Water Recycling

بِسْــــــــــــــــمِ اﷲِالرَّحْمَنِ اارَّحِيم


Recycled water is circulating that never stops from the water on earth Diman able to move water from the mainland, and then into the air and then kedaratan again, and was able to stored water bottom surface with 3 phases, namely in the form of liquid water, solid ice form, and gas in the form of air.
Water vapor present in the atmosphere, water vapor from the sea water and the water that evaporates as a result dratan terkenanya heat coming from the sun. But in general, the water vapor contained in diatmosfir just vaporized seawater, because the vast ocean reaches ¾ of the earth surface. Terkondensasinya water vapor in the atmosphere will change into clouds, clouds that eventually it will turn into rain, rain that came down in the earth will go into the soil, groundwater and eventually it will form a surface groundwater groundwater.

Available water in the soil is absorbed by plants memalui vessels in the body, and transpiration of water vapor is released by plants or plants into the atmosphere. Evapotranspiration in terrestrial ecosystems could reach 90% by plants.
Groundwater flow to the face of the earth towards the river, and empties into the sea and into the lake. Recycling this happens disebet with long cycle but this cycle begins with the process of Evapotranspiration and Transpiration in water followed by precipitation or the occurrence of water that falls to earth is called short sikus.
Just as the process of photosynthesis in the carbon cycle, the sun also plays an important role in the hydrological cycle. The sun is the energy source that drives the water cycle, heats water in oceans and seas. As a result of this warming, water evaporates as water vapor into the air. 90% of the water that evaporates from the oceans. Ice and snow can also be sublimed and directly into water vapor. Above all, the water is also going evapotranspiration occurs from plants and evaporated from the soil that increase the amount of water that enters the atmosphere.
After the water had become water vapor, rising air currents take the vapor to move up into the atmosphere. The higher the points, the lower the air temperature. Later the cold temperatures in the atmosphere cause water vapor to condense into clouds. For certain cases, water vapor condenses on the surface of the earth and forms a cloud.
Air currents (wind) carries water vapor moving around the world. Many meteorological processes occur in this section. Cloud particles collide, grow, and water falls from the sky as precipitation. Some precipitation falls as snow or hail, sleet, and can accumulate as ice caps and glaciers, which can store frozen water for thousands of years. Snowpack (compacted snow) can thaw and melt, and the melted water flows over land as snowmelt (snow melt). Most of the water falls to the surface and back to the sea or to the ground as rain, where the water flows over the ground as surface runoff.