Nitrogen in the atmosphere is converted into nitrogen in the soil by a process called nitrogen fixation, which is carried out by a number of different types of bacteria.
Some of these bacteria grow on the roots of certain plants, such as clover, alfalfa, and peanuts, and provide nitrogen to the plant and the soil.
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Lightning also causes some atmospheric nitrogen to be converted into oxides of nitrogen. These dissolve in rain water and are brought to the ground in the rain.
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Nitrogen from the atmosphere is brought into the ground primarily through a process called nitrogen fixation, where certain soil bacteria convert atmospheric nitrogen into a form that plants can use. This process can occur naturally or through human interventions such as planting nitrogen-fixing cover crops or using fertilizers.
Atmospheric nitrogen can enter the ground through nitrogen-fixing bacteria in the soil that convert nitrogen gas into a form plants can use. It can also enter the ground through rainfall, where nitrogen oxides from the atmosphere dissolve in water and are deposited on the soil.
In the absence of oxygen, nitrogen in the ground is typically found in the form of nitrogen gas (N2). Nitrogen gas makes up about 78% of Earth's atmosphere and can dissolve in soil and groundwater, providing an essential nutrient for plants and microorganisms.
Titan's atmosphere is primarily composed of nitrogen gas, with about 98.4% of the atmosphere being nitrogen. This makes it similar to Earth's atmosphere in terms of nitrogen composition.
The largest reservoir of nitrogen is in the atmosphere, where it exists primarily as nitrogen gas (N2). Nitrogen gas makes up about 78% of Earth's atmosphere.
A large amount of nitrogen can be found in the Earth's atmosphere, comprising about 78% of the air we breathe. Additionally, nitrogen can be found in the soil and in organic matter.