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General Chemistry Principles, Patterns, and Applications, 2011

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Equilibrium constant expression (law of mass action)<br />

Equation 15.8 : K = [ C]c[ D]d[ A]a[ B]b<br />

Equilibrium constant expression for reactions involving gases using partial pressures<br />

Equation 15.17 : Kp = (PC)c(PD)d(PA)a(PB)b<br />

Relationship between K p <strong>and</strong> K<br />

Equation 15.19: K p= K(RT) Δ n<br />

C O N C E PTUAL P R OBLEMS<br />

1. For an equilibrium reaction, what effect does reversing the reactants <strong>and</strong> products have on the value of the<br />

equilibrium constant?<br />

2. Which of the following equilibriums are homogeneous <strong>and</strong> which are heterogeneous?<br />

[1] The “effective pressure” is called the fugacity, just as activity is the effective concentration.<br />

[2] The reference states for pure solids <strong>and</strong> liquids are those forms stable at 1 bar (approximately 1 atm), which are<br />

assigned an activity of 1.<br />

15.3 Solving Equilibrium Problems<br />

L E A R N I N G O B JE C T I V E<br />

1. To solve quantitative problems involving chemical equilibriums.<br />

There are two fundamental kinds of equilibrium problems: (1) those in which we are given the concentrations of the<br />

reactants <strong>and</strong> the products at equilibrium (or, more often, information that allows us to calculate these<br />

concentrations), <strong>and</strong> we are asked to calculate the equilibrium constant for the reaction; <strong>and</strong> (2) those in which we are<br />

given the equilibrium constant <strong>and</strong> the initial concentrations of reactants, <strong>and</strong> we are asked to calculate the<br />

concentration of one or more substances at equilibrium. In this section, we describe methods for solving both kinds of<br />

problems.<br />

Calculating an Equilibrium Constant from Equilibrium Concentrations<br />

We saw in the exercise in Example 6 in Section 15.2 "The Equilibrium Constant" that the equilibrium<br />

constant for the decomposition of CaCO3(s) to CaO(s) <strong>and</strong> CO2(g) is K= [CO2]. At 800°C, the concentration<br />

of CO2 in equilibrium with solid CaCO3 <strong>and</strong> CaO is 2.5 × 10 − 3<br />

M. Thus K at 800°C is 2.5 × 10 − 3 . (Remember<br />

that equilibrium constants are unitless.)<br />

Saylor URL: http://www.saylor.org/books<br />

Saylor.org<br />

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