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This model presents the differences in titrating a strong acid (HCl) and a weak acid (Acetic acid). Students are able to observe the changes in pH when titrating a strong/weak acid with NaOH solution. Students may also change the concentrations of acids and the titrant and observe the corresponding results.
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This model presents the differences in titrating a strong base (NaOH) and a weak base (Ammonia). Students are able to observe the changes in pH when titrating a strong/weak base with a HCl solution. Students may also change the concentrations of bases and the titrant and then observe the corresponding results.
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Run the model
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Carbonic acid (H2CO3), Bicarbonate ion (HCO3-), and carbonate ion (CO3 (2-))are three species of dissolved inorganic carbon (DIC) that coexist in water. In a closed system, assuming that no carbon leaves or enters the system, the proportions of these species are determined by many factors. This model presents the proportions of three DIC species at different pH levels, ranging from 0 to 14, holding other factors constant. This model may serve as the foundation for students to explore the phenomenon of ocean acidification.
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Today's average ocean pH has dropped from 8.2 to about 8.1 as the ocean has taken up a large amount of CO2 from human activities since the industrial revolution. Many students are confused by the change in carbonate ion concentration in the ocean resulting from the increase in oceanic CO2 uptake. This model provides students with an established oceanic carbon system. Students may uncouple the three reactions involving the changes in three inorganic carbon species and recognize the long-term system dynamic to develop a deep understanding of these changes.
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