In a gas cycle elements move through the atmosphere. Main reservoirs are the atmosphere and the ocean.
Gas Cycles:
Carbon
Nitrogen
Oxygen
Water vapor is the gaseous form of water. When it cools down or loses energy, it condenses and returns to a liquid state, forming water droplets. This process is crucial for the water cycle on Earth.
The phosphorus cycle does not have any gas components because phosphorus does not exist in gaseous form in the Earth's atmosphere. Instead, phosphorus is primarily found in rocks and minerals, and moves through the environment in the form of dissolved phosphates in water or within organic matter in soil.
Volume
Radiation is the type of heat transfer that does not require a solid, liquid, or gaseous medium. It can occur through vacuum or transparent mediums such as air or glass.
Inside a condenser, vaporized or gaseous refrigerant is converted back into a liquid state through the process of condensation. This is achieved by transferring heat from the refrigerant to the surrounding environment, causing it to cool and change phase. The condensed liquid refrigerant can then be circulated back into the refrigeration or air conditioning system to continue the cooling cycle.
nitrogen cycle
Carbon cycle is a type of Gaseous cycle.Biological/biochemical cycles can only be either Gaseous or Sedimentary. I hope it will work :)
Gaseous cycles refer to the processes in which elements such as oxygen, nitrogen, carbon, and sulfur circulate through the atmosphere. These cycles involve the exchange of these elements between living organisms, the atmosphere, and the Earth's surface. Examples of gaseous cycles include the carbon cycle and the nitrogen cycle.
This is the transformation of liquid water in gaseous water.
Biogeochemical cycles are basically of two types: a) Gaseous cycles like carbon (as carbon dioxide), oxygen, nitrogen, etc. b) Sedimentary cycles like sulphur, phosphorus, etc. In gaseous cycles, the elements have a main reservoir in the gaseous phase, and the reservoir pool is the atmosphere or water. The biogenetic materials involved in circulation pass through a gaseous phase before completing the cycle. In sedimentary cycles, the elements main reservoir pool is lithosphere and the biogenetic materials involved in circulation are non-gaseous. The sedimentary cycles are usually very slow as the elements may get locked up in rocks and go out of circulation for long periods.
The slowest cycle without a gas phase is the phosphorus cycle. This cycle involves the movement of phosphorus through the lithosphere, hydrosphere, and biosphere, with no gaseous phase involved.
The process that involves the transformation of liquid water into gaseous water vapor in the water cycle is called evaporation. This occurs when heat energy from the sun causes liquid water on the Earth's surface to change into water vapor and rise into the atmosphere.
Elements like carbon, oxygen, and nitrogen are characterized by a gaseous biogeochemical cycle. These elements move between the atmosphere, living organisms, and the Earth's surface in a continuous cycle through processes like respiration, photosynthesis, and decomposition.
Nitrogen-fixing bacteria, such as Rhizobium and Azotobacter, convert gaseous nitrogen into ammonia through a process called nitrogen fixation. This process helps make nitrogen available to plants for growth and is a key step in the nitrogen cycle.
Charles Arthur McPherron has written: 'An evaluation of the gaseous-steam cycle (field cycle)' -- subject(s): Mechanical engineering
Biogeochemical cycles are basically of two types: a) Gaseous cycles like carbon (as carbon dioxide), oxygen, nitrogen, etc. b) Sedimentary cycles like sulphur, phosphorus, etc. In gaseous cycles, the elements have a main reservoir in the gaseous phase, and the reservoir pool is the atmosphere or water. The biogenetic materials involved in circulation pass through a gaseous phase before completing the cycle. In sedimentary cycles, the elements main reservoir pool is lithosphere and the biogenetic materials involved in circulation are non-gaseous. The sedimentary cycles are usually very slow as the elements may get locked up in rocks and go out of circulation for long periods.
lightening help to fix gaseous nitrogen to more chemically reactive forms