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Bohr Model of Atom

Bohr Model of Atom. Bohr proposed a model of the atom in which the electrons orbited the nucleus like planets around the sun Classical physics did not agree with his model. Why?

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Bohr Model of Atom

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  1. Bohr Model of Atom • Bohr proposed a model of the atom in which the electrons orbited the nucleus like planets around the sun • Classical physics did not agree with his model. Why? • To overcome this objection, Bohr proposed that certain specific orbits corresponded to specific energy levels of the electron that would prevent them from falling into the protons • As long as an electron had an ENERGY LEVEL that put it in one of these orbits, the atom was stable • Bohr introduced Quantization into the model of the atom

  2. Bohr Model of Atom By blending classical physics (laws of motion) with quantization, Bohr derived an equation for the energy possessed by the hydrogen electron in the nth orbit.

  3. Bohr Model of the Atom • The symbol n in Bohr’s equation is the principle quantum number • It has values of 1, 2, 3, 4, … • It defines the energies of the allowed orbits of the Hydrogen atom • As n increases, the distance of the electron from the nucleus increases

  4. Atomic Spectra and Bohr Energy of quantized state = - Rhc/n2 • Only orbits where n = some positive integer are permitted. • The energy of an electron in an orbit has a negative value • An atom with its electrons in the lowest possible energy level is at GROUND STATE • Atoms with higher energies (n>1) are in EXCITED STATES

  5. Energy absorption and electron excitation If e-’s are in quantized energy states, then ∆E of states can have only certain values. This explains sharp line spectra.

  6. Spectra of Excited Atoms • To move and electron from the n=1 to an excited state, the atom must absorb energy • Depending on the amount of energy the atom absorbs, an electron may go from n=1 to n=2, 3, 4 or higher • When the electron goes back to the ground state, it releases energy corresponding to the difference in energy levels from final to initial • E = Efinal - Einitital • E = -Rhc/n2 • E = -Rhc/nfinal2 - (-Rhc/ninitial2) = -Rhc (1/ nfinal2 - 1/ninitial2) • (does the last equation look familiar?)

  7. Origin of Line Spectra Balmer series

  8. Atomic Line Spectra and Niels Bohr Bohr’s theory was a great accomplishment. Rec’d Nobel Prize, 1922 Problems with theory — • theory only successful for H. • introduced quantum idea artificially. • So, we go on to QUANTUM or WAVE MECHANICS Niels Bohr (1885-1962)

  9. Wave-Particle Duality DeBroglie thought about how light, which is an electromagnetic wave, could have the property of a particle, but without mass. He postulated that all particles should have wavelike properties This was confirmed by x-ray diffraction studies

  10. Wave-Particle Duality de Broglie (1924) proposed that all moving objects have wave properties. For light: E = mc2 E = h = hc /  Therefore, mc = h /  and for particles: (mass)(velocity) = h /  L. de Broglie (1892-1987)

  11. Wave-Particle Duality Baseball (115 g) at 100 mph  = 1.3 x 10-32 cm e- with velocity = 1.9 x 108 cm/sec  = 0.388 nm • The mass times the velocity of the ball is very large, so the wavelength is very small for the baseball • The deBroglie equation is only useful for particles of very small mass

  12. 1.6 The Uncertainty Principle • Wave-Particle Duality • Represented a Paradigm shift for our understanding of reality! • In the Particle Model of electromagnetic radiation, the intensity of the radiation is proportional to the # of photons present @ each instant • In the Wave Model of electromagnetic radiation, the intensity is proportional to the square of the amplitude of the wave • Louis deBroglie proposed that the wavelength associated with a “matter wave” is inversely proportional to the particle’s mass

  13. deBroglie Relationship • In Classical Mechanics, we caqn easily determine the trajectory of a particle • A trajectory is the path on which the location and linear momentum of the particle can be known exactly at each instant • With Wave-Particle Duality: • We cannot specify the precise location of a particle acting as a wave • We may know its linear momentum and its wavelength with a high degree of precision • But the location of a wave? Not so much.

  14. The Uncertainty Principle • We may know the limits of where an electron will be around the nucleus (defined by the energy level), but where is the electron exactly? • Even if we knew that, we could not say where it would be the next moment • The Complementarity of location and momentum: • If we know one, we cannot know the other exactly.

  15. Heisenberg’s Uncertainty Principle • If the location of a particle is known to within an uncertainty ∆x, then the linear momentum, p, parallel to the x-axis can be simultaneously known to within an uncertainty, ∆p, where: = h/2 = “hbar” =1.055x10-34 J·s • The product of the uncertainties cannot be less than a certain constant value. If the ∆x (positional uncertainty) is very small, then the uncertainty in linear momentum, ∆p, must be very large (and vice versa) 

  16. Wavefunctions and Energy Levels • Erwin SchrÖdinger introduced the central concept of quantum theory in 1927: • He replaced the particle’s trajectory with a wavefunction • A wavefunction is a mathematical function whose values vary with position • Max Born interpreted the mathematics as follows: • The probability of finding the particle in a region is proportional to the value of the probability density (2) in that region.

  17. The Born Interpretation • 2 is a probabilty density: • The probability that the particle will be found in a small region multiplied by the volume of the region. • In problems, you will be given the value of 2 and the value of the volume around the region. 

  18. The Born Interpretation • Whenever 2 is large, the particle has a high probability density (and, therefore a HIGH probability of existing in the region chosen) • Whenever 2 is small, the particle has a low probability density (and, therefore a LOW probability of existing in the region chosen) • Whenever , and therefore, 2, is equal to zero, the particle has ZERO probability density. • This happens at nodes.

  19. SchrÖdinger’s Equation • Allows us to calculate the wavefunction for any particle • The SchrÖdinger equation calculates both wavefunction AND energy Potential Energy (for charged particles it is the electrical potential Energy) Curvature of the wavefunction

  20. Particle in a Box • Working with SchrÖdinger’s equation • Assume we have a single particle of mass m stuck in a one-dimensional box with a distance L between the walls. • Only certain wavelengths can exist within the box. • Same as a stretched string can only support certain wavelengths

  21. Standing Waves

  22. Particle in a Box • The wavefunctions for the particle are identical to the displacements of a stretched string as it vibrates. where n=1,2,3,… • n is the quantum number • It defines a state 

  23. Particle In a Box • Now we know that the allowable energies are : Where n=1,2,3,… • This tells us that: • The energy levels for heavier particles are less than those of lighter particles. • As the length b/w the walls decreases, the ‘distance’ b/w energy levels increases. • The energy levels are Quantized. 

  24. Particle in a Box:Energy Levels and Mass • As the mass of the particle increases, the separation between energy levels decreases • This is why no one observed quantization until Bohr looked at the smallest possible atom, hydrogen m1 < m2

  25. Zero Point Energy • A particle in a container CANNOT have zero energy • A container could be an atom, a box, etc. • The lowest energy (when n=1) is: Zero Point Energy • This is in agreement with the Uncertainty Principle: • ∆p and ∆x are never zero, therefore the particle is always moving

  26. Wavefunctions and Probability Densities • Examine the 2 lowest energy functions n=1 and n=2 • We see from the shading that when n=1, 2 is at a maximum @ the center of the box. • When n=2, we see that2 is at a maximum on either side of the center of the box

  27. Wavefunction Summary • The probability density for a particle at a location is proportional to the square of the wavefunction at the point • The wavefunction is found by solving the SchrÖdinger equation for the particle. • When the equation is solved to the appropriate boundary conditons, it is found that the particle can only posses certain discrete energies.

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