaction
  • The human body undergoes a state of hypercapnia
    (a condition in which too much CO2 is in the
    blood) otherwise known as CO2 poisoning.
  • Symptoms include rapid breathing, flushness of
    the skin, raised blood pressure, and
    unconsciousness followed by death!

16
 
17
No Oxygen
  • Dynamics within the human body change overtime
    and quickly with the loss of oxygen

 
The following symptoms take place within 6
Minutes !!
18
Other Symptoms
  • Some believe that there are other gases that
    cause further damage to people caught in Limnic
    eruptions.
  • Hydrogen Chloride (HCL) - was also thought to be
    released because of change in skin color.
  • Most depute this claim and believe other
    environmental factors are the cause.
  • Carbon monoxide (CO) - which was blamed for
    blisters on patients skin caused by poor oxygen
    levels.

19
Carbon Monoxide
  • Know as carbon monoxide poisoning
  • Due the inhalation of carbon monoxide.
  • Flu like symptoms, vertigo, headache, and
    blisters on skin.
  • Long term effects cause problems to the central
    nervous system, heart, and the fetus. If not
    treated quickly death is certain.
  • Treatment involves the use of 100 pure oxygen or
    hyperbaric treatment.

20
Prevention Methods
  • Limnic Eruptions in a highly populated area could
    be a catastrophe.
  • In January 2001, Cameroonian and French
    scientists installed a pipe in Lake Nyos to
    release the gas in safe amounts.
  • Makes Cool Fountains ?
  • Comes with a threat.

21
Degassing
  • The process of removing CO2 threatens lakes.
  • Very effective process (on small lakes)!
  • A siphon is used to pump water from the bottom of
    the lake to the top to remove CO2.
  • Requires little energy
  • Process requires little energy because as the CO2
    saturated water rises bubbles are formed.
  • These bubbles natural buoyancy causes water to
    rush out in a rapid fashion forming a fountain.

22
Drawbacks
  • A Thin layer of CO2 could be released above the
    lake.
  • A thin layer would be a biological disaster,
    killing all life within the lake.
  • Would be a mini Limnic eruption.
  • This process is good on small lakes only.
  • Larger lakes could cost millions to degas.
  • Pipes and electronics need constant maintenance
    due to the acidic water.
  • Caused by dissolved CO2

23
Pipe Corrosion
  • CO2 reacts with H2O to form Carbonic acid (H2CO3)
  • CO2 H2O ? H2CO3 ? H HCO32-
  • When Carbonic Acid comes in contact with steel
    (Fe), the following corrosion reaction occurs.
  • Fe 2H2CO3 ? Fe(HCO3)2 H2
  • 2Fe(HCO3)2 ½ O2 ? Fe2O3 4CO2 2H2O

24
Next possible threat
  • Lake Kivu meets the condition for a Limnic
    eruption
  • Has shown to erupt in the past
  • 2,000 times bigger than Lake Nyos
  • Over 2 million people live off the shores
  • Lake contains methane. An eruption would mean a
    huge release of explosive gas.
  • Too expensive for the local economy to degas
  • Remember expensive to degas large lakes plus all
    draw backs increase!

25
Recap
  • Limnic eruption is when CO2 suddenly rises from a
    lake.
  • Rare needs specific set of conditions
  • Eruption causes huge displacement of water.
  • Tsunamis
  • CO2 cloud sits over lake killing surrounding area
    by CO2 poisoning.
  • Due to density
  • The human body can survive without oxygen for
    about 6 minutes.
  • Degassing is the method of prevention.
  • Many draw backs
  • Lake Kivu is the next possible disaster.
  • 2,000 times larger than Lake Nyos and 2 million
    people live around it.

26
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