Space Travel
12, Feb, 2012

Earths Oceans are Becoming More Acidic

Written by spacetravel.org   
Sunday, 31 July 2005 22:44
The first review of all the studies relating to the acidification of the oceans has been commissioned by the Royal Society, the UK’s national academy of science. This review has led to the conclusion that the oceans are becoming more acidic as they soak up excess carbon dioxide released into the atmosphere. This could be catastrophic for marine ecosystems and for economies that rely on fishing and reef tourism. As carbon dioxide gas dissolves in the oceans, it forms carbonic acid. The oceans, which are naturally alkaline, with an average pH of 8.2, act as a buffer that can soak up large quantities of carbon dioxide with little change in acidity. However, carbon dioxide levels in the atmosphere are now rising so quickly, from 280 parts per million before the industrial age to 380 parts per million today, that the oceans are becoming more acidic. Models suggest the by the year 2100, the pH of the sea will fall by as much as 0.5 units if carbon dioxide emissions continue at their present rates.

The leader of the review, John Raven of the University of Dundee, UK, says that the increase in acidity would affect the food chain, which would have potentially harmful effects on large animals. As the oceans became more acidic, it would be more difficult to extract oxygen from water. This could affect the reproduction and growth of animals with high oxygen demands, including squid. As pH fell, the proportion of dissolved forms of toxic metals would also increase.

Organisms with calcium carbonate shells, such as shellfish, certain plankton species and coral polyps, would probably feel the greatest effect. Carbonate ions, which saturate ocean water, make calcium carbonate insoluble. As the oceans’ acidity rises, the level of carbonate ions will falls, which will make it harder for animals to make their shells. In some parts of the oceans, shells could even begin dissolving.

Acidification may add to the problems endured by coral reefs, which already include global warming and acidification. Raven says we can expect to see coral reef degradation in the tropics. This would affect fisheries and tourism, and it would leave shorelines more vulnerable. Some people say that as the oceans warm up, coral reefs will grown faster, which will make up for the increased acidity. However, all studies so far suggest that coral calcification peaks at current temperatures.

As the oceans become more acidic, it may be harder for them to absorb carbon dioxide, which would intensify the problem. Currently, many coccolithophores, photosynthetic plankton that form calcium carbonate shells, sink to the bottom of the ocean, where they safely lock away huge amounts of carbon in ocean sediments. In the last 200 years, the sea has absorbed about half the carbon dioxide produced by human beings. It currently soaks up one ton of carbon dioxide gas each year for every human being on the planet. If the growth of coccolithophores is hindered, less carbon might be removed from the ocean and the atmosphere. This could speed up climate change as well as ocean acidification.

Raven claims that it would take thousands of years for natural processes to return the oceans to their pre-industrial state. The review group considered possibly neutralizing the process by dumping chalk into the sea, but concluded that the amount of chalk needed would be so great that it wouldn’t be practical. According to Andrew Watson of the University of East Anglia, UK, it would be like dumping the White Cliffs of Dover into the ocean every year. Raven says that decreasing carbon dioxide emissions is the only way to minimize the long-term consequences.