Biogeochemical cycling moves a chemical substance through the biotic (living) and abiotoic (nonliving) components of earth. There are many biogeochemical cycles.
One example of a biogeochemical cycle is the water cycle. The water cycle describes how water on the earth evaporates and rises into the atmosphere. Once it reaches the atmosphere, it cools and condenses into clouds. From the clouds, the water falls back to the ground (precipitates) in the form of rain, snow, sleet, or hail. Once on the ground, it can evaporate again into the atmosphere.