Cycles within ecosystems
Elements move about within our environment, from organism to organism. It’s strange to think that all of the atoms inside of us have at one point formed stars, bacteria, the ocean, trees, flowers, fish and right now they happen to be sitting hanging around inside of you. This page outlines the different forms in which nitrogen, carbon and water move within ecosystems.
The nitrogen cycle
Plants can only absorb nitrogen in the form of nitrate so they depend on nitrogen-fixing bacteria to convert nitrogen in the air into nitrate in the soil. These bacteria either live freely in the soil or inside root nodules, forming a symbiotic relationship with the plant.
The Haber process is used to convert nitrogen into ammonia which is used in fertilisers. Nitrifying bacteria convert the ammonia into nitrates. Plants absorb the nitrates and incorporate the nitrogen into amino acids which are used to build proteins. The breakdown of proteins in our bodies produces urea which is removed from our body in our urine. Nitrogen is also returned to the soil by the decomposition of dead matter by microorganisms such as bacteria and fungi.
In some conditions, denitrifying bacteria convert nitrates in the soil into nitrogen in the air. This usually happens in soil which is lacking oxygen, such as waterlogged soil. Therefore, improving drainage can make soil more fertile by retaining more nitrates.
The carbon cycle
Carbon is added to the atmosphere when respiration of living organisms and combustion of fossil fuels release carbon dioxide into the air. The carbon dioxide is removed from the air by plants and converted into carbohydrate during photosynthesis. When animals eat the plants, they incorporate the carbon into their own biological molecules, such as carbohydrate, proteins and lipids. When animals and plants decompose, carbon is released into the atmosphere through the respiration of decomposers, such as bacteria and fungi. The carbon in any remaining dead material will eventually form fossil fuels after millions of years of compression beneath the Earth’s surface.
The Water Cycle
Water is essential to life on Earth and is constantly moving through our environment. Some of the water on the Earth’s surface, for example in oceans, lakes and puddles, evaporates when exposed to heat energy from the Sun, forming water vapour in the atmosphere. This condenses to form clouds which are easily blown by winds to other areas. Precipitation of the water droplets within clouds returns water back to the Earth’s surface, which is either absorbed into the ground (infiltration) or runs along the surface of the ground (surface run-off) and into streams and rivers. Some of the water that has been absorbed by soil is taken up by plants for photosynthesis. Some water evaporates from the surface of the leaf, through the stomata, in a process called transpiration. Transpiration creates a pulling force (transpiration pull), resulting in the movement of water through the plant.
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