* Your assessment is very important for improving the workof artificial intelligence, which forms the content of this project
Download Physics 2018: Great Ideas in Science: The Physics Module Quantum
Aharonov–Bohm effect wikipedia , lookup
Wheeler's delayed choice experiment wikipedia , lookup
Coherent states wikipedia , lookup
Bell's theorem wikipedia , lookup
Tight binding wikipedia , lookup
Atomic orbital wikipedia , lookup
Dirac equation wikipedia , lookup
Identical particles wikipedia , lookup
Quantum teleportation wikipedia , lookup
Schrödinger equation wikipedia , lookup
Quantum electrodynamics wikipedia , lookup
Probability amplitude wikipedia , lookup
Scalar field theory wikipedia , lookup
Quantum state wikipedia , lookup
Path integral formulation wikipedia , lookup
Wave function wikipedia , lookup
Interpretations of quantum mechanics wikipedia , lookup
Elementary particle wikipedia , lookup
Symmetry in quantum mechanics wikipedia , lookup
EPR paradox wikipedia , lookup
History of quantum field theory wikipedia , lookup
Renormalization wikipedia , lookup
Renormalization group wikipedia , lookup
Hydrogen atom wikipedia , lookup
Double-slit experiment wikipedia , lookup
Electron scattering wikipedia , lookup
Copenhagen interpretation wikipedia , lookup
Canonical quantization wikipedia , lookup
Particle in a box wikipedia , lookup
Hidden variable theory wikipedia , lookup
Relativistic quantum mechanics wikipedia , lookup
Bohr–Einstein debates wikipedia , lookup
Atomic theory wikipedia , lookup
Matter wave wikipedia , lookup
Wave–particle duality wikipedia , lookup
Theoretical and experimental justification for the Schrödinger equation wikipedia , lookup
Physics 2018: Great Ideas in Science: The Physics Module Quantum Mechanics Lecture Notes Dr. Donald G. Luttermoser East Tennessee State University Edition 1.0 Abstract These class notes are designed for use of the instructor and students of the course Physics 2018: Great Ideas in Science. This edition was last modified for the Fall 2007 semester. I. Quantum Mechanics A. Great Ideas in Physics. 1. Astronomy, the study of the night time sky, is the oldest of the sciences. a) Besides the sky, astronomy is the study of the objects that make up the solar system (our home system of the Sun), our home galaxy (the Milky Way), and the Universe as a whole. b) In an attempt to understand what was occurring in the night sky, humans invented a way to study the sky and nature in general called physics – the study and matter and energy and how these two interact with each other. 2. It is debatable as to which ideas in physics and astronomy are the most important, but such a list should include the following items: a) We live on a round planet called Earth – Eratosthenes (276–195 B.C.), an ancient Greek astronomer, was the first to accurately determine the diameter of this round Earth around 200 B.C. b) The solar system is heliocentric (i.e., Sun at the center) not geocentric (i.e., Earth at the center). i) Aristotle (384–322 B.C.) assumed the Earth was motionless and everything in the sky revolved around us. ii) Aristarchus of Samos (310–230 B.C.) reasoned that the Sun must be at the center. I–1 iii) In order to explain the periodic “backward” (i.e., retrograde) motion of the planets on the sky, Claudius Ptolemy, who lived around 140 A.D. and a firm believer in Aristotle’s philosophy, developed a geocentric system that had the planets revolving on smaller circles (called epicycles) whose “centers” orbited the Earth (with the larger circular orbits called deferents ). c) iv) In 1543, Nicholas Copernicus (1473–1543), a Polish astronomer and cleric, published his heliocentric model for the solar system where Earth was a planet, similar to the other planets, in circular orbit about the Sun =⇒ the Copernican Revolution. v) Johannes Kepler (1571–1630), a German mathematician and astronomer, modified the Copernican model by having the planets orbit the Sun in elliptical and not circular paths when he formulated the three laws of planetary motion. Invention of the scientific method owes much to the work of Galileo Galilei (1564–1642), an Italian astronomer and physicist. Galileo is considered to be the father of experimental physics. i) ii) Determined that objects of different masses fall at the same rate on the Earth’s surface (which contradicted the teachings of Aristotle). Came up with the concept of the pendulum clock. I–2 iii) iv) d) Developed the various concepts of motion. First to use the telescope to study the cosmos =⇒ discovered the 4 large moons of Jupiter (i.e., the Galilean moons), that Venus goes through phases (like our Moon), that the Moon’s surface wasn’t smooth, and that dark spots appear on the Sun (i.e., sunspots) from time to time. Isaac Newton (1642–1727), an English astronomer and physicist, was perhaps the greatest scientist whoever lived! The work he did is often referred to as the Newtonian Revolution. i) Invented calculus to describe his physics. ii) Developed the laws of motion. iii) Developed the law of gravity. iv) Invented the reflecting telescope. v) Developed many theories in optics and showed that white light is composed of the rainbow of colors. e) James Clerk Maxwell (1831–1879) was a Scottish mathematician and theoretical physicist from Edinburgh, Scotland and had two major impacts on physics. i) His most significant achievement was developing a set of equations that showed how electricity and magnetism are related =⇒ Maxwell’s equations. These equations merged the electric force and the I–3 magnetic force into one force called electromagnetism. ii) He also developed the Maxwell distribution, a statistical means to describe the number density of gases used in the kinetic theory of gases. f ) In 1905, Albert Einstein (1879–1955), a German physicist, rewrote Newton’s laws of motion in his Theory of Special Relativity. A bye-product of this theory was the famous equation E = mc2 =⇒ mass can be converted to energy and energy back to mass. g) In 1915, Einstein rewrote Newton’s law of gravity in his General Theory of Relativity. h) The quantum revolution began in the early part of the 20th century and has many people responsible for its development. Note that the word quantum means small individual packet or step. i) German physicist Max Planck (1858–1947) derived a formula describing blackbody radiation based on radiating atomic oscillators. ii) Danish physicist Niels Bohr (1885–1962) developed a quantum model for the hydrogen atom. iii) German physicist Werner Heisenberg (1901–1976) invented matrix mechanics, the first formalization of quantum mechanics in 1925, which he developed with the help of Max Born and Pascual Jordan. His uncertainty principle, developed in 1927, states that the simultaneous determination of two paired I–4 observable quantities, for example the position and momentum of a particle, has an unavoidable uncertainty. Together with Bohr, he formulated the Copenhagen interpretation of quantum mechanics. iv) In 1926 German physicist Erwin Schrödinger (1887–1961) published a paper on wave mechanics and what is now known as the Schrödinger equation. In this paper he gave a “derivation” of the wave equation for time independent systems, and showed that it gave the correct energy eigenvalues for the hydrogen-like atom. v) There are others that we could cite here, but the above four are the most important. i) From 1970 through 1973, particle physicists developed the Standard Model of particle physics which describes three of the four known fundamental interactions between the elementary particles that make up all matter. i) A large number of physicists were responsible for its development. ii) To date, almost all experimental tests of the three forces described by the Standard Model have agreed with its predictions. iii) Through the Standard Model all of the large variety of so-called “elementary” particles that have been discovered in particle accelerators can be explained as a composite of any of six quarks and six leptons. I–5 B. The Nature of Physics. 1. 2 main branches: a) Classical Physics: i) Classical Mechanics (also called Newtonian Mechanics). ii) Thermodynamics (the study of heat). iii) b) Fluid Mechanics (the study of fluids). iv) Electromagnetism (the study of electricity and magnetism). v) Optics (the interaction of light with lenses and mirrors). vi) Wave Mechanics (the study of wave motion). Modern Physics: i) Special Relativity and General Relativity. ii) Quantum Mechanics (also called Atomic Physics). iii) iv) v) Nuclear Physics. Statistical Mechanics (thermodynamics in terms of probabilities). Condensed Matter (once called Solid State Physics). I–6 2. In classical physics, matter moves (i.e., follows trajectories) as a result of a force being applied to it. a) Contact forces: Force exerted through a collision as described by Newton’s 2nd law of motion: F = ma. b) Field (or natural) forces: Force exerted on an object from its location in some natural potential field. There are 4 field forces in nature: Interaction Relative Strength Range Strong‡ 1 10−15 m Electromagnetic† ‡ 10−2 ∞ †‡ −6 −17 Weak 10 10 m −43 Gravitational 10 ∞ † - Under high energies, the electromagnetic and weak forces act as one — the Electroweak force. ‡ - Under even higher energies, all of the natural forces (except gravity) also may act as one, as described by the Grand Unified Theory. 3. There are 6 key definitions that are useful in the description of physics. a) Concept: An idea or physical quantity used to analyze nature (e.g., “space,” “length,” “mass,” and “time” are concepts). b) Laws: Mathematical relationships between physical quantities. c) Principle: A very general statement on how nature operates (e.g., the principle of relativity, that there is no absolute frames of reference, is the bases behind the theory of relativity). I–7 d) Models: A representation of a physical system (e.g., the Bohr model atom). e) Hypothesis: The tentative stages of a model that has not been confirmed through experiment and/or observation (e.g., Ptolomy’s model solar system). f ) Theory: Hypotheses that are confirmed through repeated experiment and/or observation (e.g., Newton’s theory of gravity). The word “theory” has different meanings in common English (i.e., it can mean that one is making a guess at something). However, it has a very precise meaning in science! Something does not become a theory in science unless it has been validated through repeated experiment as described by the scientific method. 4. At this point, we will differences between the classical view of physics and the quantum view of physics. C. The Classical Point of View. 1. A system is a collection of particles that interact among themselves via internal forces and that may interact with the world outside via external fields. a) To a classical physicist, a particle is an indivisible mass point possessing a variety of physical properties that can be measured. i) Intrinsic Properties: These don’t depend on the particle’s location, don’t evolve with time, and aren’t influenced by its physical environment (e.g., rest mass and charge). I–8 ii) Extrinsic Properties: These evolve with time in response to the forces on the particle (e.g., position and momentum). b) These measurable quantities are called observables. c) Listing values of the observables of a particle at any time =⇒ specify its state. (A trajectory is an equivalent way to specify a particle’s state.) d) The state of the system is just the collection of the states of the particles comprising it. 2. According to classical physics, all properties, intrinsic and extrinsic, of a particle could be known to infinite precision =⇒ for instance, we could measure the precise value of both position and momentum of a particle at the same time. 3. Classical physics predicts the outcome of a measurement by calculating the trajectory (i.e., the values of its position and momentum for all times after some initial (arbitrary) time t◦ ) of a particle: {~r(t), p~(t); t ≥ t◦ } ≡ trajectory, (I-1) where the linear momentum is, by definition, ~p(t) ≡ m d ~r(t) = m ~v (t) , dt (I-2) with m the mass of the particle. a) Trajectories are state descriptors of Newtonian physics. b) To study the evolution of the state represented by the trajectory in Eq. (I-1), we use Newton’s Second Law: X ~ = m ~a , F I–9 (I-3) P ~ is the sum of all vector forces acting on an obwhere F ject, m is the mass of an object, and ~a is the acceleration which results from the applied forces. We also can write this equation using differential calculus as m d2 ~r(t) = −∇V (~r, t) , dt2 (I-4) where V (~r, t) is the potential energy of the particle (as a function of radial distance r and time t) and ∇ is the socalled “del” operator (spatial derivatives in all directions). This equation reduces to d2 r dV (r) m 2 r̂ = − r̂ , dt dr (I-5) if the potential energy is time independent (note that r̂ is a unit vector in the radial direction). c) To obtain the trajectory for t > t◦ , one only need to know V (~r, t) and the initial conditions =⇒ the values of ~r and p~ at the initial time t◦ . d) Notice that classical physics tacitly assumes that we can measure the initial conditions without altering the motion of the particle =⇒ the scheme of classical physics is based on precise specification of the position and momentum of the particle. 4. From the discussion above, it can be seen that classical physics describes a Determinate Universe =⇒ knowing the initial conditions of the constituents of any system, however complicated, we can use Newton’s Laws to predict the future. 5. If the Universe is determinate, then for every effect there is a cause =⇒ the principle of causality. I–10 D. The Quantum Point of View. 1. The concept of a particle doesn’t exist in the quantum world — so-called particles behave both as a particle and a wave =⇒ wave-particle duality. a) The properties of quantum particles are not, in general, well-defined until they are measured. b) Unlike the classical state, the quantum state is a conglomeration of several possible outcomes of measurements of physical properties. c) Quantum physics can tell you only the probability that you will obtain one or another property. d) An observer cannot observe a microscopic system without altering some of its properties =⇒ the interaction is unavoidable : The effect of the observer cannot be reduced to zero, in principle or in practice. 2. This is not just a matter of experimental uncertainties, nature itself will not allow position and momentum to be resolved to infinite precision (see Figure I-1) =⇒ Heisenberg Uncertainty Principle (HUP): ∆x(t◦ ) ∆px(t◦ ) ≥ h̄ 1 h = , 2 2π 2 (I-6) where h = 6.62620 × 10−27 erg-sec = 6.626 × 10−34 J-sec is Planck’s Constant. a) ∆x(t◦ ) is the minimum uncertainty in the measurement of the position in the x-direction at time t◦ . b) ∆px (t◦ ) is the minimum uncertainty in the measurement of the momentum in the x-direction at time t◦ . I–11 ∆x <x> ∆p x <p> p Figure I–1: The results of measurement of the x components of the position and momentum of a large number of identical quantum particles. Each plot shows the number of experiments that yield the values on the abscissa. Results for each component are seen to fluctuate about a central peak, the mean value hxi and hpi. c) Similar constraints apply to the pairs of uncertainties ∆y(t◦), ∆py (t◦) and ∆z(t◦ ), ∆pz (t◦). d) Position and momentum are fundamentally incompatible observables =⇒ the Universe is inherently uncertain! e) The HUP strikes at the very heart of classical physics: the trajectory =⇒ obviously, if we cannot know the position and momentum of a particle at t◦ , we cannot specify the initial conditions of the particle and hence cannot calculate the trajectory. f ) Once we throw out trajectories, we can no longer use Newton’s Laws, new physics must be invented! I–12 Example I–1. Derive the energy-time uncertainty relation from the Heisenberg (position-momentum) Uncertainty Relation. Solution: A particle moves a distance ∆x in a time interval ∆t. These are related via the velocity equation ∆x = p ∆t . m Plugging this into Eq. (I-4) gives ∆x ∆p = p h̄ ∆t ∆p ≥ . m 2 Special relativity gives the energy of a particle is related to its momentum by E 2 = p2 c2 + m2◦ c4 , where m◦ is the rest mass of the particle. Taking the derivative of this equation with respect to momentum gives 2E dE = 2pc2 . dp Replacing the infinitesimal differentials with small changes in both E and p gives E p ∆p = 2 ∆E . c Substituting above gives h̄ E . ∆E ∆t ≥ mc2 2 Finally, using Einstein’s well known equation E = mc2 , we see that h̄ ∆E ∆t ≥ . (I-7) 2 I–13 3. Since Newtonian and Maxwellian physics describe the macroscopic world so well, physicists developing quantum mechanics demanded that when applied to macroscopic systems, the new physics must reduce to the old physics =⇒ this Correspondence Principle was coined by Niels Bohr. 4. Due to quantum mechanics probabilistic nature, only statistical information about aggregates of identical systems can be obtained. Quantum mechanics can tell us nothing about the behavior of individual systems. Moreover, the statistical information provided by quantum theory is limited to the results of measurements =⇒ thou shall not make any statements that can never be verified. E. Blackbody Radiation 1. In the early part of the 20th century, Max Planck asked the question: What is the spectrum of electromagnetic (EM) radiation inside a heated cavity ? More specifically, how does this spectrum depend on the temperature T of the cavity, on its shape, size, and chemical makeup, and on the frequency ν of the EM radiation in it? a) Earlier in the mid-19th century, Kirchhoff found that the energy inside such a cavity is independent of the physical characteristics of the cavity (i.e., size and shape), only ν and T were important. b) Planck was interested in the energy density in the cavity and sought an expression for the radiative energy density per unit volume ρ(ν, T ) and this density in the frequency range ν to ν + dν: ρ(ν, T ) dν. c) Kirchhoff called his model of a heated cavity in thermal equilibrium a “black-body radiator.” A blackbody is I–14 simply anything that absorbs all radiation incident upon it. Thus a blackbody radiator neither reflects nor transmits energy; it just absorbs or emits it. 2. Wien had already experimentally ascertained that the radiative energy density of a blackbody was proportional to ν 3 and, from R the work of Stefan, that the integrated energy density 0∞ ρ(ν, T ) dν is proportional to T 4 . a) Planck realized that ρ(ν, T ) could not solely depend upon ν 3 since this would imply that the energy density would blow up at small frequencies (i.e., long wavelengths). b) Planck focused on the exchange of energy between the radiation field and the walls of the cavity. i) He developed a simple model of this process by imagining that the molecules of the cavity walls are resonators — electrical charges undergoing simple harmonic motion. ii) As a consequence of their oscillations, these charges emit EM radiation at their oscillation frequency, which at thermal equilibrium, equals the frequency ν of the radiation field. iii) According to classical electromagnetic theory, energy exchange between the resonators and the energy field is a continuous process =⇒ the oscillators can exchange any amount of energy with the field, provided that the energy is conserved in the process. I–15 c) Planck deduced an empirical formula for the radiative energy density: Aν 3 ρ(ν, T ) = Bν/T . (I-8) e −1 i) A and B are constants that were to be determined by fitting experimental data. ii) The functional form of Eq. (I-8) agreed beautifully with observations. iii) In the limit of ν → ∞ and T → 0, Eq. (I-8) reduces to Wien’s law. iv) However, when Planck developed this functional form for blackbody radiation, be didn’t have a clue as to how to prove it theoretically. v) Planck made a second assault on the energy density by adopting a statistical method based upon the concept of entropy as interpreted probabilistically by Boltzmann. He also assumed in this treatment that only discrete amounts of energy can be absorbed or emitted by the resonators that comprise the walls of the blackbody. vi) He called these discrete amounts of energy quanta. To each quantum, Einstein took Planck’s idea and assigned an energy equal to an integral multiple of hν, where h is now referred to as Planck’s constant. I–16 d) Having made this assumption, Planck easily derived the radiation law: ρ(ν, T ) = 8πν 2 hν , c3 ehν/kT − 1 (I-9) where k is the above mentioned Boltzmann’s constant. As can be seen, Eq. (I-9) agrees with the empirical relation expressed in Eq. (I-8). e) The radiative energy density, ρ(ν, T ), is related to the monochromatic radiative energy flux Bν (T ) (i.e., the “brightness” of a glowing object) with the relation ρ(ν, T ) = 4π Bν (T ) . c (I-10) f ) As such, the monochromatic energy flux (or brightness) of a blackbody is Bν (T ) = 2hν 3 /c2 ehν/kT − 1 (I-11) in frequency space, where Bν is measured in J/s/m2 /Hz/sr (‘sr’ is the steradian unit) in SI units and erg/s/cm2 /Hz/sr in the cgs unit system. Since Bν dν = Bλ dλ and ν = c/λ, we can also write this function in wavelength space as Bλ (T ) = 2hc2 /λ5 . ehc/λkT − 1 (I-12) Both Eqs. (I-11) and (I-12) are called the Planck function (in frequency and wavelength space, respectively). 3. Planck’s radiation law not only solve the problem of blackbody radiation, it also opened the door to a new understanding of radiation energy in physics =⇒ quantum physics, also called quantum mechanics. I–17 F. The Semi-Empirical Model of Hydrogen. 1. Work that lead to an understanding of the spectrum of the hydrogen atom took place at the end of the 19th and beginning of the 20th century. As such, much of what of the work described in this and the next few subsections is presented in the cgs unit system since those are the units that were being used in physics at the time. 2. Rydberg (1890), Ritz (1908), Planck (1910), and Bohr (1913) were all responsible for developing the theory of the spectrum of the H atom. A transition from an upper level m to a lower level n will radiate a photon at frequency ! 1 1 2 νmn = c RA Z − , (I-13) n2 m2 where the velocity of light, c = 2.997925 × 1010 cm/s, Z is the effective charge of the nucleus (ZH = 1, ZHe = 2, etc.), and the atomic Rydberg constant, RA, is given by ! me −1 . (I-14) RA = R∞ 1 + MA a) The Rydberg constant for an infinite mass is 2π 2 me e4 R∞ = = 109, 737.31 cm−1 , (I-15) 3 ch where e = 4.80325 × 10−10 esu is the electron charge in cgs units. b) In atomic mass units (amu), the electron mass is me = 5.48597 × 10−4 amu whereas the atomic mass, MA , can be found on a periodic table (see also Table I-1). c) Eq. (I-13) can also be expressed in wavelengths (vacuum) by the following ! 1 1 1 2 = RA Z − . (I-16) λmn n2 m2 I–18 Table I–1: Atomic Masses and Rydberg Constants Atom Hydrogen, 1H Helium, 4 He Carbon, 12 C Nitrogen, 14 N Oxygen, 16 O Neon, 20Ne Atomic Mass, MA (amu) 1.007825 4.002603 12.000000 14.003074 15.994915 19.992440 Rydberg Constant, RA (cm−1 ) 109,677.6 109,722.3 109,732.3 109,733.0 109,733.5 109,734.3 3. Lines that originate from the same level in a hydrogen-like atom/ion are said to belong to the same series. Transitions out of (or into) the ground state (n = 1) are lines of the Lyman series, n = 2 corresponds to the Balmer series, and n = 3, the Paschen series. 4. For each series, the transition with the longest wavelength is called the alpha (α) transition, the next blueward line from α is the β line followed by the γ line, etc. a) Lyman α is the 1 ↔ 2 transition, Lyman β is the 1 ↔ 3 transition, Lyman γ is the 1 ↔ 4 transition, etc. b) Balmer or Hα is the 2 ↔ 3 transition, Hβ is the 2 ↔ 4 transition, Hγ is the 2 ↔ 5 transition, etc. 5. Lines that go into or come out of the ground state are referred to as resonance lines. 6. For one e− atoms (i.e., hydrogen-like: H I, He II, C VI, Fe XXVI, etc. =⇒ in astrophysics, ionization stages are labeled with Roman numerals: I = neutral, II = singly ionized, etc.), the principal (n) levels have energies of 2 π 2 m e4 Z 2 En = − , n2 h2 I–19 (I-17) 109678 13.60 100000 12.40 cm-1 eV Brackett 80000 9.92 Energy Paschen Wave Number 60000 Pfund Humphreys Balmer 7.44 Lyman H 40000 4.96 Hydrogen Z = 1 20000 2.48 0 0.00 Figure I–2: A partial Grotrian diagram of neutral hydrogen. The lowest 7 levels are shown with various transitions labeled. where Z = charge of the nucleus. a) Negative energies =⇒ bound states Positive energies =⇒ free states Ionization limit (n → ∞) in Eq. (I-17) has E = 0. b) In astronomical spectroscopy, the ground state is defined as zero potential (i.e., E1 = 0) and atomic states are displayed in terms of energy level diagrams (see Figure I–20 Efield wavecrest z y x Bfield direction of wave propagation λ Figure I–3: An electromagnetic wave. I-2), where the energy levels are determined by En = 13.6 Z 2 1 1− 2 n ! eV . (I-18) n → ∞ defines the ionization potential (IP) of the atom (or ion), so that for H: IP = 13.6 eV, for He II: IP = 54.4 eV, etc. c) NOTE: 1 eV = 1.602 × 10−19 J = 1.602x10−12 erg = 8066 cm−1 = 12,398 Å = 11,605 K. d) The lowest energy state (E = 0) is called the ground state. States above the ground are said to be excited. G. Emission and Absorption of Radiation. 1. Electromagnetic Waves. a) An electromagnetic (EM) wave consists of a transverse, and mutually perpendicular, oscillating electric and magnetic fields (see Figure I-3). b) An atom, in the presence of a passing EM wave, responds primarily to the electric component of the EM wave. I–21 c) i) If the wave is long as compared to the size of the atom, the spatial variation of the electric field can be ignored during the interaction. ii) This is the same thing as saying that the period of oscillation is long as compared to the time it takes the charge to move around (or within) the atom. As a result, the atom is essentially exposed to a purely sinusoidal oscillating electric field, E, of the form E = E◦ cos(ωt) ẑ , (I-19) where here the electric wave oscillates about the z axis with an amplitude of E◦ with an angular frequency ω = 2πν. d) The potential, φ, is related to the E field by E = −∇φ , (I-20) hence the potential must be a sinusoidal function as well. e) The potential of an EM wave passing a bound electron can perturb the potential energy Ve of said electron via the potential energy equation from classical EM theory: 1 (I-21) Ve = q φ , 2 where q is the charge of the electron. This oscillating perturbation then can cause the bound electron to change its state. 2. Absorption, Stimulated Emission, and Spontaneous Emission. a) We shall see later in the course that bound electrons in an atom are only found in certain energy states or levels. Each of these states are described by wave functions. I–22 i) The form of an electron wave function is solved with the partial differential equation called the Schrödinger equation (see §I.I). ii) The solution of this equation depends upon the potential energy of the given state. b) Bound electrons will jump from one state to another based upon the probability of the transition occurring. This probability is calculated from the wave function of the particle/state. c) Photon perturbations also can cause electrons to de-excite in an atom (called stimulated emission). d) From the HUP (∆E ∆t ≥ h̄/2), electrons also can deexcite spontaneously (i.e., spontaneous emission). i) ∆t represents the half-life of the time an electron stays excited before spontaneously decaying back to a lower energy state. ii) ∆E in HUP represents the “half-width” of the thickness of the energy probability distribution of a given state. For this natural broadening, this is typically nothing more than a Gaussian (i.e., normal) distribution. Note that ∆E = 0 for the ground state of an atom (or molecule) since an electron stays there indefinitely until perturbed by a passing photon. H. Matter and Energy: Particles or Waves? 1. In 1905, Einstein proposed that the energy in an EM field is not spread out over a spherical wavefront, as Maxwell had assumed, I–23 but instead is localized in indivisible clumps — in quanta. a) Each quantum of frequency ν travels through space at the speed of light c, carrying a discrete amount of energy hν and momentum hν/c. b) Thus Einstein formulated the particle view of light. c) G.N. Lewis subsequently dubbed Einstein’s and Planck’s quantum of radiation energy a photon, the name we use today. d) In Einstein’s view, not only is the radiation found in clumps, but the radiation field itself is quantized ! e) Einstein went on to use this photon model to describe the photoelectric effect — the ejection of electrons from a metal, such as sodium, when light impinges on it. Einstein won a Nobel Prize for his theory of the photoelectric effect. f ) Millikan reported a precise verification of Einstein’s equation of Planck’s quantized energy idea, E = hν, and the first measurement of the Planck constant, hence further showing the validity of the particle-like nature of light. g) In 1923, Compton published results of his X-ray scattering experiments, and drove the last nail in the coffin of the wave theory of light. Wavelength shifts were observed as the X-rays scattered of a thin carbon film which were inconsistent with Maxwell’s theory. However, the scattering was easily explained in the particle theory of light. 2. However, classical physics is filled with experiments that show light as a wave phenomenon: diffraction and interference are two such experiments. I–24 a) Light takes on whatever characteristic for which the experiment is testing. The observation gives the photon its identity! b) Light, having both wave and particle characteristics, is sometime jokingly referred to as a wavicle. 3. As this wave-particle debate continued for photons, a set of experimentalist set out to run known particles (e.g., electrons) through the same experiments that produce wave-like characteristics for light. a) Surprisingly, electrons also showed wave-like characteristics! b) When electrons are passed through a double slit, interference patterns arose on the detector that mimics the results for photons — the slits defracted the electrons. c) Electrons were found to have a wavelength of λ=√ h , 2mE (I-22) where m and E are the mass and energy of the electron, respectively. d) de Broglie came up with the answer — all microscopic material particles are characterized by a wavelength and a frequency, just like photons =⇒ matter waves. This idea led de Broglie, with the help of Einstein, to equations relating to the equality of matter and radiant energy. i) The photon is a relativistic particle of rest mass m◦ = 0 and its momentum is defined by p= E . c I–25 (I-23) ii) The energy of a photon is E = hν , (I-24) and using this in Eq. (I-23) gives p= hν . c (I-25) iii) For a wave in free space, the wavelength is λ = c/ν, so Eq. (I-25) becomes p= h . λ (I-26) iv) For a particle with mass traveling at relativistic velocities (in a zero potential energy field), its total energy is E 2 = p2 c2 + m2◦ c4 . (I-27) v) If its velocity is non-relativistic (v c), then its kinetic energy is simply p2 , T = 2m◦ (I-28) where T is the kinetic energy, or T = E − m◦ c2 . vi) (I-29) de Broglie proposed that Eqs. (I-24) and (I-26) be used for material particles as well as photons. Thus, for electrons, atoms, photons and all other quantum particles, the energy and momentum are related to the frequency and wavelength by p = h/λ E = hν de Broglie-Einstein equations. I–26 (I-30) vii) Notice that the de Broglie wavelength equation λ = h/p implies an inverse relationship between the total energy E of a particle and its wavelength, viz., hc/E λ= r (I-31) . m◦ c2 2 1− E If applied to a photon (by setting the rest mass to zero), this equation reduces to Eq. (I-24). Hence the larger the energy of a particle, the smaller is its wavelength, and vise versa. e) Trying to understand the meaning of these matter waves led Schrödinger and Heisenberg to create the physics of quantum mechanics. I. The Schrödinger Equation. 1. As previously mentioned, quantum mechanics approaches the trajectory problem of Newtonian mechanics quite differently. On a microscopic level, particles do not follow trajectories, but instead are characterized by their wave function, Ψ(x, t), where x is the 1-dimensional position of the wave function at time t. (Actually we would need to include all 3-dimensions, x, y, and z, in the wave function, but there’s no need to complicate this too much in this class.) a) The wave function is determined from Schrödinger’s Equation: ∂Ψ h̄2 ∂ 2 Ψ ih̄ =− +VΨ . (I-32) ∂t 2m ∂x2 √ i) Here, i = −1 (note that having an “i” in a function or a number makes it a “complex” function or number), h h̄ = = 1.054573 × 10−34 J s , 2π I–27 and ∂ is the symbol for a “partial” differential (which is covered in Calculus III). ii) b) Whereas Newton’s Second Law, F = ma, is the most important equation in all of classical physics, Eq. (I-32) is the most important equation in all of quantum physics. Given suitable initial conditions [typically, Ψ(x, 0)], the Schrödinger equation determines Ψ(x, t) for all future times, just as, in classical mechanics, Newton’s Second Law determines x(t) for all future times. 2. What exactly is the wave function, and what does it do for you once you got it? a) Whereas a particle is localized at a point in classical mechanics, a wave function is spread out in space =⇒ it is a function of x for any given time t. b) Born came up with a statistical interpretation of the wave function, which says that |Ψ(x, t)|2 gives the probability of finding the particle at point x, at time t, or more precisely, ( ) probability of finding the particle 2 |Ψ(x, t)| dx = between x and (x + dx) at time t. (I-33) c) The wave function itself is complex, but |Ψ|2 = Ψ∗Ψ (where Ψ∗ is the complex conjugate of Ψ) is real and nonnegative — as a probability must be. d) For the hypothetical wave function in Figure (I-4), you would be quite likely to find the particle in the vicinity of point A, and relatively unlikely to find it near point B. I–28 { | Ψ |2 dx A B C x Figure I–4: A hypothetical wave function. The particle would be relatively likely to be found near A, and unlikely to be found near B. The shaded area represents the probability of finding the particle in the range dx. 3. From the concept of the wave function, it becomes easier to see how the Heisenberg Uncertainty Principle arises in nature. The wave function will not allow you to predict with certainty the outcome of a simple experiment to measure a particle’s position — all quantum mechanics has to offer is statistical information about the possible results. 4. As can be seen from this section, to truly understand quantum mechanics, one must be skilled in handling partial differential equations and understanding the rules of statistics. One characteristic of wave functions that result from the solution of the Schrödinger Equation is that particles in negative energy states (called bound states) can only exist in discrete states described by quantum numbers: a) The principal quantum number (n) which is proportional to the total energy of a given bound state and idenI–29 tifies a given “shell” that a bound electron is in. b) The orbital angular momentum quantum number (`) which helps describes the orbital angular momentum (the classical analogy of an electron “in orbit” about a nucleus) of a given bound state and identifies a given “subshell” within a shell. c) The spin angular momentum quantum number (s) which helps describes the spin angular momentum (the classical analogy of an electron “spinning” about an axis just as the Earth spins about an axis). Note that there are only 2 spin states, “up” and “down” (the classical analogy of a counterclockwise versus a clockwise spin). d) The total angular momentum quantum number (j = ` ± s) which helps describes the total angular momentum. J. Philosophical Interpretations of Quantum Mechanics. 1. The Realist Position: a) We view the microscopic world as probabilistic due to the fact that quantum mechanics is an incomplete theory. b) The particle really was at a specific position (say point C in Figure I-4), yet quantum mechanics was unable to tell us so. c) To the realist, indeterminacy is not a fact of nature, but a reflection of our ignorance. d) If this scenario is, in fact, the correct one, then Ψ is not the whole story — some additional information (known as a hidden variable) is needed to provide a complete description of the particle. I–30 2. The orthodox position =⇒ the Copenhagen interpretation: a) The particle isn’t really anywhere in space. The act of the measurement forces the particle to take a stand — though how and why we dare not ask! b) Observations not only disturb what is to be measured, they produce it. c) Bohr and his followers put forward this interpretation of quantum mechanics. d) It is the most widely accepted position of the interpretation of quantum mechanics in physics. 3. The agnostic position: a) Refuse to answer! What sense can there be in making assertions about the status of a particle before a measurement, when the only way of knowing whether you were right is precisely to conduct the measurement, in which case what you get is no longer before the measurement. b) This has been used as a fall-back position used by many physicists if one is unable to convince another of the orthodox position. 4. In 1964, John Bell astonished the physics community by showing that it makes an observable difference if the particle had a precise (although unknown) position prior to its measurement. a) This discovery effectively eliminated the realist position. b) Bell’s Theorem showed that the orthodox position is the correct interpretation of quantum mechanics by proving that any local hidden variable theory is incompatible with I–31 quantum mechanics (see Bell, J.S. 1964, Physics, 1, 195). c) We won’t get into the details of Bell’s Theorem in this class. Suffice it to say that a particle does not have a precise position prior to the measurement, any more than ripples in a pond do =⇒ it is the measurement process that insists upon one particular number, and thereby in a sense creates the specific result. 5. The act of the measurement collapses the wave function to a delta function (e.g., a sharp peak) at some position — Ψ soon spreads out again after the measurement in accordance to the Schrödinger equation. I–32