Using round figures,
Mass of atmosphere = 5 x 10
18 kg
Mass of oxygen in atmosphere = 1 x 10
18 kg ( 1 x 10
15 tonnes )
If all the atmospheric oxygen came from water at 1000kg/m
3 ( water mostly oxygen )
Thus, Volume of water = 1 x 10
15 m
3 ( times 2 for O
2 )
Or 1 x 10
15 tonnes of water
Or a cube of water 1 x 10
5 m per side.
Or a cube of water 100 km per side.
A few mountains of water, something like the size of Everest, would have to dissassociate into as oxygen to make and keep the atmosphere the way as we know it.
Iron oxide mountains - there would have to a few more mountains.
One would need that many bugs working away to make an atmosphere richer in oxygen, if that is the method and means, and where "that many bugs" would be a figure to be determined somehow.
Present biomass in terms of carbon. ( all organisms , not just photsynthetic )
1 x 10
12 tonnes of carbon ( rough figure ) ( amount of bacteria unknown, but by some estimates more than that of all other biomass )
There is an exception with https://www.physicsforums.com/wiki/Cyanobacteria . Marine cyanobacteria are the smallest known https://www.physicsforums.com/wiki/Photosynthesis organisms; the smallest of all,
https://www.physicsforums.com/wiki/Prochlorococcus , is just 0.5 to 0.8 micrometres across.
[10] Prochlorococcus is possibly the most plentiful https://www.physicsforums.com/wiki/Species on Earth: a single millilitre of surface seawater may contain 100,000 cells or more. Worldwide, there are estimated to be several https://www.physicsforums.com/wiki/Octillion (~1027) individuals.
[11] Prochlorococcus is ubiquitous between 40°N and 40°S and dominates in the https://www.physicsforums.com/wiki/Oligotroph (nutrient poor) regions of the oceans.
[12] The bacterium accounts for an estimated 20% of the https://www.physicsforums.com/wiki/Oxygen in the Earth's https://www.physicsforums.com/wiki/Atmosphere , and forms part of the base of the ocean https://www.physicsforums.com/wiki/Food_chain .
[13]
https://en.wikipedia.org/wiki/Biomass_(ecology )
In the early earth, that 20% figure would have to be 100%.
We could use a ratio of carbon biomass/ atmospheric oxygen as a guide, and assume bacterial biomass is the total biomass.
In which case 10
12 / 10
15 which gives each carbon unit is responsible for 1000 units of atmospheric oxygen.
Actual corelation ?? in the early earth.
Bacterial output of oxygen would have to be > reconversion back to locked in oxgen as a compound.
That would be a lot of bacteria, even if the atmospheric oxygen was 1%.
Very crude, and open to criticism.