88 Introduction

Chapter Outline

14.1 Ionic Compounds in Aqueous Solution

14.2 Brønsted-Lowry Acids and Bases

14.3 pH and pOH

14.4 Relative Strengths of Acids and Bases

14.5 Hydrolysis of Salt Solutions

14.6 Polyprotic Acids

14.7 Buffers

14.8 Acid-Base Titrations

Sinkholes such as this are the result of reactions between acidic groundwaters and basic rock formations, like limestone. (credit: modification of work by Emil Kehnel)

A photograph is shown of a pond formed in a sinkhole. Layers of limestone with trees and shrubs surround the murky green water of the pond.

Liquid water is essential to life on our planet, and chemistry involving the characteristic ions of water, H+ and OH–, is widely encountered in nature and society. As introduced in another chapter of this text, acid-base chemistry involves the transfer of hydrogen ions from donors (acids) to acceptors (bases). These H+ transfer reactions are reversible, and the equilibria established by acid-base systems are essential aspects of phenomena ranging from sinkhole formation ((Figure)) to oxygen transport in the human body. This chapter will further explore acid-base chemistry with an emphasis on the equilibrium aspects of this important reaction class.

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Introduction Copyright © by D. Latimer; D. Vanderwel; and J. Hollett is licensed under a Creative Commons Attribution 4.0 International License, except where otherwise noted.

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