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Earth's Early Ocean

Once the Earth began to cool, water vapor, one of the volatiles, began to condense and form an ocean. According to the Goldilocks theory, Earth is at just the right distance from the sun for the temperature of the surface to be appropriate for the formation of liquid water. The presence of running water influenced the rest of the gases in the atmosphere, which began to dissolve into the forming ocean. By this time Earth was busy generating its secondary atmosphere. These atmospheric gases came out of a volcano. All volcanoes are different but in general those gases would include H2O, CO2, SO2, H2S, HCl, N2, NO2.

Gases such as CO2, SO2, and HCl form acids when dissolved in water. Such acids would immediately be neutralized via reaction with the surface minerals of the Earth, but the addition of so much acid to both the land and sea changed the pH of the ocean and surface from a reducing environment (hydrogen-based) to an oxidizing environment (oxygen-based).

Scientists think that the Earth's secondary atmosphere may have come to be dominated by N2 because it alone does not readily dissolve in water.

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Windows to the Universe, a project of the National Earth Science Teachers Association, is sponsored in part is sponsored in part through grants from federal agencies (NASA and NOAA), and partnerships with affiliated organizations, including the American Geophysical Union, the Howard Hughes Medical Institute, the Earth System Information Partnership, the American Meteorological Society, the National Center for Science Education, and TERC. The American Geophysical Union and the American Geosciences Institute are Windows to the Universe Founding Partners. NESTA welcomes new Institutional Affiliates in support of our ongoing programs, as well as collaborations on new projects. Contact NESTA for more information. NASA ESIP NCSE HHMI AGU AGI AMS NOAA