Evolution of the Atmosphere (Edexcel GCSE Chemistry)

Earth´s Early Atmosphere

• Theories on the development of Earth’s atmosphere have developed over time as instrumental analysis has improved

• The surface of the early Earth was molten for millions of years during which time there was no atmosphere surrounding the planet

• Eventually cooling began to take effect and allow for molten materials to slowly solidify forming land masses

• Volcanoes formed on the land masses and released gases from the Earth’s interior through violent eruptions

• Earth’s gravity prevented the gases from escaping into outer space and they formed the atmosphere

• Analysis of the minerals in the earth's crust enables scientists to deduce the gases present millions of years ago that helped form those minerals

• It is thought that the atmosphere at that moment in Earth’s history was similar to that of Venus or Mars today which consist mainly of CO₂

• During a period of intense volcanic activity, large amounts of carbon dioxide and water vapour were released, as well as nitrogen, hydrogen, ammonia, methane and other gases.

• The early atmosphere therefore contained mainly CO₂ and water vapour

• There was little or no oxygen present

Volcanoes spewed out water, carbon dioxide and other gases from the Earth’s interior

• While the surface of the Earth was still very hot the large quantities of water vapour remained in the gaseous state

• When conditions cooled sufficiently, the water vapour later condensed and fell to the surface of the Earth, forming the oceans

• Carbon dioxide is a water soluble gas (it is the gas used in fizzy drinks) and dissolves readily

• When the water vapour condensed large amounts of CO₂ dissolved in the oceans

• Carbonate substances were precipitated during this process which later formed sediments

How Carbon Dioxide Decreased

• Carbon dioxide is a water soluble gas (it is the gas used in fizzy drinks) and dissolves readily

• When the water vapour in Earth’s early atmosphere condensed large amounts of CO₂ dissolved in the oceans

• Carbonates were precipitated during this process which later formed sediments on the seabed

• As marine life began to evolve sea creatures began to appear which used up the carbonates to form shells and skeletons

• Green plants and algae began to evolve and absorbed considerable amounts of carbon dioxide during photosynthesis

Photosynthesis gradually removed large amounts of carbon dioxide from the atmosphere

• When these organisms died, their remains locked the atmospheric carbon into the rocks

• This is how the large amounts of carbon dioxide in the early atmosphere were reduced

How Oxygen Increased

• Primitive plants and algae began photosynthesizing which used up carbon dioxide from the atmosphere and released oxygen:

Carbon dioxide and water producing glucose and oxygen during photosynthesis

• Through these processes over a long period of time, the amount of O₂ in the atmosphere increased  and the amount of CO₂ decreased

• Algae first evolved around 2.7 billion years ago and during the next billion years or so small green plants began to appear

• As more and more plants began to appear the levels of oxygen began to increase which allowed for more complex life forms to evolve

• This trend continued until around 200 million years ago the composition of the atmosphere reached similar characteristics as today: around 20% oxygen, 80% nitrogen and tiny amounts of other gases

• Marine algae are throught to be responsible for about 90% of all the atmospheric oxygen produced

Investigating the percentage of oxygen in air

• The percentage of oxygen in the air can be investigated by passing a known quantity of air over a metal

• The oxygen in the air will react with the metal, forming a metal oxide

• The oxygen will be removed from the air and the volume of the air with the oxygen removed can be measured

• An example of the apparatus that can be used to investigate this is shown below:

Method:

• Heat the copper using a Bunsen burner

• Push the plunger of the syringe containing air, forcing the air into the other plunger until all of the air has transferred

• Push the air back from the now filled plunger to the other plunger

• Repeat this several times for about 3 minutes

• The copper will turn black as copper reacts with the oxygen in the air and copper oxide is produced

• Allow the apparatus to cool

• Ensure all the gas is in one syringe and record the volume of gas

• The percentage of oxygen in the air can be calculated from the results

The Test for Oxygen

• The test for oxygen consists of placing a glowing splint inside a test tube of gas

• If the gas is oxygen the splint will relight

Diagram showing the test for oxygen gas