Section 4 - Chemistry of Ocean Acidification

Overview and Purpose

There are two activities in this section. The Combustion Lab will explore how burning fossil fuels (combustion) causes oceans to acidify. The LEGO activity will go into more detail about how this will affect marine organisms that utilize calcium carbonate.

In the previous section, students explored how carbon forms different materials and is recycled through various carbon sinks (reservoirs). One of the ways that carbon moves from one sink to another is when humans burn fossil fuels. Burning coal, oil, and gas breaks the bonds that hold carbon atoms together inside those fuels, and carbon is released into the atmosphere. The ocean absorbs about a quarter of the CO2 we release into the atmosphere every year, so as atmospheric CO2 levels increase, so do the levels in the ocean. Initially, many scientists focused on the benefits of the ocean as a carbon sink as it is removing this greenhouse gas from the atmosphere. However, decades of ocean observations now show that there is also a downside: the CO2 absorbed by the ocean is changing the chemistry of seawater.

As the ocean absorbs increasing amounts of CO2 from the atmosphere, chemical reactions take place that decrease the pH of the ocean. This lowering of pH makes ocean water more acidic. The ocean’s pH has lowered by .1 pH units since the Industrial Revolution. This may not seem like much, but pH is measured on a logarithmic scale, which means a 0.1 difference in pH indicates the ocean has become 30% more acidic. With CO2 continuing to sink into the ocean at extreme rates, scientists predict that the ocean could become 150% more acidic by 2100.

NGSS STANDARDS

OBJECTIVES

MATERIALS NEEDED

PROCEDURE

DIFFERENTIATION

ASSESSMENT

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