Gaseous cylces Is a process by which elements like oxygen,carbon, nitrogen & water move through atmosphere in a gaseous phase . The reservoir pool is atmosphere or water .
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.
The formation of clouds
The biogeochemical cycle consists of several interconnected processes involving the exchange of elements between living organisms and the environment. The main parts include the atmosphere (gaseous phase), lithosphere (solid Earth), hydrosphere (water bodies), and biosphere (living organisms). These cycles include the carbon cycle, nitrogen cycle, phosphorus cycle, and water cycle, among others.
A particle of gaseous water begins its journey in the atmosphere as water vapor, where it can condense into clouds during the cooling process. Next, it precipitates as rain or snow, falling to the ground and entering bodies of water or soil. From there, it can either be absorbed by plants, enter rivers and lakes, or evaporate back into the atmosphere. The cycle continues as the water vapor rises again, completing its trip through the water 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 :)
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.
This is the transformation of liquid water in gaseous water.
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 gaseous cycle refers to the movement of gases such as oxygen, carbon dioxide, and nitrogen through different parts of the Earth's ecosystem. These gases are constantly being exchanged between the atmosphere, organisms, soil, and bodies of water through processes like photosynthesis, respiration, and decomposition. The gaseous cycle is essential for maintaining the balance of gases in the atmosphere and supporting life on Earth.
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