Description and Uses
Lead is the 82nd element of the periodic table. It has been used as a common, unreactive metal for thousands of years. However, we now know that lead is both
poisonous and carcinogenic, so it has few uses in the modern world. In Roman times, it was known as “plumbum”, which is where its symbol “Pb” comes from.
Lead's main use was in pipes. The Romans used it to build large water pipes in cities across the empire. It was a cheap, easily malleable and long-lasting metal,
so perfect for its job. Many Roman lead water pipes still exist now, though they are slowly being replaced, usually with plastic.
One of lead's uses now is as a store of corrosive materials, such as sulfuric acid in lead batteries. This is due to its unreactivity, as it does not react to
the acid it stores.
Lead has 9 naturally occurring isotopes, with atomic weights ranging from 204 to 214. It has 4 observationally stable isotopes, being 204Pb,
206Pb, 207Pb, 208Pb, with 206Pb, 207Pb and 208Pb being at the end of the
uranium, actinium and
thorium decay series respectively. The most abundant lead isotope is 208Pb, with an abundance of
around 52%. It is also the heaviest stable isotope. Lead has 6 radioactive isotopes, with 214Pb having the shortest half-life, being just
26.8 minutes. 210Pb and 214Pb are parts of the uranium decay series; 207Pb and 211Pb are part of the actinium decay
series; and 208Pb and 212Pb are part of the thorium decay series. The remaining 209Pb occurs naturally as a part of the decay
of 237Np.