| MadSci Network: Science History |
In 1808 John Dalton published "A New System of Chemical Philosophy"
where he outlined his atomic theory of matter. Let's briefly write out
what that theory states.
Dalton's Atomic Theory
1. Matter consists of indivisible atoms.
2. All of the atoms of a given chemical element are identical in mass and
in all other properties.
3. Different chemical elements have different kinds of atoms; in
particular, their atoms have different masses.
4. Atoms are indestructible and retain their identities in chemical
reactions.
5. A compound forms from its elements through the combination of atoms of
unlike elements in small whole number ratios.
The first part of Dalton's theory was nothing really new. This idea
dates back to Greek times and seems almost intuitive. There has to be some
limit at which particles cannot be "divided" anymore. You can imagine a
leaf, a coin, or anything else. If you divide (or cut) that into smaller
pieces, eventually you will get a piece that can't be cut anymore - an
atom!
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Actually, this wasn't all that obvious to the ancients; most saw no reason
that matter could not be subdivided indefinitely. Greek atoms were purely
speculative!
-- Moderator
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But we can use scientific reasoning also to come upon this
conclusion. During Dalton's time, stoichiometry was just beginning to
develop. (Stoichiometry is the study of mass relationships in chemical
reactions). The fact that there is some regularity to chemical compounds
and reactions leads us to the idea that there must be small particles
(atoms!) combining in a regular way to produce compounds.
The second idea stems to a certain extent for the first idea. Let's
look at water as an example. Dalton knew that water was composed of
hydrogen and oxygen. Today we know the chemical formula to be H2O, but
Dalton believed the formula to be HO. Let's ignore the formula conflict
right now and pretend that water is made up of 1 oxygen atom and 1 hydrogen
atom. We know all water to be the same (same weight, same physical
properties). That is, a given molecule or a given volume of pure water
will weight the exact same amount. The only way this can be true is if we
assume that atoms of a given element all weigh the same and that hydrogen
and oxygen consistently have the same properties. If atoms of the same
element all have the same properties, given elements will always react the
same way given certain conditions. We can see how the third idea relates
to the second. It merely assumes that there are different elements.
The fourth idea tries to explain the law of conservation of mass and
can be related to an experiment performed by French chemist Antoine
Lavoisier. Lavoisier performed some of his experiments with mercury.
Essentially, he heated mercury with air in a sealed flask. After a few
days, mercury (II) oxide was produced. Lavoisier took a carefully weighed
amount of the mercury (II) oxide and heated it strongly. This reaction
produced elemental mercury and oxygen gas. After weighing the amount of
mercury and oxygen produced, Lavoisier noted that these products had the
same combined mass as the mercury (II) oxide he started with! Mass stayed
the same, so no matter was created or destroyed (no atoms were created or
destroyed). We can also see that atoms retain their identities in a
reaction. That is, we don't form any new elements in a chemical
reaction. We started with mercury (II) oxide, which we know contains
the elements mercury and oxygen, and we end up with elemental oxygen and
mercury after heating.
The fifth part of Dalton's theory pulls in something called the law of
definite proportions. This idea started as a debate between two prominent
French chemists, Claude Berthollet and Joseph Proust. Berthollet claimed
that given two samples of the same compound, those samples do not have to
have identical weights. For example, we know today that water contains
11.1% hydrogen by mass. According to Berthollet's idea, water will not
always be 11.1% hydrogen by mass, but rather the amount of hydrogen could
vary. Proust vehemently disagreed and claimed that Berthollet's
conclusions were the result of experimental error (for example, using a
scale that is not properly calibrated) and impurities in samples. So the
law of definite proportions essentially says that in a given chemical
compound, the proportions by mass of the elements that compose it are
fixed, independent of the origin of the compound or its mode or
preparation. For example, pure sodium chloride (better known as table
salt) will always contain 60.66% chlorine and 39.34% sodium by mass,
whether it is obtained from seawater, mines, or by synthesis in the
laboratory. From this we can draw another conclusion: elements will
combine in certain whole number ratios. (As a side note, today we know
that a few compounds - called berthollides - do not combine as whole number
ratios. This happens because some elements can accept different numbers of
electrons - that is, they have a wide variety of oxidation numbers. Iron
is one example.)
Though Dalton did rely on the experiments of others as proof for his
theory, he also did a lot of experimentation himself. He experimented
mostly with gases and used that data to support his ideas. Specifically,
he noted that water existed as a gas in air. Since two particles cannot
occupy the same space at the same time, he realized that the air and water
must somehow mix, and that the agents of mixing must be tiny particles
(atoms!).
As I found, the actual events that brought Dalton's atomic theory to
fruition are long and complicated. To list and describe the experiments
would require the length of a book, so I have tried to condense everything
a bit.
If you are curious, the information contained above is from a first
year college chemistry text:
Oxtoby, David W. and Norman H. Nachtrieb. "Principles of Modern Chemistry:
Third Edition." Fort Worth: Saunders College Publishing, 1996.
The following website also has information on Dalton's atomic theory.
http://antoine.fsu.umd.edu/chem/senese/101/atoms/dalton.shtml
If you are even more curious, I found another text that goes into
extreme (and sometimes confusing!) detail concerning Dalton's experiments
as well as reactions from some contemporary scientists:
Rocke, Alan J. "Chemical Atomism in the Nineteenth Century: From Dalton to
Cannizzaro." Columbus, OH: Ohio State University Press, 1984.
Try the links in the MadSci Library for more information on Science History.