b) We have assumed [CO;²] << [HCO;] in our precedent calculation and accordingly ignored the [CO;²] contribution. Explain why it is a good assumption to make for most natural waters. Note: the common pH range in natural waters is 5.5 to 8.5. (Hint: either use the second acid dissociation constant expression, or a quick sketch of the carbonate system Bierrum plot to demonstrate vour point)

Organic Chemistry
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ISBN:9781305580350
Author:William H. Brown, Brent L. Iverson, Eric Anslyn, Christopher S. Foote
Publisher:William H. Brown, Brent L. Iverson, Eric Anslyn, Christopher S. Foote
Chapter4: Acids And Bases
Section: Chapter Questions
Problem 4.35AP: The sec-butyl cation can react as both a Brnsted-Lowry acid (a proton donor) and a Lewis acid (an...
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b) We have assumed [CO;2] << [HCO;] in our precedent calculation and accordingly ignored the [CO32]
contribution. Explain why it is a good assumption to make for most natural waters. Note: the common pH
range in natural waters is 5.5 to 8.5. (Hint: either use the second acid dissociation constant expression, or
a quick sketch of the carbonate system Bjerrum plot to demonstrate your point)
Transcribed Image Text:b) We have assumed [CO;2] << [HCO;] in our precedent calculation and accordingly ignored the [CO32] contribution. Explain why it is a good assumption to make for most natural waters. Note: the common pH range in natural waters is 5.5 to 8.5. (Hint: either use the second acid dissociation constant expression, or a quick sketch of the carbonate system Bjerrum plot to demonstrate your point)
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