The nitrogen goes into the nodules of the plant.
The nitrogen goes into the nodules of the plant.
carbon dioxide
The nitrogen goes into the nodules of the plant.
The nitrogen goes into the nodules of the plant.
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.
carbon dioxide
The correct name for a shooting star is a Meteorite. Before a meteorite enters the Earths atmosphere it is called a Meteoroid.
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 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.
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.
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.