To define limnic eruption we can say that it is a physical phenomenon in which gas erupts from the depths of a body of water to the surface and threatens to strangle wild animals, livestock, and people. A limnic eruption is characterized by the chemical composition, mass, and origin of gases, the duration of the release, and the “trigger” of the catastrophe. Such gas emissions can cause tsunamis in the reservoir due to the displacement of water by rising gas. Scientists believe that landslides, earthquakes, and volcanic activity can lead to a limnological catastrophe.
Do you want to know what causes eruption and how long does a limnic eruption lasts? A limnological disaster is a rare natural disaster that is a sudden release of a large volume of dissolved carbon dioxide from an open body of water.
Being heavier than air, carbon dioxide collects in low-lying places, including in the vicinity of a reservoir, causing suffocation in people and animals who find themselves there, until after a while (hours, sometimes days) it is scattered by the wind.
A degassing limnic eruption can be caused by an earthquake, an underwater volcanic eruption, large-scale underwater or near-water avalanches, the penetration of lava flows into a reservoir, and other catastrophic events. The emission itself can cause a tsunami in the reservoir if the gas cloud displaces the water in it, which is why the catastrophe is also called “turning the lake”.
The conditions necessary for the occurrence of limnological disasters can be created by the release of carbon dioxide (CO2), injected into deep geological strata for long-term storage. Gas entering open water bodies can be of magmatic (Nyos and Monun), biogenic (Kivu), or technogenic (pumped for long-term storage) origin.
A limnological catastrophe is a physical phenomenon, a mandatory component of which is destructive for people and gas emissions from an open reservoir. Limnological characteristics of the chemical composition, mass, and origin of gases, the continuation of the gas release, the “descent mechanism” of the catastrophe.
To date, two lacustrine limnological disasters have been registered:
The trigger of a limnological catastrophe is characterized by composition, the arrangement of constituent parts, and mass transfer. Limnological catastrophes can be triggered in various combinations:
A typical example of a limnological catastrophe is presented by the catastrophes in Cameroon:
August 15, 1984, at Lake Manun, which killed 37 people.
On August 21, 1986, on Lake Nyos, which killed 1,746 people and about 3,500 head of livestock. The conditions necessary for the occurrence of limnological disasters exist not only in the lakes of Cameroon but also in other open bodies of water on our planet, for example:
Blocking the triggering mechanism prevents a limnological catastrophe.
The way to block the activation of the “trigger” can be:
Natural disasters of a hydrological nature are destructive and sometimes unpredictable. Knowledge of the causes and nature of natural disasters allows, with early adoption of protective measures, with reasonable behavior of the population, to significantly reduce all types of losses. Thus, efforts are needed not only by special rescue services to save people, but also the citizens themselves, who are in the disaster zone, in order to save themselves and their loved ones. Take action, do not panic.
The Worst Natural Disaster In the Indian Ocean: 2004 ...
Wow! Heatwave Of 2003 Facts: What Should You Know About ...
The Biggest And The Deadliest Floods: Our TOP-5 Famous ...