Defusing Africa's Killer Lakes
In a remote region of Cameroon, an international team of scientists takes extraordinary steps to prevent the recurrence of a deadly natural disaster
- By Kevin Krajick
- Smithsonian magazine, September 2003, Subscribe
(Page 4 of 6)
In addition, the scientists observed that a lakeside promontory had been stripped of vegetation to a height of 262 feet, presumably by a carbon dioxide-driven waterspout rocketing into the air. The explosion released a cloud of carbon dioxide—perhaps as much as a billion cubic yards, scientists estimate—that thundered over the lake's rim, hit Suley's family first and poured downhill at 45 miles per hour through two valleys and into the villages of Lower Nyos, Cha, Fang, Subum and, finally, Mashi, which is 14 miles from the lake.
Those on high ground survived. Afew individuals at lower elevations, like Suley, were spared for no apparent reason. The only other survivor in her family was her husband, Abdoul Ahmadou. He had been away on business in Wum that night. When he returned, it was to join his wife in burying their dead, then to flee to a refugee camp near Wum. Amid fears that the lake could erupt again, the military ordered out most of the region's survivors, around 4,000 in all.
The scientists began making frequent return trips to Cameroon, not only to study both Nyos and Monoun but also to make the region safe for people wishing to return. Testing of the lake depths showed that the explosions had not cleared all the pent-up carbon dioxide; indeed, the gas was accumulating at alarming rates. The researchers speculated that certain layers of Monoun, if left untouched, could become saturated with carbon dioxide by this year, and Nyos, sometime after. But either lake, even short of saturation, could explode at any moment.
The researchers considered various measures, such as blowing out the carbon dioxide by dropping bombs (too dangerous); dumping in massive quantities of lime in order to neutralize the gas (too expensive); or digging tunnels in the lake bed to drain the gas-laden bottom waters (way too expensive). In the end, they settled on a low-tech approach: running a pipe from the lake's deepest water layer to the surface, gradually releasing the gas to disperse quickly and harmlessly in the air. In theory, such a pipe, once primed, would carry the pressurized water from the depths and shoot it into the air like a natural geyser—a controlled explosion that could be sustained for years.
But not all researchers agreed that vent pipes would work. Geologist Samuel Freeth of the University of Wales, among others, speculated the process might set off a new explosion by spurting cold, dense bottom water onto the surface of the lake; the water would sink and create turbulence below. Even the researchers who advocated venting were worried, says Michel Halbwachs, an engineer from France's University of Savoy, who would design and install most of the equipment: "We were in an area [of science] little known and dangerous."
Using seed money from the European Union and private sources, a team headed by Halbwachs tested garden-hose-diameter pipes in Nyos and Monoun in 1990, then progressively larger pipes in 1992 and 1995. The experiment worked: the gas began venting. Halbwachs and coworkers were jubilant. Then the money ran out. The Cameroon government said it could not afford the $2 million to $3 million for permanent degassing installations. International aid agencies—more used to reacting to natural disasters than preventing them—did not grasp the concept. Kling, Kusakabe and others lobbied oil companies, governments and other organizations to pay for venting. Finally, in 1999, the U.S. Office of Foreign Disaster Assistance (OFDA) came up with $433,000 for a permanent pipe to be installed at Nyos.
By January 2001, the researchers had assembled rafts and piping at the site. Attached to a raft in the middle of the lake, a 5.7-inch-diameter pipe reached 666 feet to the deepest water layer. The Cameroon military provided emergency oxygen tanks for all workers in case of a rogue carbon dioxide release. After everyone retreated to distant high ground, Halbwachs pushed a remote-control button to activate a pump that primed the pipe. Within seconds a 148-foot spray shot into the sunlight at 100 miles per hour, and the small crowd let out a cheer. The degassing of LakeNyos had begun.
But with 5,500 tons of carbon dioxide still pouring into the lake annually, one pipe barely keeps up; Kling and Evans estimate it may take more than 30 years before enough dissolved carbon dioxide can be vented to make the lake safe. Five pipes, the researchers say, might do the job within five or six years—but so far funding has not materialized. The venting of the lake cannot happen too quickly, as far as locals are concerned. Families have begun drifting back into nearby hills, siting their compounds in high passes but venturing down to the forbidden zone by day. "You can't keep people out forever," says Greg Tanyileke of Cameroon's Institute for Geological and Mining Research. "We need to go faster."
Single Page « Previous 1 2 3 4 5 6 Next »
Subscribe now for more of Smithsonian's coverage on history, science and nature.









Comments (3)
I wonder if it's correct that the gas is "dissolved" if it can be released as a gas. A bigger problem with the article is confusing asphyxiation with carbon dioxide poisoning. Asphyxiation is caused by lack of oxygen. Carbon monoxide can cause asphyxiation because it has a higher affinity than oxygen for combining with haemoglobin, but elevated carbon dioxide cannot on its own cause asphyxiation if there is sufficient oxygen available. Carbon dioxide poisoning is more correctly described as hypercapnia (e.g. see this article http://www.pnas.org/content/108/40/16545.full relating to risks of carbon capture and storage).
Posted by Philip Machanick on January 8,2012 | 02:54 AM
Why of common sense was no autopsies performed?
Posted by Ryan on December 5,2009 | 09:27 PM
A very interesting story, and well written.
I have a point of disagreement with the theories put forth on what triggers the massive CO2 releases, however. The lakes named are meromictic and the bottom waters can stay still, and probably anaerobic, for centuries. In order for former tales of Nyos to have metamorphosed into myth, the period between cataclysmic releases must have been considerable. If that were true (quite a lengths of "if's", I admit), then the deep waters were not only fully saturated, but supersaturated. There comes a point when just an iota more of the highly pressurized CO2 will trigger the rest of the load.
I have read about this incident a number of times, and have decided that it is likely that the rockslide was triggered by the early stages of the explosion.
I think the solution manifested by safety teams was quite ingenious.
Posted by Parris ja Young on April 8,2009 | 07:53 PM