Nitrogen returns to the atmosphere primarily through the process of denitrification, where anaerobic bacteria convert nitrates in the soil back into nitrogen gas (N₂) or nitrous oxide (N₂O). This gas is then released into the atmosphere. Additionally, the decomposition of organic matter also contributes to this process, as it releases nitrogen compounds back into the soil, which can subsequently be denitrified. Overall, these natural processes help maintain the nitrogen cycle and balance atmospheric nitrogen levels.
Carbon is returned to the atmosphere through processes like respiration by living organisms, decomposition of organic matter, and combustion of fossil fuels. When organisms respire, they release carbon dioxide back into the atmosphere. Decomposition of dead organic matter also releases carbon dioxide, while burning fossil fuels releases carbon that has been stored underground back into the atmosphere.
Carbon is returned to the atmosphere through several processes, including respiration, combustion, and decomposition. During respiration, living organisms release carbon dioxide as they break down glucose for energy. Combustion of fossil fuels and biomass also releases stored carbon into the atmosphere as CO2. Additionally, the decomposition of organic matter by microbes and other decomposers releases carbon back into the atmosphere.
Carbon dioxide is returned to the atmosphere primarily through processes such as respiration by animals and plants, decomposition of organic matter, and combustion of fossil fuels. Additionally, natural events like volcanic eruptions and wildfires also release CO2. Human activities, particularly industrial processes and deforestation, significantly contribute to increased carbon dioxide levels in the atmosphere.
Carbon is returned to the atmosphere primarily through processes such as respiration, decomposition, and combustion. During respiration, animals and plants release carbon dioxide (CO2) as they convert glucose and oxygen into energy. Decomposition of organic matter by microbes also releases CO2 as they break down dead plants and animals. Additionally, the burning of fossil fuels and biomass for energy contributes significantly to the release of carbon back into the atmosphere.
Nitrogen is removed from the atmosphere primarily through a process called nitrogen fixation, where certain bacteria convert atmospheric nitrogen (N₂) into ammonia (NH₃), which can be utilized by plants. This ammonia can further be transformed into nitrates and nitrites through nitrification, allowing it to enter the food chain. Nitrogen is returned to the atmosphere through denitrification, where bacteria convert nitrates back into N₂ gas, completing the nitrogen cycle. Additionally, processes like combustion and industrial activities can also contribute to the release of nitrogen compounds back into the atmosphere.
Evaporation
Denitrification by bacteria
Carbon is returned to the atmosphere through the process of respiration by living organisms, where they release carbon dioxide as a byproduct. Additionally, the burning of fossil fuels for energy also releases carbon dioxide into the atmosphere.
precipitation, evaporation & condensation
precipitation, evaporation & condensation
* combustion * respiration * oxidization * Retrixilization (rare)
Carbon atoms are generally returned to the atmosphere in the form of carbon dioxide (CO2) through processes like respiration, decomposition, and combustion.
Nitrates are returned to the atmosphere through a process called denitrification, where bacteria convert nitrates back into nitrogen gas. This process occurs in oxygen-limited environments such as waterlogged soils or sediments. Nitrates can also be released into the atmosphere through volatilization from fertilizers or animal waste.
the TWO methods in which water is returned into the atmosphere:EvaporationCondensationThe water then precipitates and returns back.
Nitrogen is returned to the atmosphere by a process called denitrification, where certain bacteria convert nitrates in the soil back into nitrogen gas which is then released into the air. This helps maintain the balance of nitrogen in the environment cyclically.
The major process by which water in the atmosphere is returned to the earth is through precipitation. This includes rain, snow, sleet, and hail. When the water droplets in the clouds become heavy enough, they fall back to the earth's surface.
Carbon is returned to the atmosphere through processes like respiration by living organisms, decomposition of organic matter, and combustion of fossil fuels. When organisms respire, they release carbon dioxide back into the atmosphere. Decomposition of dead organic matter also releases carbon dioxide, while burning fossil fuels releases carbon that has been stored underground back into the atmosphere.