THE mass of an atom is concentrated in a very small central portion
of the atom which is called the atomic nucleus. The atomic nucleus is made
up of electrically positive protons and electrically neutral
neutrons.
Surrounding the atomic nucleus are the electrically negative electrons.
The masses and charges of these three fundamental constituents of atoms
are given below:
Electron -1
0
Proton
+1
1
Neutron
0
1
Before moving further into this unit, link to:atoms02.htm.
For many of the chemical elements there are several known isotopes.
Isotopes are atoms with different atomic masses which have the same
atomic number. The atoms of different isotopes are atoms of the same
chemical element; they differ in the number of neutrons in the nucleus.
REMEMBER:
Atoms of the same chemical element do
not always have the same mass because, although the number of protons in
the nucleus is the same for all atoms of the same element, the number of
neutrons is not.
Most elements as they occur naturally on earth
are mixtures of several isotopes.
For example, the element hydrogen has atoms
that have one proton in the nucleus. This is the most common form
of hydrogen. Most of the atoms of hydrogen found in the Universe
are 1H. That is, they have an atomic number of one due
to the presence of single proton in the nucleus, and a mass of one
due to the presence of a single proton.
Occasionally, one finds and atom of hydrogen
in which a neutron has been incorporated into the nucleus. This isotope
of hydrogen is characterized by an atomic number of one (only one proton;
hydrogen can only have one proton in the nucleus), but an atomic mass of
two (one proton plus one neutron). This isotope of hydrogen is known
as "deuterium" or heavy hydrogen.
Finally, even rarer is the third isotope of
hydrogen [3H]. It has a mass of three which can only occur
from the presence of two neutrons in the nucleus. Remember, that
if there was another proton in hydrogen-3-it would not be hydrogen.
This final isotope of hydrogen is known as "tritium" and it is radioactive.
Later, we shall consider isotopes again when we consider the important question of atomic mass
Historical background. The atomic mass of an element is
a relative quantity. Originally the atomic mass of hydrogen, the lightest
of the elements, was taken to be one and the atomic masses of all other
elements were measured in relation to the atomic mass of hydrogen. This
later proved to have been a poor choice. Not only does hydrogen naturally
consist of more than one isotope, but there was the additional question
(particularly among early chemists) as to whether monatomic hydrogen or
diatomic hydrogen should be taken as having atomic mass one.
Can you see the problem?
If all hydrogen existed as a single atom (which it does not) it would
have been possible to use hydrogen as a basis for comparing its mass to
the mass of any other element. Hydrogen could have been taken as
one mass unit and everything else compared relative to hydrogen.
However, hydrogen has three isotopes and it occurs as diatomic hydrogen
(two atoms in a single molecule).
After some effort, and one major false start with oxygen, chemists and
physicists agreed on a common scale of relative atomic mass. Carbon of
isotopic mass twelve was assigned an atomic mass of exactly twelve, and
all other atomic masses whether of isotopes or of elements were specified
relative to carbon of atomic mass twelve. This had the effect of making
the relative atomic mass of hydrogen 1.0079...rather than exactly 1.0000....
The difference of less than 1% is too small to matter in many approximate
chemical calculations, but it is large enough to be significant when accurate
work must be done.
Do you understand?
Carbon-12 was taken as the standard and now everything is taken relative
to this single isotope of carbon. That is why hydrogen has an atomic
mass greater than unity.
YOU MUST MEMORIZE AVOGADRO'S NUMBER AND HAVE AN ABSOLUTELY CLEAR UNDERSTANDING OF EXACTLY WHAT IT MEANS AND WHY IT IS SO IMPORTANT IN MODERN CHEMISTRY
Chemists therefore distinguish the molar atomic mass of an isotope, which is the mass of one mole of the identical atoms which form that isotope, from the molar atomic mass of an element, which is the mass of one mole of the atoms of the various isotopes of that element having the natural abundance as they are found on earth.
I know that this is very difficult, but if you truly understand this
concept, then the following is clear to you:
Chemists deal with elements as they are naturally found, and so the
atomic mass of a particular isotope is of less interest than the weighted
mean molar atomic mass of the individual isotopes which is the molar
atomic mass of the naturally occurring element.
This property has open been called the atomic weight or chemical atomic weight of the element. The weighted mean molar atomic mass of an element as it naturally occurs will be referred to simply as the atomic mass of the element from now on.
Example. The relative abundance's of the isotopes 6Li and 7Li in naturally occurring lithium can be computed as follows. Their atomic masses are 6.0151214 and 7.0160030, respectively. The atomic mass of naturally occurring lithium given in the table of atomic mass or weight is 6.941.
If the relative abundance of 6Li is 7.5% and the relative abundance of 7Li is 92.5%, then the atomic weight of Lithium (for the entire population of lithium atoms) is:
(.075 x 6.0151214) + (.925 x 7.0160030) = 0.451 + 6.49 or 6.941Remember that this is a weighted average in which the contribution of each isotope is taken into account. The final atomic mass of Li is very close to the atomic mass of the 7Li isotope because so much of this isotope (as compared to 6Li) makes up the natural population of lithium atoms.