Everything about The Rutherford Model totally explained
The
Rutherford model or
planetary model was a model of the
atom devised by
Ernest Rutherford. Rutherford directed the famous
Geiger-Marsden experiment in (1909), which suggested to Rutherford's analysis (1911) that the
Plum pudding model (of
J. J. Thomson) of the atom was incorrect. Rutherford's new model for the atom, based on the experimental results, had a number of essential modern features, including a relatively high central charge concentrated into a very small volume in comparison to the rest of the atom.
Experimental basis for the model
In the
Geiger-Marsden experiment at Rutherford's laboratory,
alpha particles were used as a probe into atomic structure by being allowed to pass through a thin piece of
gold foil, then detected. Rutherford predicted that all of the particles would pass through the foil, or be deflected slightly. This is indeed what happened most of the time, but a few particles, 1 in 8000, bounced unexpectedly nearly straight back toward the source. This supported the hypothesis that atoms have a dense region containing most of their mass, and associated with a highly concentrated electric field (probably positive in nature), instead of spread-out positive or negative field. Rutherford thought it likely, on purely symmetric and aesthetic grounds, that such a region of dense charge and mass would be located in the atom's center. Such a region would then form a sort of atomic core.
In 1911, Rutherford came forth with his own physical model for subatomic structure, as an interpretation for the unexpected experimental results. In it, the atom is made up of a central charge (this is the modern
atomic nucleus, though Rutherford didn't use the term "nucleus" in his paper) surrounded by a cloud of orbiting
electrons. In this 1911 paper, Rutherford only commits himself to a small central region of very high positive or negative charge in the atom, but uses the following language for pictorial purposes:
"For concreteness, consider the passage of a high speed a particle through an atom having a positive central charge N e, and surrounded by a compensating charge of N electrons."
From purely energetic considerations of how far alpha particles of known speed would be able to penetrate toward a central charge of 100 e, Rutherford was able to calculate that the radius of his gold central charge would need to be less (how much less couldn't be told) than 3.4 x 10
-14 metres (the modern value is only about a fifth of this). This was in a gold atom known to be 10
-8 metres or so in radius--- a very surprising finding, as it implied a strong central charge less than 1/3000th of the diameter of the atom.
The Rutherford model didn't attribute any structure to the orbits of the electrons themselves, though it did mention the atomic model of
Hantaro Nagaoka, in which the electrons are arranged in one or more rings (this is the ONLY previous atomic model mentioned in Rutherford's 1911 paper).
The Rutherford paper suggested that the central charge of an atom might be "proportional" to its atomic mass in hydrogen mass units (roughly 1/2 of it, in Rutherford's model). For gold, this mass number is 197 (not then known to great accuracy) and was therefore modeled by Rutherford to be possibly 196. However, Rutherford didn't attempt to make the direct connection of central charge to atomic number, since gold's place on the periodic table was known to be about 79, and Rutherford's more tentative model for the structure of the gold nucleus was 49 helium nuclei, which would have given it a mass of 196 and charge of 98. This differed enough from gold's "atomic number" (at that time merely its place number in the periodic table) that Rutherford didn't formally suggest the two numbers might be exactly the same.
Successor model
The Rutherford model of the atom was soon superseded by the
Bohr atom, which used some of the early
quantum mechanical results to give locational structure to the behavior of the orbiting electrons, confining them to certain circular (and later eliptical) planar orbits. In the Bohr model, expanding on the work of
Henry Moseley, the central charge was identified as being directly connected with the
atomic number (that is, the element's place on the periodic table). Since the Bohr model is an improvement on the Rutherford model in this and other ways, some sources combine the two, referring to the Bohr model as the Rutherford-Bohr model. However, even an atom with a core containing an atomic number of charges was the work of a number of men, including those mentioned, and also lesser known workers such as
Antonius Van den Broek.
The Rutherford model was important because it essentially proposed the concept of the nucleus, although this word isn't used in the paper. What Rutherford notes as the (probable) concomitant of this results, is a "concentrated central charge" in the atom: "Considering the evidence as a whole, it seems simplest to suppose that the atom contains a central charge distributed through a very small volume, and that the large single deflexions are due to the central charge as a whole, and not to its constituents." The central charge containing most of the atom's positive charge, invariably later become associated with a concrete structure, the atomic nucleus.
]], the study of the atom branched into two separate fields,
nuclear physics, which studies the nucleus of the atom, and
atomic physics which studies atom's electronic structure.
Symbolism
Despite its inaccuracy, the Rutherford model caught the imagination of the public in a way that the more correct Bohr model did not, and has continually been used as a symbol for atoms and atomic energy. Examples of its use over the past century include:
Key points of Rutherford model
The electron clouds of the atom don't influence alpha scattering.
A large number of the atom's charges, up to a number equal to about half the atomic mass in hydrogen units, are concentrated in very small volume at the center of the atom. These are responsible for deflecting both alpha and beta particles.
The mass of heavy atoms such as gold is mostly concentrated in the central charge region, since calculations show it isn't deflected or moved by the high speed alpha particles, which have very high momentum in comparison to electrons, but not with regard to heavy atoms (such as gold) on the whole. This suggests that much of the mass of atoms is concentrated in their centres.
The Rutherford model's contribution to modern science
After this discovery, scientists started to realize that the atom isn't ultimately a single particle, but is made up of far smaller subatomic particles. Later workers began research to figure out the exact atomic structure which lead to Rutherford’s gold foil experiment. They eventually discovered that atoms have a positively-charged nucleus (with an exact atomic number of charges) in the center, with a radius of about 1.2 x 10-15 meters x [AtomicMass Number]1/3. Since electrons were found to be even smaller, this meant that the atom consists of mostly empty space.
Later on, scientists found the expected number of electrons (the same as the atomic number) in an atom by using X-ray beams. When an X-ray passes through an atom, some of it's scattered, while the rest passes through the atom. Since (in many cases with X-rays of the proper frequency) the X-ray loses its intensity primarily due to electron scattering, by noting the rate of decrease in X-ray intensity, the number of electrons contained in an atom could be estimated accurately.
Further Information
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