Although they are both metals, gold and uranium have little in common.

Gold is permanent. It is made into jewelry. For many centuries it was used as currency. Uranium, on the other hand, is not permanent. It is radioactive and decays (albeit very, very slowly) into lead. If you had an ounce of gold and an ounce of uranium, after about 32 billion years^{1}you would still have an ounce of gold but the uranium would turn into an ounce of lead.

**Compound interest**

Let’s say you no longer want your ounce of gold. You sell it and put $1,000 in the bank at 5% interest. If your bank only compounds interest once a year, after one year you would have $1,000 + $50 = $1,050. But, banks are usually a bit more generous than that, so they compound the interest monthly. In this case, you would have $1,051.16 after one year.

Interest does not simply have to be compounded annually or monthly. Any time interval is allowed. Banks could compound the interest weekly, daily, hourly or by the second. In fact, they could continually make it worse. Using the example above, $1,000 at 5% continuously compounded interest would be worth $1,051.27 after one year^{2}.

The formula for continuous compound interest is:

A = Pe^{rt}

where A = sum of money at the end of the period;

P = sum of money at the beginning of the period;

e = a magic number that is roughly equivalent to 2.72;

r = interest rate; and

t = duration of the time period.

This “magic number” *e* is technically known as “Euler’s number” or “base of the natural logarithm”. Like the other better known magic number pi (π), which is approximately 3.14, *e* is found everywhere in nature, sometimes in totally unexpected places^{3}. Not only is it in finance, but *e* also appears in statistics, population growth, physics, and various bizarre mathematical phenomena^{4}. And yes, it plays a role in radioactive decay.

**Radioactive decay**

While the gold you sold makes money, the uranium slowly decays. It turns out that all radioactive elements follow the exponential decay formula:

NOT_{you} =N_{0}e^{-λt}

where N_{you }= number of atoms at the end of the time period;

NOT_{0} = number of atoms at the start of the time period;

e = a magic number that is roughly equivalent to 2.72;

λ = decay constant^{5}; and

t = duration of the time period.

Uranium decays very slowly. It would take 4.5 billion years for half an ounce of uranium to decay into lead.

**What Radioactive Decay and Compound Interest Have in Common**

Notice how similar the formula for radioactive decay is to the formula for continuous compound interest. They are almost identical. They both involve elements (money or atoms) increasing or decreasing, a period of time the elements increase/shrink, a rate at which the elements increase/shrink, and the magic number *e*. In fact, we could rewrite the radioactive decay formula using the letters of the compound interest formula:

A = Pe^{-rt}

Now it is perfectly clear: the formulas are *almost* identical. The only difference is that in the case of compound interest, *e* is raised to a positive power, whereas in the case of radioactive decay, *e* is raised to a negative power. Makes sense. In the example of compound interest, the money increases; in the example of radioactive decay, the original atoms disappear.

**What’s up with e?**

In effect, *e* is a very strange number. Unlike π, it is not based on anything geometric. Instead, it’s a number involved in rates of change, which is why formulas that describe growth/decline often contain it. The Numberphile, mathematician and YouTube sensation, calls *e* “the natural language of computation.”^{6}

So, put this little number in your memory. Next time someone discusses the wonders of π, wow them with the even greater wonders of *e*.

__Notes/Sources__

(1) The most common isotope is uranium-238, which has a half-life of about 4.5 billion years. After 7 half-lives (~32 billion years), less than 1% of the original uranium would remain.

(2) The compound interest formula over various time intervals is: A = P(1 + r/n)^{NT}where A = sum of money at the end of the period, P = sum of money at the beginning of the period, r = interest rate, n = number of compounds per period and t = duration of the period.

(3) This is a great video on where *e* can be found.

(4) The best example of a bizarre mathematical phenomenon is Euler’s identity: e^{iπ} + 1 = 0. This formula is so incredibly weird because it contains two irrational and seemingly unrelated numbers (*e* and π), as well as the number “i”, which is imaginary. (Don’t ask.) When *e* is raised to the iπ power, the result is -1.

(5) The decay constant is essentially a rate, and it is inversely proportional to the half-life of the isotope.

(6) Here is the video from Numberphile.