The following aspects of industrialization is likely to have had an effect on the long-term carbon cycle are burning fossil fuels for energy.
When we burn fossil fuels, carbon (C) combines with oxygen molecules (O2) to make carbon dioxide (CO2), that's a greenhouse fueloline this is the principle contributor to weather change. This technique traps the oxygen molecules which can be in our air into the CO2–because of this that there is much less oxygen for existence to breathe.The more advantageous greenhouse effect.
Human interest has swiftly accelerated the emission of greenhouse gases to the atmosphere. Since the begin of the Industrial Revolution, in approximately 1750, human sports inclusive of burning fossil fuels, which include coal and oil, have accelerated greenhouse fueloline concentrations in our atmosphere.
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