Some notes on Atomism, 1806-1860
The principal problem confronting the development of a suitable atomic weight
scale was the concept that "molecules" of elements i.e. O2,
N2, Cl2, etc. could not form. This concept was principally
due to John Dalton. Dalton referred to "simple" atoms and
"compound atoms", compound atoms being our molecules. Great confusion
reigned through most of the nineteenth century regarding such terminology, one
man's atom being another man's molecule. The need for a common language
developed slowly. Those present at the Karlsruhe Conference in 1860 were
presented with the following question at the top of the agenda.
| "Shall a difference be made between the expressions molecule
and atom, such that a molecule be named the smallest particle of bodies
which can enter into chemical reactions and which may be compared to
each other in regard to physical properties -- atoms being the smallest
particles of those bodies which are contained in molecules." |
Even in 1860 no consensus was reached. Part of the original problem was
Dalton's insistence that atoms of the same kind could not react together. This
was reinforced by the electrochemical researches of Davy and Faraday which added
the concept that metals were positive and non-metals negative e.g. non-metals
would repel each other especially those of the same kind. On top of this, when
atoms did combine there was no way of telling in what atomic ratio they
combined.
A guiding principal was the "Rule of Greatest Simplicity"
which said that the most stable compound between elements would be the 1:1
atomic ratio. Relative combining weights could be measured e.g. 8 g of
oxygen combined with 1 g of hydrogen. Water being the most stable (the only)
compound between these two elements the formula was HO. This meant the relative
atomic weight for oxygen would be 8. There were several compounds between
nitrogen and oxygen known to Dalton.
- N2O, NO, and NO2 for instance. The most stable of
these would be NO. The other compounds between these two elements could form
giving other formulas based on the weight ratios found and "Law of
Multiple Proportions".
The solution to the problem presented by Cannizzaro at Karlsruhe and debated
afterward was solved using two ideas from the early 1800s. These were:
- Gay Lussac's "Law of Combining Volumes" - In 1809 Gay Lussac
presented his "Law of Combining Volumes of Gases", an experimental
result which said "Whenever gases react or gases form under the same
conditions of temperature and pressure they do so in the ratio of small
whole numbers."
- Avogadro's Hypothesis - In 1811 A. Avogadro published what is now known as
Avogadro's hypothesis, a theoretical result. This said that "equal
volumes of gases under the same conditions of temperature and pressure
contain equal numbers of molecules".(1809 Gay Lussac, 1811 Avogadro)
Dalton and many others would not accept the implications of these. The
arguments using these two ideas are the following.
1) Suppose nitrogen reacts with oxygen to form NO, according to Dalton.
N + O -----> NO. Gas volumes measure the following ratios:
1 volume N + 1 volume O ----> 2 Volumes NO. According to Avogadro's
Hypothesis using one atom or molecule in each volume (equal numbers) (consider
each box to be a volume with the same volume as every other box.)
This does NOT fit the hypothesis but
does fit because now there are the same number of atoms of each element on
each side of the equation; i.e. the equation is balanced and the reaction obeys
the Law of Conservation of Mass, one of Dalton's rerequirements.
Therefore elemental nitrogen must be diatomic, elemental oxygen must
be diatomic.
2) The same result is obtained for water.
H + O -----> HO (vapor)
from Gay-Lussac:
2 volumes H + 1 volume O -----> 2 volumes water vapor
from Avogadro:
works for H & H2O but not for O but
works for all three. Therefore hydrogen must be H2, oxygen O2
and water H2O.
The H2O formula for water would mean that if the atomic weight for
H were 1, then oxygen must be 16 and not 8. Other arguments can be made for the
solution to other elements which we now take to be diatomic, Cl2, F2
etc.
The solution to this problem ultimately led to a correct scale of
atomic weights.