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Marine Effect The CO2 in the atmosphere transfers to the ocean by dissolving in the surface water as carbonate and bicarbonate ions; at the same time the carbonate ions in the water are returning to the air as CO2.
This exchange process brings14C from the atmosphere into the surface waters of the ocean, but the 14C thus introduced takes a long time to percolate through the entire volume of the ocean.
You' II be surprised; there is more to traffic management in Texas than meets the eye. 1730-1830 Portuguese 17705 Af E there are three current affairs pro- This postcard from Botswa11a features the town of Mochudi, which lies about 25 miles northeast of Gaborone on the country's one railroad.
The carbon exchange between atmospheric CO2 and carbonate at the ocean surface is also subject to fractionation.
Reservoir Effects Libby’s original exchange reservoir hypothesis assumed that the exchange reservoir is constant all over the world, but it has since been discovered that there are several causes of variation in the 14C/12C ratio across the reservoir.
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