Gina M. Barrier, Director Northwest Outreach Office The Science House North Carolina State University

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Gina M. Barrier, Director Northwest Outreach Office The Science House North Carolina State University www.science-house.org

Outreach program of the College of Sciences, NC State University Established in 1991 Programs serve 5,000 teachers and 36,000 students annually

The Science House Mission Cultivate. Educate. Innovate. www.science-house.org 10/3/12 NOSC, Tuscaloosa, Oct. 2011

Outreach to North Carolina for 20 Years

What do we do? Teacher Professional Development Equipment Loan Curriculum Development and Dissemination FREEDM IMHOTEP Photonics NC Science Olympiad

CASE STUDIES Case studies have mainly been used in medical, business, and law school. Case Studies involve self-contained, relevant, short stories that pose a dilemma. Skills: Role-playing Debate / Discussion / Communication Analytical / Critical-Thinking / Problem-solving Teamwork / Cooperation / Leadership Research Skills

Inquiry-Based Learning As Defined By The Science House Inquiry is an ongoing cyclical process in which a learner questions investigates analyzes discusses shares results Learners develop habits of mind to extract and construct meaning, connecting past knowledge and current experiences with future applications.

A KILLER LAKE National Center of Case Study Teaching in Science (http://ublib.buffalo.edu/libraries/projects/cases/ubcase.htm) In 1986, Lake Nyos, a volcanic lake located in Cameroon, Africa, released a huge amount of gas resulting in the deaths of 1,700 people and their livestock.

Topics Covered Chemistry Gas solubility Density Solutions Vapor pressure Gas Laws Physics Behavior of Gases Pressure Earth/Environmental Limnology Volcanic lakes Biology Aquatic Life Asphyxiation

Limnology Lake + Knowledge The study of inland waters: Lakes Ponds Rivers Streams Wetlands Groundwater"

POST-IT BIN Read the article provided by your teacher. As you are reading, use the post-it notes provided to collect questions and post them here.

Use the Graphic Organizer provided to sequence the story! Village of Lower Nyos, Cameroon, Africa Milla had been in the highlands Late summer Weather had been warm and dry, now temperature was cooler and it had rained night before no insects, biting flies, or mosquitoes Dead cow- carcass wasn t warm, no rotting smell, no decomposers Villagers seemed to have died in their sleep Blue around the lips Elders told of Lake Monoun 2 years ago. 37 people died of asphyxiation when a cloud of gas erupted from the lake and moved along the ground. Volcanic activity had caused the carbon dioxide stored in the bottom layer of the lake to escape. Milla visited the Elders who stayed on higher ground outside the village 1700 people died in the valley below the lake Milla remembered his grandmother s story of the Water Mammies Water had an odd rust color and vegetation was floating on surface Bottom-water sample retrieved from Van Dorn Bottle bubbled violently when brought to the surface. Conducted a vertical profile of lake to collect temp, ph, and conductivity data

K W L A

Temp and Conductivity Profiles

http://waterontheweb.org/under/lakeecology/05_stratification.html

Lake Nyos is layered. K W L A What is causing the layering? CO 2 gas may be building up in Lake Nyos. The water sample from the bottom of the lake bubbled when brought to the surface. The CO 2 gas escaped from the lake water. The CO 2 cloud caused the deaths in the village. It could happen again. How would CO 2 affect the water in Lake Nyos? Why did the water sample bubble so violently when brought to the surface? What may have caused the CO 2 gas to escape? Why did the CO 2 cloud kill life in the village but not Milla and the Elders? How could we protect the other villages around these lakes from future eruptions?

Station # 1 Question: Why is Lake Nyos layered or stratified? Inquiry: Have students brainstorm reasons for density differences and devise an experiment to test their hypothesis. 1A - Temperature 1B - Dissolved gases

Temp and Conductivity Profiles Monimolimnion (lowest layer) of water is warmer than the epilimnion (top layer). Monimolimnion has a higher conductivity than the layers above it. Density differences in Lake Nyos are caused by a higher concentration of salts or gases.

Station # 2 Question: How would CO 2 affect the water in Lake Nyos? Inquiry: Have students identify some changes that may occur when CO 2 gas dissolves in lake water and devise an experiment to test their hypothesis. 2A - Conductivity 2B - ph

Conductivity increased as more CO 2 reacted with the water. CO 2 + H 2 0 <=> H 2 CO 3 H 2 CO 3 <=> H + (H 3 O + ) + HCO 3 - Conductivity is greatest in the monimolimnion possibly indicating higher levels of CO 2.

ph = - log [H 3 O + ] H 2 CO 3 <=> H 3 O + + HCO 3 - Monimolimnion is most acidic indicating higher levels of CO 2

Station # 3 Question: Why did the water sample from the bottom of the lake bubble when brought to the surface? Inquiry: Identify differences between the water at the bottom of the lake and the water at the top of the lake that may affect the dissolving of CO 2 in the water. Pressure Gas solubility

Increased Pressure at bottom of lake increases CO 2 solubility

Henry s Law At a given temperature, the solubility of a gas in a liquid is directly proportional to the partial pressure of the gas in equilibrium with the liquid. In the lake, hydrostatic pressure from the top layers of water would be exerted on the lower layer to keep the CO 2 dissolved in solution.

K W L A Lake Nyos is layered. What is causing the layering? Temperature and dissolved gases or salts can cause a difference in density. Lake Nyos is a freshwater lake, so dissolved salts may not be a major factor. The most dense layer (warm water or a high concentration of dissolved salts or gases) will be at the bottom. The temperature difference from top to bottom is minimal. The lake must be layered due to density differences as a result of dissolved gases. CO 2 gas may be building up in Lake Nyos. How would CO 2 affect the water in Lake Nyos? When CO 2 dissolves in and reacts with water the - conductivity increases - ph decreases The ph is lowest and the conductivity is highest in the lowest layer of the lake. So, the CO 2 must be concentrated in the lowest layer. The water sample from the bottom of the lake bubbled when brought to the surface. Why did the water sample bubble so violently when brought to the surface? Pressure is greatest at the bottom of the lake. Gases are more soluble under pressure. CO 2 is held in solution by the hydrostatic pressure of the upper layers of water.

Station #4 Question: What may have caused the CO 2 gas to escape from the lake water? Inquiry: Develop a procedure to extract gas from solution. The CO2 eruption brought up lower waters rich in iron which were oxidized to give the lake waters a red-brown color. Courtesy of J. P. Lockwood, USGS.

CO 2 erupts from the lake Possible Triggers: Landslide Earthquake Explosion Volcanic eruption on lake bed Heavy rain on one side of lake None (supersaturated)

Station #5 Question: Why did the CO 2 cloud kill life in the village but not Milla and the Elders? Inquiry Option: Build a model of Lake Nyos to investigate the behavior of CO 2 gas.

Since CO 2 is denser than air and stays close to ground, it traveled down the mountain following the valleys suffocating the villagers and their animals along the way.

Station # 6 Question: How could we protect the other villages around Lake Nyos from future eruptions? Inquiry Option: Build a model to solve this problem.

The Degassing Tube Tube is placed vertically in lake. A pump initiates water flow. As water rises, lower pressure in the tube allows the gas to escape from solution forming bubbles. The natural buoyancy of the gas bubbles draws the water up the tube in a self-sustaining manner.

K W L A The CO 2 gas escaped from the lake water. What may have caused the CO 2 gas to escape? Gas can be extracted from solution by - shaking - providing nucleation sites - adding more solute to a supersaturated solution - Heating the solution Limnologist s suspect - geologic activity (tremor) - landslide - gas-rich volcanic eruption - heavy rains on one side of lake forcing it to turn over so that cold water sinks and warm water rises The CO 2 cloud caused the deaths of life in the village. Why did the CO 2 cloud kill life in the village but not Milla and the Elders? CO 2 stays in the bottom of the aquarium CO 2 will displace the O 2 in the air and suffocate flames. CO 2 cloud traveled down the mountain because it was more dense than air CO 2 displaced the oxygen in the air suffocating the villagers Could it happen again? How could we protect the other villages around Lake Nyos from future eruptions? The higher pressure on the surface of the liquid forced it up the straw. The buoyancy of the bubbles drew the solution up the straw in a self-sustaining manner. Degassing Tubes inserted in the deepest layers of the lake will allow the CO 2 to escape over time.

Application Pick ONE of the following concepts: Density of Liquids Density of Gases Water Quality Effects of Pressure on Solubility Effects of Temperature on Solubility Effects of Concentration on Solubility Diffusion Apply the concept you chose to TWO other situations found in life.

To Contact Us Gina M. Barrier, Director Northwest Outreach Office The Science House NC State University Gina_Barrier@ncsu.edu