The Magic of Adsorption
Imagine you have a dry sponge and you place it in a puddle of water. The sponge eagerly soaks up the liquid, holding it within its porous structure. In the realm of surface chemistry, we observe a remarkably similar phenomenon known as adsorption. This occurs when a solid surface (the adsorbent) accumulates molecules of a gas or liquid (the adsorbate) on its exterior.
To mathematically model how much adsorbate is captured at a given concentration, scientists rely on the Freundlich Adsorption Isotherm. It provides a beautiful, empirical relationship:
Here, mx represents the mass of adsorbate per unit mass of adsorbent, C is the equilibrium concentration, and K and n are constants specific to the system at a given temperature. This equation is the master key to unlocking our problem.
Linearizing the Curve
The Power of Logarithms
Dealing with fractional exponents like n1 can be algebraically tedious. How do we simplify this? We bring down the power using the magic of logarithms! By taking the base-10 logarithm on both sides, we transform the exponential curve into a crisp, straight line:
Notice how this perfectly mirrors the classic equation of a straight line, y=mx+c. Our y-axis is log(mx), our x-axis is logC, our slope is n1, and our y-intercept is logK. This linear form makes it incredibly easy to solve for our unknown constants using experimental data.
Decoding the Constants
Using Experimental Data
The problem provides us with two sets of experimental observations. Let's plug in the reality of our experiment. For our first data point, when the concentration C is 10, the adsorbed amount mx is 4. Substituting these into our linear equation gives:
The problem generously provides a handy tool: log2=0.3. Since 4=22, we can easily calculate log4=2×0.3=0.6. And we know that log10=1. So, our first equation simplifies beautifully to:
Now, let's move to the second experimental observation. When the concentration increases to 16, the adsorbed amount goes up to 10. Substituting this gives:
Again, log10=1. What about log16? Well, 16=24. Therefore, log16=4×log2=4×0.3=1.2. Our second equation is now:
Look at what we have built: a neat system of two linear equations with two variables, logK and n1. The easiest way to solve this is to eliminate logK by subtracting equation (1) from equation (2):
1−0.6=(logK+n1.2)−(logK+n1)
We've found our slope! With the slope in hand, finding the intercept is a walk in the park. Let's substitute n1=2 back into our simpler first equation:
We now have all the constants that define our specific adsorption system.
The Final Prediction
Calculating the Unknown
We have successfully decoded the isotherm for this specific fly ash and phenol system. The question now asks us to predict the future: what will be the adsorbed amount when the concentration is 20? Let's set up the final equation by substituting C=20, logK=−1.4, and n1=2 into our logarithmic isotherm equation:
This is the final stretch. Let's calculate log20. Since 20=2×10, we have log20=log2+log10=0.3+1=1.3. Multiplying that by our slope gives 2×1.3=2.6. Now, add our intercept:
How do we find the final value of mx? We take the antilog:
Here is a brilliant mathematical trick to solve this without a calculator: recognize that 1.2=4×0.3. Since we were given that 100.3=2, we can rewrite the expression:
101.2=104×0.3=(100.3)4=24=16
And there we have it! The final adsorbed concentration is exactly 16 mg g−1.