Today, as we were
travelling along the Brazilian coast, we were visited by a pod of playful
dolphins. They reminded me of the
delicacy of Earth’s ocean biome, and how small changes can result in large
consequences.
Time for a brief
chemistry lesson! When carbon dioxide from the atmosphere
dissolves in the ocean, it forms carbonic acid. However, it quickly breaks down
into bicarbonate (HCO3) and hydrogen ions (H+).
H2O +
CO2 →
HCO3 + H
Since acidity is
the measure of hydrogen ions in a fluid, as the number of ions increases, the
acidity of the oceans rises as well.
HCO3 +
H →
H2O + CO2
However, there
must be enough calcium carbonate in the oceans to increase carbon dioxide
levels, and currently, the ocean’s buffering system is not effective enough to
counter the rapid increase in the water’s acidity.
The Earth’s oceans are normally slightly basic, but with an increase in greenhouse gases, the seawater will likely slide down the Ph scale. Since the Ph scale’s intervals are by powers of 10 (each level is to the 10th power more acidic then the level below), this represents a drastic increase in the water’s acidity.
Dolphins are considered a symbol of protection in many cultures around the world. The health of these dolphins relies on the health of the ocean’s ecosystems, and hopefully we can all make an effort to ensure that these lovely creatures survive.
References
Adam-Carr, Christine, Douglas Fraser, et al. Science Perspectives 10. Toronto: Nelson
Education Ltd, 2010. Print.
Findlay, Helen. "Ocean
Acidification." Catlin Arctic Survey Blog. Catlin Arctic Survey, 12
Apr 2011. Web. 21 April 2012.
<http://www.catlinarcticsurvey.com/2011/04/12/ocean-acidification/>.
Gerad
Bandos. Ph
Scale. 2007. Graphic. Chemical Education Digital Library. Web. 6
May 2012.
<http://chemteacher.chemeddl.org/services/chemteacher/images/stories/pH_Scale.jpg>.
Kim
Martineau. Ocean
Chemistry. 2009. Photograph. Ocean Acidification. Web. 27 April 2012.
<http://theotherco2problem.files.wordpress.com/2009/11/ocean-chemistry.gif>.
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