Now
that we have acquired some fundamental ideas about atomic structure, we can
more thoroughly discuss the concept of chemical elements. All atoms of a
particular element have the same atomic number, Z, and, conversely, all
atoms with the same number of protons are atoms of the same element. The
elements shown on the inside front cover have atomic numbers from Z = 1 to
Z = 112. Each element has a name and a distinctive symbol. Chemical symbols
are one- or two-letter abbreviations of the name (usually the English
name). The first (but never the second) letter of the symbol is capitalized;
for example: carbon, C; oxygen, O; neon, Ne; and silicon, Si. Some elements
known since ancient times have symbols based on their Latin names, such as Fe
for iron (ferrum) and Pb for lead (plumbum). The element sodium
has the symbol Na, based on the Latin natrium for sodium carbonate.
Potassium has the symbol K, based on the Latin kalium for potassium carbonate.
The symbol for tungsten, W, is based on the German wolfram. Elements
beyond uranium (Z = 922) do not occur naturally and must be synthesized in
particle accelerators. Elements of the very highest atomic numbers have been produced
only on a limited number of occasions, a few atoms at a time. Inevitably,
controversies have arisen about which research team discovered a new element and,
in fact, whether a discovery was made at all. However, international agreement
has been reached on the first 112 elements; each one, except element 112, has
an official name and symbol.
Isotopes
To represent the
composition of any particular atom, we need to specify its number of protons
(p), neutrons (n), and electrons (e). We can do this with the symbolism
This
symbolism indicates that the atom is element E and that it has atomic number Z
and mass number A. For example, an atom of aluminum represented as Al has 13 protons and
14 neutrons in its nucleus and 13 electrons outside the nucleus. (Recall that
an atom has the same number of electrons as protons.)
Contrary
to what Dalton thought, we now know that atoms of an element do not necessarily
all have the same mass. In 1912, J. J. Thomson
measured the mass-to-charge ratios of positive ions formed from neon atoms.
From these ratios he deduced that about 91% of the atoms had one mass and that
the remaining atoms were about 10% heavier. All neon atoms have 10 protons in their
nuclei, and most have 10 neutrons as well. A very few neon atoms, however, have
11 neutrons and some have 12. We can represent these three different types of
neon atoms as
Atoms
that have the same atomic number (Z) but different mass
numbers (A) are called isotopes. Of all Ne atoms on Earth, 90.51% are Ne. The percentages of Ne and Ne are 0.27% and 9.22%,
respectively. These percentages 90.51%, 0.27%, 9.22% are the percent natural
abundances of the three neon isotopes.
Sometimes
the mass numbers of isotopes are incorporated into the names of elements, such
as neon-20 (neon twenty). Percent natural abundances are always based on numbers,
not masses. Thus, 9051 of every 10,000 neon atoms are neon-20 atoms. Some
elements, as they exist in nature, consist of just a single type of atom and
therefore do not have naturally occurring isotopes.* Aluminum, for example,
consists only of aluminum-27 atoms.
Ions
When
atoms lose or gain electrons, for example, in the course of a chemical reaction,
the species formed are called ions and carry net charges. Because an electron is
negatively charged, adding electrons to an electrically neutral atom produces a
negatively charged ion. Removing electrons results in a positively charged ion.
The number of protons does not change when an atom becomes an ion. For example,
22Ne+ and 22Ne2+ are ions. The
first one has 10 protons, 10 neutrons, and 9 electrons. The second one
also has 10 protons, but 12 neutrons and 8 electrons. The charge on an
ion is equal to the number of protons minus the number of electrons.
That is
Another example is the 16O2- ion. In this ion,
there are 8 protons (atomic number 8), 8 neutrons (mass number - atomic number),
and 10 electrons (18 - 10 = -22).
Isotopic Masses
We
cannot determine the mass of an individual atom just by adding up the masses of
its fundamental particles. When protons and neutrons combine to form a nucleus,
a very small portion of their original mass is converted to energy and
released. However, we cannot predict exactly how much this so called nuclear
binding energy will be. Determining the masses of individual atoms, then, is
something that must be done by experiment, in the following way. By
international agreement, one type of atom has been chosen and assigned a
specific mass. This standard is an atom of the isotope carbon-12, which is
assigned a mass of exactly 12 atomic mass units, that is, 12 u. Next, the
masses of other atoms relative to carbon-12 are determined with a mass spectrometer.
In this device, a beam of gaseous ions passing through electric and magnetic
fields separates into components of differing masses. The separated ions are focused
on a measuring instrument, which records their presence and amounts. Figure below
illustrates mass spectrometry and a typical mass spectrum.
Although
mass numbers are whole numbers, the actual masses of individual atoms (in
atomic mass units, u) are never whole numbers, except for carbon-12. However, they
are very close in value to the corresponding mass numbers, as we can see for the
isotope oxygen-16. From mass spectral data the ratio of the mass of 16O
to 12C is found to be 1.33291. Thus, the mass of the oxygen-16 atom
is
1.33291
X 12 u = 15.9949 u
Which
is very nearly equal to the mass number of 16.
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