The difference between the short and long carbon cycle is that the short cycle emphasizes the interaction between the biosphere and atmosphere while the long cycle emphasizes the formation and destruction of fossil fuels.
To write a short story on the carbon cycle, you can personify carbon molecules as they journey through different reservoirs like the atmosphere, plants, animals, soil, and oceans. You can describe their transformations, interactions with different organisms, and the role of human activities in disrupting this cycle. To add depth, you can explore the impacts of these disruptions on the environment and climate.
The short form for carbon dioxide is CO2.
Long term cycle: phosphorus is found in bedrock in the form of phosphate ions combined with a variety of elements. Phosphates are soluble in water and so can be dissolved out of rock. While dissolved, phosphates can be absorbed by photosynthetic organisms and passed into food chains. Short term cycle: wastes from living things are recycled by decomposers, which break down wastes and dead tissues and release the phosphates. This cycle is much more rapid.
One important carbon cycle occurs as carbon dioxide is captured by plants and, during photosynthesis, the Sun's energy is used to dissociate the carbon and oxygen from the CO2. The carbon is used by the plant to build tissues while the oxygen is emitted into the air. At a later time the plant is burned, maybe as fuel or in a forest fire. The burning press reunites the carbon and oxygen, producing carbon dioxide, and the original energy is released as heat. Some plant material may be left in the ground for millions of years until it becomes coal, oil or gas. In this case, digging it up and burning it produces new carbon dioxide that the short-term carbon cycles can not absorb. This causes a buildup of CO2 in the atmosphere.
The short electron configuration for carbon is [He] 2s^2 2p^2.
The short-term carbon cycle involves the rapid exchange of carbon among the atmosphere, oceans, and living organisms, primarily through processes like photosynthesis, respiration, and decomposition. This cycle typically operates on timescales of days to years. In contrast, the long-term carbon cycle involves the geological processes that sequester carbon over millions of years, including the formation of fossil fuels, sedimentation, and the weathering of rocks. This cycle regulates Earth's climate over much longer periods and plays a crucial role in carbon storage in geological formations.
Carbon Cycle-short and sweet :)
In the short-term cycle, plants convert carbon dioxide into carbohydrates. Organisms eat the plants and obtain carbon, and then release it back into the air as carbon dioxide. Carbon is also released through wastes and decay of their remains.
The carbon cycle is a process by which carbon is cycled between the atmosphere, land, water and organisms. Carbon enters a short-term cycle in an ecosystem when producers, such as plants, convert carbon dioxide in the atmosphere into carbohydrates during photosynthesis.The carbon cycle is the biogeochemical cycle by which carbon is exchanged among the biosphere, pedosphere, geosphere, hydrosphere, and atmosphere of the Earth
well.......the carbon cylcle goes through two processes. one is i short term cycle. the other is a long term cycle
From an accounting perspective, short-term investments have a life cycle of less than 12 months; long term investments have a life cycle of 12 months or longer.
difference between short,near and far jump
To write a short story on the carbon cycle, you can personify carbon molecules as they journey through different reservoirs like the atmosphere, plants, animals, soil, and oceans. You can describe their transformations, interactions with different organisms, and the role of human activities in disrupting this cycle. To add depth, you can explore the impacts of these disruptions on the environment and climate.
the long term is different between a short term because the short
nothing
There is no difference. Limo is just short for limousine.
The carbon cycle consists of slow and fast pathways for carbon movement in the environment. The fast pathway involves the rapid exchange of carbon between the atmosphere and living organisms through processes like photosynthesis and respiration, where carbon dioxide is absorbed and released within short time frames. In contrast, the slow pathway encompasses long-term processes, such as the weathering of rocks, sedimentation, and the formation of fossil fuels, which can take thousands to millions of years to cycle carbon through the Earth’s systems. Together, these pathways maintain the balance of carbon in the atmosphere and contribute to climate regulation.