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The formula for cobalt(III) chromate is Co2(CrO4)3.
Carbon dioxide (CO2) possesses 3 vibrational modes.
The formula for cobalt (III) carbonate is Co2(CO3)3.
Carbon can be separated from carbon dioxide (CO2) through a process called carbon capture and storage (CCS). This involves capturing CO2 emissions from sources like power plants or industrial facilities, then separating the carbon from the CO2 gas. The separated carbon can then be stored underground or used in various industrial processes.
There are two elements in CO2, carbon and oxygen.
air is CO2
Some sources of CO2 include burning of fossil fuels (such as coal, oil, and natural gas), deforestation, livestock farming, and industrial processes like cement production. Additionally, transportation and heating systems also release CO2 into the atmosphere.
Carbon Dioxide is water soluble. Some of the main sources would be CO2 produced bay any animals that live in water and CO2 produced by decay of vegetable matter.
there are many sources including many which are caused by us human. Plants proudce co2 at night when there is no light. In burning fossil fuels we also produce vasts amounts of co2 the co2 conc of the air now is 0.004%
How long does co2 remain in the atmosphere
You think probable to the anion carbonate - CO2-3.
Co2, H2o and sunlight and the major sources required.
Cobalt (II) selenide has the formula CoSe.
A 20 oz CO2 bottle will hold 20 ounces of carbon dioxide gas when filled to capacity. This is a common size used in paintball markers and some other applications where portable sources of CO2 are needed.
Natural sources of CO2 include volcanic eruptions, respiration by plants and animals, and decomposition of organic matter. Human activities, such as burning fossil fuels and deforestation, have significantly increased CO2 levels in the atmosphere.
The formula for cobalt(III) chromate is Co2(CrO4)3.
Some bacteria, called autotrophs, make their own food from the carbon in CO2. Most bacteria are heterotrophs, taking their food 'ready-made' from other sources.