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A majority of the earths carbon is located in the ocean.
Carbon dioxide is the main one.
Carbon is mostly found in the Earth's crust as carbonates, in the atmosphere as carbon dioxide, and in living organisms such as plants and animals. It is also found in fossil fuels such as coal, oil, and natural gas.
Bicarbonates,carbonates and organic molecules
Carbon dioxide can form carbonates when it react with a basic substance
Both metal carbonates and metal hydrogen carbonates form carbon dioxide when mixed with acid.
Carbon dioxide moves from the hydrosphere to the geosphere primarily through processes like sedimentation and mineralization. When CO2 dissolves in ocean water, it can react with minerals and form carbonates, which eventually settle to the ocean floor. Over geological time, these carbonates can become part of sedimentary rock formations, effectively sequestering carbon in the geosphere. Additionally, volcanic activity can release stored carbon back into the atmosphere, completing the cycle.
The atmosphere, the ocean, and the terrestrial biosphere.Carbon can be found in the earths oceanic and continental crust in different types of stones as well as in the soil from the decay of organic matter.
The largest amount of inorganic carbon is found in the Earth's lithosphere, primarily in carbonate rocks such as limestone and dolomite. These rocks contain carbon in the form of carbonates, which are compounds made up of carbon, oxygen, and other elements.
Acids produce carbon dioxide gas when they react with carbonates. This is due to the acid breaking down the carbonate to form carbon dioxide, water, and a salt.
The geological process that removes carbon from the atmosphere is called carbon sequestration, primarily occurring through the weathering of silicate minerals. During this process, carbon dioxide reacts with minerals to form carbonates, which are then transported to the ocean. In marine environments, carbonates can eventually form sedimentary rock, effectively sequestering carbon for millions of years. Additionally, the formation of fossil fuels and the long-term storage of organic carbon in sediment and soil also play significant roles in this carbon removal process.
Fairly reactive metals such as iron, lead, and zinc are commonly found as ores in the form of oxides and carbonates. These metals can be extracted using carbon as a reducing agent to convert the metal oxides or carbonates into pure metals through a process called smelting. This method involves heating the ore with carbon in a furnace to produce the desired metal.