Setting the Stage
The ICE Table
Imagine you are setting up a chemical reaction in a laboratory. The reaction is a simple one: A+B⇌C+D. The problem gives us a very specific and somewhat unusual starting condition. Instead of just starting with reactants, we are told that initially, all four species—both reactants and products—are present at a concentration of 1 M each.
To keep track of how these concentrations change as the system moves towards equilibrium, we use a powerful tool called an ICE table (Initial, Change, Equilibrium).
We start by filling in the 'Initial' row with 1 M for A, B, C, and D. Now, we need to determine the 'Change'. Let's assume the reaction proceeds in the forward direction to reach equilibrium. This means a certain amount of A and B will be consumed. Let's call this amount x. Consequently, the concentrations of A and B will decrease by x (−x), while the concentrations of the products C and D will increase by the exact same amount x (+x).
Adding the initial concentrations and the changes gives us our equilibrium concentrations:
[A]eq=1−x
[B]eq=1−x
[C]eq=1+x
[D]eq=1+x
The Master Equation
Equilibrium Constant
The heart of any chemical equilibrium problem is the equilibrium constant expression. The equilibrium constant, Keq, is defined as the ratio of the product of the equilibrium concentrations of the products to the product of the equilibrium concentrations of the reactants.
For our reaction, the expression is:
Keq=[A][B][C][D]
We are given that
Keq=100 at
298 K. Now, we simply substitute the equilibrium expressions we derived from our ICE table into this master equation:
100=(1−x)(1−x)(1+x)(1+x)
The Algebraic Elegance
At first glance, this equation might look like it's going to turn into a messy quadratic equation. If you were to expand the numerator and the denominator, you would indeed get a quadratic. However, take a closer look at the structure of the equation!
The numerator is
(1+x) multiplied by itself, which is
(1+x)2. The denominator is
(1−x) multiplied by itself, which is
(1−x)2. This means the entire right side of the equation is a perfect square:
100=(1−x1+x)2
This is where we can use a little algebraic elegance to save a lot of time. By taking the square root of both sides, we completely bypass the need for the quadratic formula. The square root of
100 is
10, so our equation simplifies beautifully to:
10=1−x1+x
Now, it's just a matter of simple linear algebra. We cross-multiply to get:
10(1−x)=1+x
Expanding the bracket gives:
10−10x=1+x
Grouping the
x terms on one side and the constants on the other, we find:
9=11x
Solving for
x, we get:
x=119≈0.818
The Final Piece of the Puzzle
We have found the value of x, but we are not quite done yet. The question specifically asks for the equilibrium concentration of D.
Let's look back at our trusty ICE table. The equilibrium concentration of
D is given by the expression
1+x. Now that we know
x=0.818, we simply substitute this value back in:
[D]eq=1+0.818=1.818 M
And there we have it! By carefully setting up our initial conditions, applying the law of mass action, and using a clever algebraic shortcut, we've arrived at the final answer. The equilibrium concentration of D is 1.818 M.