# Mazuku

Mazuku (Swahili for "evil winds") are pockets of dry, cold carbon dioxide-rich gases released from vents or fissures in volcanically and tectonically active areas, and mixed with dispersed atmospheric air and accumulating in typically low-lying areas. Since CO$_2$ is ~1.5 times heavier than air, it tends to flow downhill, hugging the ground like a low fog and gather in enclosed spaces with poor ventilation, such as lava tubes, ditches, depressions, caves, house basements or in the stratified water layers of meromictic lakes if a water column exists. In high concentrations (≥1vol.%), they can pose a deadly risk to both humans and animals in the surrounding area because they are undetectable by olfactory or visual senses in most conditions.
Mazuku primarily occur on northern shores of Lake Kivu on both sides of the twin towns of Goma in the Democratic Republic of the Congo (DRC) and Gisenyi in Rwanda where local communities in these areas use this term in their vernacular (Kinyabwisha language) to describe the dangerous gases. They believe mazuku occur in cursed locations where invisible forces that travel unnoticed often silently kills people during the night when they are sleeping. In many mazuku places, CO$_2$ levels fall during daytime but can rise to significantly dangerous concentration levels of about 90% at night, early mornings or evening hours posing great threat. This is because during nighttime, the atmospheric temperature drops, and wind speeds are significantly reduced. These conditions hinder the rapid dispersal of these heavy gases into the atmosphere, allowing them to accumulate in lower-lying areas, such as valleys and depressions.

## Geological setting and occurrence

The East African Rift System (EARS) is formed by the divergence of three ancient cratonic plates: the Somalian plate, the Nubian plate, and the Arabian plate, which are splitting apart due to the influence of a mantle plume beneath them. The rift extends ~4,000 km, starting from the Afar triple junction in the northern Ethiopian Plateau and running southwards. It is divided into two main segments: the volcanically active Eastern branch, ~45Ma which passes through Djibouti, Eritrea, Kenya, and northeastern Tanzania, and the younger, seismically active Western branch, (~5 and 8Ma), that cuts through the Democratic Republic of the Congo (DRC), Uganda, Rwanda, Burundi, southwestern Tanzania, Zambia, Malawi, Zimbabwe and terminates at the Okavango Delta in Botswana. The rifting process is responsible for the tectonic and volcanic activity in East Africa, leading to the formation of deep rift lake basins e.g. Lake Tanganyika, Lake Malawi, Lake Rukwa, Lake Albert and Lake Kivu as well as frequent natural disasters such as earthquakes, volcanic eruptions, and massive landslides, along with prolonged dry CO$_2$-rich gas emissions like mazuku (toxic gas) releases.
It has been observed that most mazukus are found along the Western branch of the EARS, particularly in areas of active volcanic and tectonic activity. These areas include:
* Virunga Volcanic Province (VVP) at the foot hills of volcanic mountains of Nyamulagira and Nyiragongo, on the northern shoreline part of Lake Kivu particularly on the busy city centers of Goma and Sake on the Democratic Republic of Congo (DRC) and Gisenyi city in Rwanda.
* Rungwe Volcanic Province (RVP) in southwestern Tanzania, at the intersection of three rift segments (Tanganyika-Malawi-Usangu rifts, forming a triple junction), where CO$_2$ is mined commercially by TOL Company Limited for supply to the beverage industry.

## Formation

Geologically, mazuku are natural CO$_2$ emissions linked to magmatically and tectonically active regions, such as young and active or dormant volcanic systems, active hydrothermal systems and deep fault structures systems. Isotopic signature from He and C gases analyses has confirmed that the origin of mazuku is mainly magmatic, as opposed to being derived from thermal decomposition of organic matter. These gases are temporarily trapped and stored in subsurface pockets, such as lava tubes formed during previous eruptions and remain isolated from the rest of the surrounding hydrothermal system. Over time, they are released following porous pathways and channeled to the surface through a network of extensional fissures, faults, or fractures. Once at the surface, they accumulate in cavities or in low-lying areas (depressions) due to their densities and the influence of gravity. In meromictic lakes e.g. Lake Kivu, Lake Nyos and Lake Monoun the CO$_2$-rich gases remain trapped in the dense, cold, and anoxic stratified lower layers (monimolimnion), which do not mix with the O$_2$-rich surface layers (mixolimnion) due to density discrepancies.
In the anoxic zones, methanogenic bacteria converts CO$_2$ into CH$_4$ through a process called methanogenesis, whereby over time, both CO$_2$ and CH$_4$ accumulate under extremely high pressure creating a potential future limnic eruption disaster. However, CH$_4$ is currently extracted economically in Lake Kivu through degassing which reduces the risk of a dangerous limnic eruption while providing a valuable energy source for power generation. Mazuku can extend up to 100m in length and cover an area of up to 4,700m$^2$ e.g. the mazuku of Bulengo Seminaire on the shores of Lake Kivu, DRC and it has been observed that there is a strong correlation between the occurrence and location of mazuku with the regional alignment of tectonic faults and fracture network.

## Geochemical composition and origin

The bulk geochemical composition of the CO$_2$-rich dry gases in mazuku consists of a mixture of variable proportions of other atmospheric components, such as N$_2$, O$_2$, and Ar, with smaller amounts of CH$_4$, H$_2$S and water vapour. These gases contain between 12% and 99% CO$_2$, Ar concentrations range from 0.01% to 0.85%, and CH$_4$ concentrations range from 0.0002% to 0.002%. Helium is also present in low concentrations, ranging between 0.0003% and 0.004%.
The isotopic signature of He-Ar and CO$_2$ systematics identify mazuku's sources as being derived from both mantle (magmatic sources) and/or crustal origins with significant potential secondary modification processes such as magma mixing and solubility-driven degassing fractionation). The dry gases are continuously released very slowly through a passive degassing mechanism from the earth's interior via vents, fractures, cracks, and hot springs, fumaroles, gas plumes without the need/presence for an active volcanic eruption

### Surface manifestations

Areas with mazuku can be readily identified in the field through several distinctive characteristics/features as follows:
* The peculiar types and species of vegetation that thrive in CO$_2$-rich waters and gases, such as cyperus papyrus, fern, reeds and poaceae serve as indicators of the mazuku environments
* Burnt-out vegetation and altered rocks due to high acidity levels associated with elevated CO$_2$ concentrations normally (70-90v.%) results in patches of weathered bareland, which is a typical feature for identifying mazuku areas.
* Regions with ultrahigh CO$_2$ concentrations, the high CO$_2$/O$_2$ ratio can be perceived as a sensation of heat on human skin, a condition related to hypercapnia. This includes tingling and burning sensations in the mouth lips, eyes and nose because of the acidic nature of CO$_2$ which reacts with moisture to form a weak carbonic acid that causes irritation and a burning sensation in these soft body parts
* Systematic occurrences of dead animals, such as insects, rodents and reptiles alongside larger animals like cattle, dogs, and goats indicate areas of high CO$_2$ concentration.
* Bulging and swelling of the ground due to pressure caused by CO$_2$ accumulation. These characteristics collectively aid in the identification of mazuku regions in the field

### Factors affecting CO$_2$ levels in mazuku

CO$_2$ levels in mazuku areas are affected and influenced by a combination of various factors:
* Increased volcanic and seismic activities: Increasing CO$_2$ concentration levels in mazuku areas may be influenced by an increasing amount of volcanic and seismic activities (e.g. earthquakes) which can result to creation of more permeable fractures in the earth's crust allowing more CO$_2$ to escape from underground leading to the formation of new degassing zones with higher CO$_2$ levels
* Anthropogenic activities
** Unauthorized well drilling: For instance, at Colli Albali volcano in Italy, a well was dug through a pressurized gas pocket and exploded which created a low-pressure zone leading to more CO$_2$ gas dispersion in the area and resulted to further 3 more gas blowouts along a continuous fault line
** Tarmac roads construction: Tarmac roads and other concrete surfaces can seal natural gas conduits, blocking the natural flow of gas and leading to its accumulation. As pressure builds up due to the trapped gases, it can cause bulging and swelling and subsequently explosive release (gas blowout) when the gas eventually escapes, this can cause a road collapse or any other infrastructure damage
** Drilling of pit latrines: A man died from asphyxiation near the foothills of Ngozi volcanic crater, in the Rungwe Volcanic Province in Tanzania while digging a 6m deep pit latrine. The cause was likely due to the accumulation of hazardous gases in the hole after the gas pockets was mechanically disturbed. However, CO$_2$ continuously degasses in the area to date, leading to more deaths of birds, cows, and rodents due to the toxic gas buildup (personal communication)
* Weather conditions and atmospheric influences (meteorological parameters)
** Pressure: Pressure variations in the atmosphere has an inverse relationship with CO$_2$ emissions from the soil, i.e. when the atmospheric pressure drops, the CO$_2$ emissions are high but when pressure rises the CO$_2$ emissions are lower
** Wind speed: Low wind speed decreases the chance of CO$_2$ dispersion to the atmosphere and this causes the heavy gases to accumulate in low-lying areas like valleys and depressions
** Soil moisture content and season of the year: During heavy winter rains, subsurface soil voids are totally filled with water, causing a significant amount of CO$_2$ to dissolve in them. In contrast, during summer, when the soil is dry, these voids remain empty and can accumulate large amounts of degassed CO$_2$ that would escape and fill in the low lying depressions areas posing great health threat
** Time of a day: At night, with no solar radiation and reduced solar intensity, atmospheric temperatures drop, and wind speeds decrease significantly. These conditions slow the dispersal of heavy gases, causing them to accumulate in low-lying areas like valleys and depressions. During the day, sunlight heats the air, creating low pressure that allows CO$_2$ emissions to rise and disperse, reducing the risk of dangerous concentration levels

## CO$_2$ exposure health effects and International Guideline Limits

The health hazards linked to both short-term and long-term exposure of lethal doses of CO$_2$ in mazuku are outlined in the table below, along with permissible exposure limits (PELs) for CO$_2$ to promote safety in workplaces and for residents near active volcanic areas. These limits specify safe exposure durations at various concentrations to help prevent health risks over time.
| CO$_2$% Concentration mixed with air | Short term exposure effects | Long term exposure effects | Average time of exposure |
| 0 - 1.5% | Mostly unnoticed by olfactory or visual senses | Over a longer exposure time it can be noticeable with developed conditions as shortness of breath, lightheadedness and dizziness | 8 hours maximum exposure |
| 1.5 - 6% | Difficulty in breathing, increase heart beat rates, dyspnoea, shortness of breath | Tingling sensations in lips, eyes and nose because of the acidic nature of CO$_2$ which reacts with moisture to form a weak carbonic acid that causes irritation and a burning sensation in these soft body parts | Only 15 minutes maximum exposure time |
| 6 -10% | Dizziness, buzzing sound in ears, lightheadedness, muscular and joint weakness, drowsiness, headaches, sweating, shortness of breath, low mood and mental distress, fainting, shortness of breath and increased heart rate (heart pounding) | Long term exposure of can result into dizziness and unconscious | Tolerable within a span of several minutes |
| 11–15% | A victim suffers severe abrupt muscle contractions because body cells lack enough oxygen for respiration and subsequently becomes unconscious within few seconds | Severe muscle cramps and loss of consciousness | Death in less than a minute |
| ˃25% | This is an intolerable amount of CO$_2$ for full function of a human body, generally a victim suffers convulsions, coma and finally death | Convulsions, coma and finally death | Death in less than a minute |

## Mazuku hazard case studies else where around the world

Here is a list of "mazuku" case studies from various parts of the world, where volcanic or geologically active regions release CO$_2$-rich gases. These gases accumulate in low-lying areas, valleys, or confined spaces or in the stratified water layers of meromictic lakes, creating hazardous conditions and deadly asphyxiation zones for humans, wildlife, and plants across different continents.

### Lake Monoun

Lake Monoun, volcanic crater lake is situated in the Oku Volcanic Field which is part of the Cameroon Volcanic Line and was formed when a lava flow created a natural barrier. In 1984, the lake experienced a deadly gas exsolution, triggering a violent limnic eruption that claimed the lives of 37 people. The primary source of the gas was volcanic CO$_2$ emissions, confirmed by C-isotope signatures, which had accumulated in the lake's stratified waters over time, leading to increased pressure. Seismic activity and an underwater landslide were responsible for the disturbance of the lake's stratification, releasing the trapped CO$_2$ violently and causing a very dangerous gas outburst.

### Lake Nyos

A similar scenario occurred two years later in 1986 at Lake Nyos, another crater lake in Cameroon, often referred to as a "killer lake". The lake experienced a catastrophic limnic eruption also known as a lake overturn which resulted in the sudden release of a massive amount of CO$_2$, leading to deaths of 1,700 people and 300 cattle.
Geologically, the crater lake sits over a network of active faults and lineaments and is being fed by volatile-rich basaltic dikes underneath. These dikes release magmatic gases/volatiles like CO$_2$ and H$_2$O which upon their release at low pressure, likely contributed to a phreatomagmatic explosive eruption that formed a diatreme beneath the lake and a maar depression on the surface.
Normally, mazuku involves dry CO$_2$ gas seeping through fissures and accumulating in low-lying areas before dispersing into the atmosphere. However, when gas columns are obstructed by rock strata, such as thick pyroclastic deposits or stratified lake water e.g. meromictic lakes, the gases remain trapped or dissolved in the lake waters respectively. In the later case, CO$_2$-rich gas accumulated in the Lake Nyos crater lake waters to significant levels under extreme pressure
It is believed that landslide event was the triggering factor responsible for exsolution of the dissolved gases which caused a limnic eruption. As a result, a massive CO$_2$ cloud (of about (98v.% CO$_2$) rose from the lake's floor at about 208m, spreading over and down the valleys, engulfing the nearby villages and killing everything along the way due to asphyxiation. The event was classified as a lake overturn which is a very rare phenomenon where dissolved volcanic gases are released from the stratified bottom layers of lakes after a mechanical disturbance

### Mammoth Mountain

Mammoth Mountain, a dormant volcano in the Sierra Nevada region of California, United States, is underlain by a shallow dacitic dome that releases cold and dry CO$_2$-rich gases (98v% CO$_2$) through fumarolic vents and fractures located on the flanks of the mountain. The gas fluxes were estimated at a rate of ~1,200 tonnes/day, comparable to gas fluxes observed at the summit craters of Kīlauea in Hawaii, Mount Etna in Italy, and Mount St. Helens in Washington. The CO$_2$ originates from deeper magmatic sources (evidence from He-CO$_2$ isotopic signature), at about 10 km below the surface, traveling through permeable networks of fractures and faults. The CO$_2$-rich gases accumulates in the soil layers at depths between 0.6-1m, closed subsurface cavities and snow caves, suggesting an ongoing active magmatic activity beneath the mountain.
One visible consequence/manifestation of this toxic degassing is the large-scale mortality of coniferous trees, covering an area of up to 100 hectares on the mountain's flanks. The accumulation of CO$_2$ in closed depressions and subsurface soil layers exposes tree roots to toxic gases, leading to widespread tree death. In addition to CO$_2$ poisoning, the trees are affected by highly altered and acidic soils. The region also experiences frequent earthquakes, often with up to magnitudes of 6 on the Richter scale. These seismic events, combined with the mountain's bulging and exhumation, fracture the surface and allow high-pressure volatiles to escape, further contributing to the release of CO$_2$ in the tree-kill zones.

### Mount Amiata

Mt. Amiata is a dormant volcano located in Tuscany, Central Italy, and it is known for its significant emissions of dry and cold CO$_2$-rich gases, which are primarily magmatic in origin. The gases originate from the deep geothermal system beneath the volcano and pass through a permeable network of faults and fractures by passive mechanism degassing processes. Although the area has not experienced recent volcanic eruptions, it remains geothermally active, with CO$_2$ emissions contributing to environmental risks like soil acidification and potential CO$_2$ build-up in low-lying areas, posing hazards to local wildlife and humans. The region is also notable for its significance in geothermal energy production, and gas emissions are closely monitored to assess both volcanic hazards and energy sustainability.

### Mount Sinila

Mt. Sinila is a volcanic mountain located on the Diëng Plateau in Indonesia. In 1979 it experienced a tragic phreatic eruption disaster when a mixture of steam, lahar and toxic gases were released from the open cracks and fissures located near the crater and gushing down the valley asphyxiating insects, rodents, big animals like goats, dogs and cows as well as claiming lives of 172 people. Before the eruption, the area experienced a series of earthquakes which reactivated ancient fractures over the span of a few hours. After few hours during the main course of eruption, dry gas was emitted from a 1000m long new fissure which had emerged on the western flank of the volcano near Sumur crater. Gas analysis revealed that the dry gas was CO$_2$-rich from magmatic sources, with concentrations reaching up to 99% by volume. Since CO$_2$ is heavier than air, it flowed down the valley, displacing oxygen and hugging the ground like fog. All victims were found dead in a linear path of gas flow, likely caught them off guard as they slept, with the gas suffocating them simultaneously.

## Effects

Mazukus can cause a variety of effects on flora and fauna in the regions in which they occur depending on the composition and concentration of the gases that they consist of. Massive clouds of CO$_2$, such as those released from lakes in the 1980s, can cause widespread devastation of human and wildlife populations. However, they may have little or no effect on local vegetation. If the concentration of CO$_2$ is high enough and maintained in a prolonged outgassing event, even vegetation can be affected by the mazuku, as is the case on Mammoth Mountain in California, United States, where deforestation has occurred as well as CO$_2$ poisonings, including the deaths of two skiers, one in 1995 and one in 1998.
In some cases, mazuku are large enough to cause a localized flora and fauna extinction events that is documented in the fossil record. For-example, sediment core radiocarbon dating record from Lake Kivu have shown a sequence of repeated and regular massive lake overtuns events circa.0.8kyr that were caused by methane explosions and tsunamis due to accumulation of magmatic CO$_2$.
If mazuku occurs underneath bodies of water e.g. lakes, it can lead to changes in water chemistry, creating meromictic lakes making it dangerous for aquatic life. For example, the buildup of CO$_2$ in Lake Kivu, Nyos and Monoun caused stratification and oxygen depletion, affecting fish and other organisms living in the water.

### Summary

| | Country | Volcanic edifice | Year the Hazard Occurred | State of the volcano | CO$_2$ release events | CO$_2$ concentration measured | Environmental effects | Casualties |
| 1 | Democratic Republic of the Congo (DRC) and Rwanda | Virunga Volcanic Province Mt. Nyiragongo and Mt. Nyamulagira | 1900s to present | Active | Dry CO$_2$ degassing | 90% | Acidic soil, dead of animals due to ˃500 000 ppm of CO$_2$ in the soil | ~13 deaths per year |
| 2 | Democratic Republic of the Congo | Virunga Volcanic Province Lake Kivu | 1900s to present | Active | Diffuse outgassing of CO$_2$ into the lake water | ˃25% | Water chemistry alteration, habitat disruption, loss of biodiversity | Dizziness, and convulsions lead to drowning of 2 swimmers A potential future catastrophic limnic eruption |
| 3 | Cameroon | Cameroon Volcanic Line Lake Monoun | 1984 | Active | Limnic eruption/Lake Overturn | 96.73% | Water chemistry alteration, habitat disruption, loss of biodiversity | 37 people died |
| 4 | Cameroon | Cameroon Volcanic Line Lake Nyos | 1986 | Active | Limnic eruption/Lake Overturn | 98% | Water chemistry alteration, habitat disruption, loss of biodiversity | 1700 deaths |
| 5 | United States | Mt. Mammoth Mountain | 1998 | Dormant | Dry diffuse CO$_2$ through the soil | 98% | Acidic soil, barren land ~100 hectares in a tree-kill area and dead animals | A skier died from acute pulmonary edema in a snow cave with ~98% CO$_2$ |
| 6 | Indonesia | Diëng Plateau Mt. Sinila | 1979 | Dormant | Phreatic eruption | 99% | Tree kill zones due to acidic soils, dead reptiles and rodents | 172 people died |
| 7 | Tanzania | Rungwe Volcanic Province Mt. Rungwe Mt. Ngozi | 2001, 2004 and 2022 | Dormant | Dry CO$_2$ degassing | 95% | Tree kill zones due to acidic soils, dead reptiles and rodents | 1 man died when he was digging a pit latrine 2 men died when fell into a ditch (personal communication) |
| 8 | Italy | Vulcano Island | 1980 | Active | Diffuse CO$_2$ on mountain flanks | 50% | Tree kill zones due to acidic soils, dead reptiles and rodents | 2 children died from asphyxiation |
| 9 | Italy | Lazio and Alban Hills | 2000 | Dormant | Dry diffuse CO$_2$ through the soil | 92.7% | Tree kill zones due to acidic soils, dead reptiles and rodents | 1 man died when he fell into an abandoned well |
| 10 | Italy | Alban Hills (Colli Albani) Cava dei Selci | 2011 | Dormant | Dry diffuse CO$_2$ through the soil | 99% | Dozens of cow and pets are killed by inhaling toxic gases Gas blowouts, ground swells and roads collapses | 3 people died in an open Spa |
| 11 | Japan | Hakkoda | 1997 | Dormant | Dry diffuse CO$_2$ through the soil into depressions | 15-20% | Bare land and a pattern of dead animals were observed | 3 soldiers died after falling into a depression |
| 12 | Portugal | Furnas, Sao Miguel, Azores | 1999 | Active | Dry diffuse CO$_2$ through the soil | 99% | Tree kill zones due to acidic soils, dead reptiles and rodents | 3 people died from asphyxiation in house cellars and a well |

## Hazard assessment and mitigation
### Hazard assessment

The areas experiencing mazuku emissions are facing with multiple forms of hazards due to their proximity to active volcanoes. These include:

#### Continuous hazards

These are long lasting volcanic hazards that persist for extended periods of time, even without an active volcanic eruption. For instance, in regions near active volcanoes, such as the Virunga Volcanic Province, people, livestock, and wildlife in low-lying areas are silently killed by mazuku gases. These gases flow downhill and accumulate in depressions, displacing oxygen and causing suffocation. The danger from mazuku remains constant, posing a long-term threat to communities living in these volcanic zones
Long-term exposure to mazuku can lead to environmental degradation and loss of biodiversity.
Agricultural lands may be impacted by CO$_2$ accumulation in subsurface layers of soils, creating toxic acidic soil leading to crop failures and economic disruption.

#### Latent hazards

Latent hazards are dormant threats that require an external trigger to become dangerous and deadly under specific conditions e.g. a mechanical disturbance. For-example; dissolved gases in meromictic lakes like Lake Nyos, Lake Kivu and Lake Monoun contains enormous amounts of dissolved carbon dioxide (CO$_2$) and sometimes methane (CH$_4$) in their deep stratified layers (monimolimnion). This presents a latent hazard because, under normal conditions, these gases remain trapped in the lower layers of the lake. However, if triggered by an external mechanical disturbance as volcanic activity, an earthquake, or landslide, a limnic eruption (also known as a lake overturn) could occur, releasing a cloud of these gases explosively. This could lead to widespread asphyxiation and fires across the surrounding regions, putting millions of people at risk.
Also, mazuku may indicate deeper magmatic unrest, posing further natural disasters as earthquakes, volcanic eruptions and massive landslides.

### Mitigation measures

Due to the silent (colorless and odorless) and deadly nature of CO$_2$ in volcanic active areas, authorities must plan for combating this natural hazard and utilize all available resources to mitigate the hazardous effects associated with it. Some of the mitigation measures are;
On ground CO$_2$ detection sensors: Early warning systems should be installed in high-risk areas. For-example at Mt. Amiata in Italy, researchers employ soil CO$_2$ flux sensors to measure diffuse CO$_2$ emissions with a notable flux measurement of about 13,000 tons/day
Volcano Geoengineering technologies: Human-induced degassing technologies should be employed in meromictic lakes to prevent the sudden natural release of gases. For instance, at Lake Nyos, siphons were installed to lower gas pressure by extracting CO$_2$-rich water from the lake's bottom saline layers (monimolimnion). This process enables the dissolved carbon dioxide to escape into the atmosphere as the water rises to the surface. By reducing the concentration of dissolved gases, this method decreases the risk of catastrophic limnic eruptions, like the one happened in 1986. The siphon system effectively promotes controlled gas exsolution, preventing dangerous pressure build-up. Land-use planning: Town planners should indicate buffer zones which are prone to mazuku and prevent settlements in these areas.
Reallocation and closing high CO$_2$ concentrated areas: For essential community safety, there should be an immediate evacuation plans and putting warning signs in hazardous places.
Developing gas hazard and risk maps is essential in volcanic areas prone to mazuku. Key data on CO$_2$, such as soil gas concentrations, carbon isotopes (which help trace CO$_2$ sources), and CO$_2$ flux levels, should be collected. Mapping these areas through gas concentration and flux measurements can be of a great help during construction and settlement allocation decisions
Education and Sensitization campaigns: There should be continued scientific research on CO$_2$ emissions in volcanic active regions that includes creation and improvement of existing CO$_2$ dispersion models on the causes and occurrence of mazuku.

## Mazuku's influence on climate

* Volcanic mountains e.g. Mount Etna in Italy, Kilauea in Hawaii, Nyiragongo and Nyamulagira in Congo, and their adjoining areas are significant sources of magma-derived gases, releasing massive amounts of CO$_2$ both during eruptions and through continuous magma upwelling (passive degassing) in non-eruptive states through fumaroles, hot springs and gas plumes (mazuku). During active eruptions, they can emit up to 6.18 x 10⁵ tons of CO$_2$ per day. However, during their non-eruptive period (during quiescence), for instance Mt. Etna in Italy is still passively degassing and it can emit around 137 tons of CO$_2$ per day. The cycling of CO$_2$ and other gases, such as SO$_2$, H$_2$S, water vapor and HCl is driven by magma convection, where degassed magma sinks, recharges with CO$_2$ at depth, and rises again, ensuring a constant supply of volatile-rich magma a process likely fueled by a mantle source beneath
* By doing so they contribute to global warming primarily through their large continuously (nonstop) emissions of CO$_2$ fluxes, (a greenhouse gas). During both quiescence and high eruptive activity periods the volcanoes releases significant amounts of CO$_2$ into the atmosphere. The continuous release and accumulation of CO$_2$ (accounting for up to 10% of the global total budget) leads to an increase in the concentration of greenhouse gases in the atmosphere. This gas acts like a blanket, trapping heat that would otherwise be re-radiated into space, causing the heat to accumulate and, as a result, warming the Earth's surface. Although volcanic CO$_2$ emissions are relatively small compared to human-caused emissions from burning fossil fuels, the persistent degassing of volcanoes like Mt. Etna still plays a role in the overall carbon cycle, indirectly contributing to climate change by increasing the amount of CO$_2$ in the atmosphere.