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 3 of 6)
Carbon dioxide is also a natural by-product of geologic processes, the melting and cooling of rock. Most of the time it's harmless, surfacing and dispersing quickly from vents in the earth or from carbonated springs—think San Pellegrino water. Still, CO2 poisonings have occurred in nature. Since Roman times, vented carbon dioxide in volcanic central Italy occasionally has killed animals or people who have wandered into topographic depressions where the heavy gas pools. At YellowstoneNational Park, grizzly bears have met the same fate in a ravine known as Death Gulch.
Sigurdsson, after a few weeks, began to conclude that carbon dioxide from magma degassing deep under LakeMonoun had percolated up into the lake's bottom layers of water for years or centuries, creating a giant, hidden time bomb. The pent-up gas dissolved in the water, he believed, suddenly had exploded, releasing a wave of concentrated carbon dioxide. He wrote up his findings, calling the phenomenon "a hitherto unknown natural hazard" that could wipe out entire towns, and in 1986, a few months before the Nyos disaster, he submitted his study to Science, the prestigious U.S. journal. Science rejected the paper as far-fetched, and the theory remained unknown except to a few specialists.ThenLake Nyos blew up, killing 50 times more people than at Monoun.
word of the nyos disaster spread quickly around the world. In Japan, a government official awakened Minoru Kusakabe of OkayamaUniversity at 1 a.m., inquiring if the geochemist would be willing to go at once to Cameroon. Kusakabe did not even know where the country was. French volcanologists; German, Italian, Swiss and British scientists; U.S. pathologists, geologists and chemists—all would converge on Nyos. Many departed from home so precipitously that they carried little more than a briefcase, a change of clothes and whatever scientific instruments they could grab. Among the Americans was limnologist (lake scientist) George Kling of the University of Michigan, who, as it happens, was making his second visit to the remote location. While studying the chemistry of Cameroonian lakes for his doctoral thesis the year before, he had sampled Nyos' waters from the shore because he didn't have access to a boat. The shallow water had yielded no hints of the dangerous gas in the depths. Now, a year later, the local boy who had guided him along the lake was dead, along with nearly everyone else he had met. "I was numb," recalls Kling. "I had always dreamed of going back there, but not like this."
Arriving within days of the disaster, the scientists themselves were fearful; no one was sure what had just happened—or if it was about to happen again. The Cameroon military had buried human victims in mass graves. Thousands of cattle lay dead, their carcasses bloated and decomposing. Heavy rains fell. Only the survivors' hospitality alleviated the grimness. They took the researchers into their houses and cooked meals of corn mush over open fires. "Can you imagine that?" says Kling's research partner, geochemist Bill Evans of the U.S. Geological Survey. "These people had just lost everything, and they were worried about us."
The scientists motored out onto Nyos in inflatable dinghies to take water samples and look for clues. Once again, some assumed that an underwater volcano had erupted. But others immediately grasped that the villagers around Nyos had perished under the same conditions previously documented at Monoun—that Sigurdsson's "unknown natural hazard" was real.
Over ensuing weeks and months, scientists would piece together the Nyos story. The crater lake is extraordinarily deep (682 feet) and rests atop a porous, carrot-shaped deposit of volcanic rubble—a subaqueous pile of boulders and ash left from old eruptions. Carbon dioxide may remain from this old activity; or it could be forming now, in magma far below. Wherever it comes from, underwater springs apparently transport the gas upward and into the deep lake-bottom water. There, under pressure from the lake water above, the gas accumulates; pressure keeps the CO2 from coalescing into bubbles, exactly as the cap on a seltzer bottle keeps soda from fizzing.
If the lake were farther north or south, seasonal temperature swings would mix the waters, preventing carbon dioxide buildup. Cold weather causes surface waters to become dense and sink, displacing lower layers upward; in spring, the process reverses. But in equatorial lakes like Nyos and Monoun, the deep layers seldom mix with top layers; indeed, the deepest layers may stagnate for centuries.
But something must have detonated the built-up carbon dioxide that August night 17 years ago. One theory is that boulders crashing into the lake (perhaps the rockslide Ephriam Che heard) set it off; the scientists at Nyos noted that an adjacent cliff face bore signs of a fresh rockslide. Or a fluky drop in air temperature, causing surface water to cool and abruptly sink, might have been the trigger, or a strong wind that set off a wave and mixed the layers. Whatever the cause, water saturated with carbon dioxide was displaced upward from the depths; as it rose and pressure lessened, dissolved carbon dioxide bubbled out of solution, and the bubbles drew more gasladen water in their wake, and so on, until the lake exploded like a huge shaken seltzer bottle. (The explosion, they determined, had also brought up iron-rich water, which oxidized at the surface and turned the lake red.)
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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