Typically, atmospheric nitrogen gets into the soil by nitrogen-fixing bacteria that are symbiotic with such plants as clover, soybeans and alfalfa. Bacteria in the plant extract nitrogen from the air, and when the plants die, the nitrogen remains in the soil as the plant decays.
The nitrogen goes into the nodules of the plant.
The nitrogen goes into the nodules of the plant.
carbon dioxide
The element in the atmosphere that causes scatter of light is nitrogen. When sunlight enters the Earth's atmosphere, nitrogen molecules scatter shorter wavelengths of light, such as blue and violet, which is why the sky appears blue to our eyes.
Nitrogen enters the atmosphere primarily through volcanic eruptions and the release of gases from the Earth's crust. It also comes from biological processes, such as denitrification, where bacteria convert nitrates in soil back into nitrogen gas. Nitrogen leaves the atmosphere mainly through nitrogen fixation, where certain bacteria convert atmospheric nitrogen into ammonia, and through processes like precipitation, where nitrogen compounds are deposited back to the Earth's surface. Additionally, human activities, such as burning fossil fuels and industrial processes, can also influence nitrogen levels in the atmosphere.
Nitrogen from the atmosphere primarily enters the soil through a process called nitrogen fixation, which is carried out by certain bacteria and archaea that can convert atmospheric nitrogen (N₂) into ammonia (NH₃). This ammonia can then be further transformed into nitrates (NO₃⁻) by nitrifying bacteria. Plants absorb these nitrates and ammonium ions through their roots, allowing them to utilize nitrogen for growth and development.
The nitrogen goes into the nodules of the plant.
Nitrogen enters the atmosphere through natural processes like volcanic eruptions and bacterial activity in soil. It is released through processes like denitrification, which converts nitrates into nitrogen gas, and nitrogen fixation, where nitrogen gas is converted into compounds that can be used by plants.
Nitrogen enters the atmosphere from the lithosphere through processes like volcanic eruptions and denitrification by bacteria. It enters the hydrosphere mainly through rainwater and runoff. In the biosphere, nitrogen is absorbed by plants from the soil, and in the atmosphere, it leaves through denitrification and nitrogen-fixing bacteria returning it to the soil. In the geosphere, nitrogen is locked in rocks and minerals for long periods until released through weathering processes.
The nitrogen goes into the nodules of the plant.
Nitrogen from the atmosphere primarily enters the soil through a process called nitrogen fixation, where certain bacteria convert atmospheric nitrogen (N₂) into ammonia (NH₃) or related compounds. This process occurs in the root nodules of specific plants, like legumes, or in the soil by free-living bacteria. Once in the soil, nitrogen can be taken up by plants or further transformed by other soil microorganisms through processes like nitrification and denitrification. Ultimately, nitrogen becomes part of the food chain as it is absorbed by plants, which are then consumed by animals.
Nitrogen in animal tissues primarily enters the atmosphere through the process of decomposition. When animals die or excrete waste, bacteria and other decomposers break down the organic matter, releasing nitrogen in the form of ammonia. This ammonia can then be further converted by nitrifying bacteria into nitrites and nitrates, which may eventually be converted into nitrogen gas (N₂) through denitrification, returning nitrogen to the atmosphere. Thus, the cycle of nitrogen continues as it moves between different forms and reservoirs in the ecosystem.