The atmospheric cycle is the exchange of heat between the sun and the surface of the earth. It is these atmospheric cycles that determine the weather.
The annual cycle of atmospheric carbon dioxide concentration is mainly due to the natural processes of photosynthesis and respiration in plants. During the spring and summer months, plants take in carbon dioxide for photosynthesis, which reduces the concentration in the atmosphere. In the fall and winter, when plants go dormant and decay, they release carbon dioxide back into the atmosphere, causing an increase in concentration. This cycle repeats annually, leading to fluctuations in atmospheric carbon dioxide levels.
Phosphorus, often leached from rocks and minerals, is an important component of soils. Phosphorus does not have an atmospheric form, so it is most often transported by water. Inorganic phosphorus is taken in by plants, incorporated into organic compounds, and moves up the food chain. Phosphorus is returned to the soil and rock cycle through decomposition of waste.
The first step of the nitrogen cycle is nitrogen fixation.
The water cycle involves weather as it drives processes such as evaporation, condensation, and precipitation that are influenced by atmospheric conditions like temperature and pressure. These weather-related factors play a critical role in transporting water and energy around the Earth.
The movement of air is considered a cycle because it continuously circulates in the Earth's atmosphere through processes such as convection, wind patterns, and atmospheric circulation. Air masses are constantly being displaced and redistributed, creating a cycle of air movement around the globe.
No, the nitrogen cycle has an atmospheric component. Nitrogen gas (N2) in the atmosphere is converted into compounds that can be used by living organisms through processes like nitrogen fixation and denitrification. This atmospheric nitrogen is essential for the functioning of the nitrogen cycle on Earth.
Phosphorus is not an atmospheric cycle because it is not found in significant quantities in the atmosphere like other elements such as carbon, nitrogen, and oxygen. Instead, phosphorus cycles through the lithosphere, hydrosphere, and biosphere primarily through the weathering of rocks, runoff into oceans, and biological processes. This makes phosphorus a terrestrial cycle rather than an atmospheric cycle.
carbon dioxide
The nitrogen cycle involves the process of nitrogen fixation by certain bacteria converting atmospheric nitrogen into forms usable by plants, which are then consumed by animals. Decomposers break down organic matter into ammonia and return nitrogen to the soil. Denitrification by bacteria converts nitrates back to atmospheric nitrogen to complete the cycle.
The major parts of the nitrogen cycle include nitrogen fixation (conversion of atmospheric nitrogen into forms usable by plants), nitrification (conversion of ammonium into nitrites and nitrates by bacteria), denitrification (conversion of nitrates back into atmospheric nitrogen), and assimilation (incorporation of nitrogen into plant and animal tissues).
Yes, in the nitrogen cycle, atmospheric nitrogen is converted to biologically active forms through a process called nitrogen fixation. This can occur through abiotic processes, such as lightning or industrial methods, where atmospheric nitrogen is converted to ammonia or nitrate that can be used by plants.
The annual cycle of atmospheric carbon dioxide concentration is mainly due to the natural processes of photosynthesis and respiration in plants. During the spring and summer months, plants take in carbon dioxide for photosynthesis, which reduces the concentration in the atmosphere. In the fall and winter, when plants go dormant and decay, they release carbon dioxide back into the atmosphere, causing an increase in concentration. This cycle repeats annually, leading to fluctuations in atmospheric carbon dioxide levels.
Various bacteria are responsible for carrying out key processes in the nitrogen cycle. For example, nitrogen-fixing bacteria convert atmospheric nitrogen into a form usable by plants. Other bacteria, like nitrifying bacteria, convert ammonium into nitrates, which can then be used by plants. Denitrifying bacteria convert nitrates back into atmospheric nitrogen, closing the cycle.
Photosynthesis
Phosphorus, often leached from rocks and minerals, is an important component of soils. Phosphorus does not have an atmospheric form, so it is most often transported by water. Inorganic phosphorus is taken in by plants, incorporated into organic compounds, and moves up the food chain. Phosphorus is returned to the soil and rock cycle through decomposition of waste.
The rock cycle does not include a major path that cycles through the atmosphere. This cycle involves processes such as erosion, sedimentation, and metamorphism that occur within the Earth's crust and do not involve atmospheric exchanges.
The first step of the nitrogen cycle is nitrogen fixation.