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! ----- 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 ----- 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.
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