Quantum Theory
Planck’s radiation law
By
the end of the 19th century, physicists almost universally accepted the wave
theory of light. However, though the ideas of classical physics explain
interference and diffraction phenomena relating to the propagation of light,
they do not account for the absorption and emission of light. All bodies
radiate electromagnetic energy as
heat; in fact, a body emits radiation at all wavelengths. The energy radiated
at different wavelengths is a maximum at a wavelength that depends on the
temperature of the body; the hotter the body, the shorter the wavelength for
maximum radiation. Attempts to calculate the energy distribution for the
radiation from a blackbody using
classical ideas were unsuccessful. (A blackbody is a hypothetical ideal body or
surface that absorbs and reemits all radiant energy falling on it.) One
formula, proposed by Wilhelm Wien of
Germany, did not agree with observations at long wavelengths, and another,
proposed by Lord Rayleigh (John William Strutt) of England, disagreed with
those at short wavelengths.
In 1900 the German theoretical physicist Max Planck made a bold
suggestion. He assumed that the radiation energy is emitted, not continuously,
but rather in discrete packets called quanta. The energy E of
the quantum is
related to the frequency ν
by E = hν. The quantity h, now known as Planck’s constant, is a universal constant with the
approximate value of 6.62607 × 10−34 joule∙second. Planck showed that the calculated
energy spectrum then
agreed with observation over the entire wavelength range.
Einstein and the photoelectric effect
In 1905 Einstein extended Planck’s hypothesis to
explain thephotoelectric effect, which is the emission of electrons by a metal surface when it is
irradiated by light or more-energetic photons. The kinetic energy of
the emitted electrons depends on the frequency ν
of the radiation, not on its intensity; for a given metal, there is a threshold
frequency ν0 below which no electrons are emitted.
Furthermore, emission takes place as soon as the light shines on the surface;
there is no detectable delay. Einstein showed that these results can be
explained by two assumptions: (1) that light is composed of corpuscles or photons, the energy of which is given by Planck’s
relationship, and (2) that an atom in the metal can absorb either a whole photon or nothing. Part of the energy of the absorbed
photon frees an electron, which requires a fixed energy W,
known as the work function of
the metal; the rest is converted into the kinetic energy meu2/2 of the
emitted electron (me is
the mass of the electron and u is its
velocity). Thus, the energy relation is
If ν is less than ν0, where hν0 = W,
no electrons are emitted. Not all the experimental results mentioned above were
known in 1905, but all Einstein’s predictions have been verified since.
Bohr’s theory of the atom
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A
major contribution to the subject was made by Niels Bohr of
Denmark, who applied the quantum hypothesis to atomic spectra in 1913.
The spectra of light emitted by gaseous atoms had been studied extensively
since the mid-19th century. It was found that radiation from gaseous atoms at
low pressure consists of a set of discrete wavelengths. This is
quite unlike the radiation from a solid, which is distributed over a continuous
range of wavelengths. The set of discrete wavelengths from gaseous atoms is
known as a line
spectrum, because the radiation (light) emitted consists of a series of
sharp lines. The wavelengths of the lines are characteristic of the element and
may form extremely complex patterns. The simplest spectra are those of atomic
hydrogen and the alkali atoms (e.g., lithium, sodium, and potassium). For
hydrogen, the wavelengths λ are given by the empirical formula
where m and n are
positive integers with n > m and R∞, known as theRydberg constant, has the value 1.097373157 × 107 per metre. For a given value of m,
the lines for varying n form a series. The lines
for m = 1, the Lyman series, lie in the
ultraviolet part of the spectrum; those for m = 2,
the Balmer series,
lie in the visible spectrum; and those for m = 3,
the Paschen series, lie in the infrared.
Bohr started with a model suggested by the New
Zealand-born British physicist Ernest Rutherford. The model was based on the experiments ofHans Geiger and Ernest Marsden, who in 1909 bombarded gold atoms with massive, fast-moving alpha
particles; when some of these particles were deflected backward, Rutherford concluded
that the atom has a massive, charged nucleus. In Rutherford’s model, the atom
resembles a miniature solar system with the nucleus acting as the Sun and the
electrons as the circulating planets. Bohr made three assumptions. First, he
postulated that, in contrast to classical mechanics, where an infinite number of orbits is possible,
an electron can be in only one of a discrete set of orbits, which he
termed stationary states. Second, he postulated that the only orbits allowed are those for
which the angular momentum of the electron is a whole number n times ℏ (ℏ = h/2π). Third,
Bohr assumed that Newton’s laws of motion, so successful in calculating the paths of the
planets around the Sun, also applied to electrons orbiting the nucleus. The
force on the electron (the analogue of the gravitational force between the Sun
and a planet) is the electrostatic attraction between the positively charged
nucleus and the negatively charged electron. With these simple assumptions, he
showed that the energy of
the orbit has the form
where E0 is a
constant that may be expressed by a combination of the known constants e, me, and ℏ. While in a stationary state, the
atom does not give off energy as light; however, when an electron makes a transition from a state with
energy En to
one with lower energy Em, a quantum of energy is radiated with frequency ν, given by the
equation
Inserting the expression for En into this
equation and using the relation λν = c, where c is
the speed of light,
Bohr derived the formula for the wavelengths of the lines in the hydrogen
spectrum, with the correct value of the Rydberg constant.
Bohr’s
theory was a brilliant step forward. Its two most important features have
survived in present-day quantum mechanics. They are (1) the existence of
stationary, nonradiating states and (2) the relationship of radiation frequency
to the energy difference between the initial and final states in atransition.
Prior to Bohr, physicists had thought that the radiation frequency would be the
same as the electron’s frequency of rotation in an orbit.
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