Carbon Sequestration Journal

 Carbon sequestration, the long-term storage of carbon in plants, soils, geologic formations, and therefore the ocean. Carbon sequestration occurs both naturally and as a results of anthropogenic activities and typically refers to the storage of carbon that has the immediate potential to become CO2 gas. In response to growing concerns about global climate change resulting from increased CO2 concentrations within the atmosphere, considerable interest has been drawn to the likelihood of accelerating the speed of carbon sequestration through changes in land use and forestry and also through geoengineering techniques like carbon capture and storage.   Anthropogenic activities like the burning of fossil fuels have released carbon from its long-term geologic storage as coal, petroleum, and gas and have delivered it to the atmosphere as CO2 gas. CO2 is additionally released naturally, through the decomposition of plants and animals. the quantity of CO2 within the atmosphere has increased since the start of the economic age, and this increase has been caused mainly by the burning of fossil fuels. CO2 may be a very effective greenhouse gas—that is, a gas that absorbs infrared emitted from Earth’s surface. As CO2 concentrations rise within the atmosphere, more infrared is retained, and therefore the average temperature of Earth’s lower atmosphere rises. This process is mentioned as heating

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