History of Quantum Theory At the turn of the 20th century, classical physics was well defined and physicists thought they could explain all naturally occurring phenomena. • X-rays were discovered (Roentgen). • Radioactivity of Uranium salts (Bequerel). • Plank proposes E=hv (light as quantized energy packets) • Einstein provides another example of the quantization of energy when he explains the photoelectric effect. • Rutherford’s gold foil experiment, J.J. Thompson’s plum pudding goes bad. • Bohr puts it all together to explain the absorption spectrum of hydrogen. Photoelectric effect In 1905, Einstein further solidified the idea of quantized energy packets. Basically, he showed that it took a certain amount or threshold of energy (certain frequency) to kick an electron out of a metal. In the photoelectric effect, it takes a single photon to emit a single electron. Any excess energy goes into the kinetic energy of the emitted electron. Additional photons eject additional electrons. 3 Rules for Electron Configurations: 1. Aufbau principle 2. Pauli exclusion principle 3. Hund’s rule Angular momentum (orbital) quantum number, l, give the sublevel (s, p, d, f) l = 0, 1, 2, 3 1/2 life Xo = original amount X = amount remaining after time t ln .6 Xo = - k t Xo k = .693 = 1.21 x 10-4 5720 ln .6 = - 1.21 x 10-4 t t = 4220 years Ion Size As with atoms, the size of ions increases as you go down the periodic table and decreases as you go across, if you consider cations and anions separately. However , when you switch from cations to anions in a horizontal row, the size increases. Ionization energy: This is the energy required to remove the outermost electron. The bigger the difference between the shielded nucleus and the outer electrons the bigger I.E. Watch out for jumps that occur because of orbital stability issues. Like when you lose a lone p-electron and then try to remove the next electron from an s-sublevel. That will require a big jump in energy because the s-sublevel is of lower energy and more stable. The higher energy p-electron takes less energy to remove. Also, each successive electron requires more I.E. Remember cations are smaller than atoms, so outer electrons are held more tightly by nucleus. Lewis Structures 1. Count total number of valence electrons (add electron for negative ions, subtract for positive ions.) 2. Divide by two to get number of electron pairs. 3. Determine central atom (usually lowest electronegativity; never hydrogen) 4. Place one pair between each pair of bonding atoms (sigma bonds) 5. Assign electron pairs to terminal atoms to complete octets. 6. Assign any extra electrons to central atom. 7. If central atom does not have octet, you may complete the octet by forming double bonds if atoms are O, C., S, N, or P. Intermolecular Forces Vapor Liquid Equilibrium Equilibrium is dynamic. Things don’t stop happening, they just stop changing. Vapor Pressure: The pressure exerted by the vapor above a liquid when the liquid and vapor are in equilibrium. Vapor pressure depends upon temperature. The higher T, the easier time molecules have leaving the liquid phase. Vapor pressure is independent of the volume of the system. Boiling point: eq vapor pressure = pressure of atmosphere. The vapor pushes back the atmosphere. Critical Phenomena Critical temperature: the temperature above which vapor cannot be liquefied not matter what pressure is applied. Critical pressure: Pressure required to produce liquefaction at critical temperature. Phase Diagrams Be able to tell what is happening on the lines Identify the triple point. Triple point of water is 0.01C. Identify phase changes: evaporation, fusion, sublimation Raoult’s Law Raoult’s Law allows you to calculate the partial pressure that a species will exert when it is a component of a solution. We know that a pure liquid exerts a vapor pressure. This equation allows you to find the pressure exerted by all members in a solution.. PA = XAPo This just says that the partial pressure of species A (PA) is equal to the mole fraction of species A in the solution (XA ) times the vapor pressure of pure A (Po ) at the specified temperature. Henry’s Law Henry’s Law is less emphasized than Raoult’s Law but you should still know what it is. Henry’s Law says that the solubility of a gas in a liquid is directly proportional to the partial pressure of the gas over the solution. Cg = k Pg You often have to solve for k, the Henry’s Law constant at one set of conditions and then calculate the solubility (Cg) at another pressure (Pg ). (large # of e-) Dipole Determining rate laws from concentration vs initial rate data. These problems assume initial rates where concentrations are constant. Determining rate laws from concentration vs time data. For these problems, the concentration is constantly changing. These problems are a little harder than concentration vs rate problems because you have to look at the behavior of the entire data set to determine the rate relationship. The whole name of the game here is what form of the concentration of reactant A, [A}, do you need to plot against time, t, in order to get a linear relationship. Solutions and Colligative Properties Mass % Solute ppm mass solute X 100% total mass solution mass solute = total mass soln ppb X 106 g mass solute = total mass soln X 109 Remember that when you add something to a solution you change the total mass of the solution. You have to keep track of what you add, not just the amount of solvent that you start with. Molarity, M M = moles solute liters of solution Molarity is almost always used for concentration in chemistry problems. [ A ] square brackets mean the concentration of A in molarity. Be able to relate moles and volume MV = n (molarity x volume = moles) Molarity Dilution Mc Vc = Md Vd Molality, m m= moles solute kilograms solvent Freezing and Boiling Point Change Tf = kfmi Tb = kbmi Here it doesn’t matter how much solute you add, it’s always based upon the number of kilograms of solvent present. Use molality in colligative properties problems, i.e. boiling point elevation, freezing point depression