NUCLEAR CHEMISTRY NUCLEONS – The particles found in the nucleus Protons (+) Neutrons (0) ATOMIC NUMBER (Z) – The number of protons in the nucleus, also equal to the charge of the nucleus MASS NUMBER (A) – The number of nucleons in the nucleus, or protons plus neutrons in the nucleus 2F-1 (of 15) NUCLIDE – An atom with a specific number of protons and neutrons A 196 Hg Z 80 Protons: 80 Neutrons: 196 - 80 = 116 ISOTOPES – A set of nuclides with the same number of protons 196 Hg 80 and 2F-2 (of 15) 198 Hg 80 are isotopes NUCLEAR REACTIONS Reactions that produce new atoms TRANSMUTATION – When an atom of one element is changed into an atom of another element 14 N 7 + 4 He 2 → 17 O 8 + 1 H 1 Artificial elements are made by bombarding large nuclei with smaller ones 238 U 92 + 2 H 1 → 238 Np 93 + 2 01n In all nuclear reactions (1) the mass number is conserved and (2) atomic number (or charge) is conserved 2F-3 (of 15) STABILITY SERIES STABLE NUCLIDES (STABLE ISOTOPES) – Atoms with nuclei that last forever RADIOACTIVE NUCLIDES (RADIOISOTOPES) – Atoms with nuclei that eventually break down to more stable nuclei Nuclides are stable when their nuclei have enough neutrons to minimize proton-proton repulsion (a) For Z < 20 Stable nuclei have n:p ratio of 1:1 (b) For Z > 20 As Z increases, stable nuclei have n:p ratio that increases from 1:1 to eventually 1.5:1 2F-4 (of 15) Stable 16O atom: 8 n, 8 p (1:1 ratio) Stable 200Hg atom: 120 n, 80 p 1.5:1 ratio Nuclides to the left of the line of stability are unstable because they are neutron poor Nuclides to the right of the line of stability are unstable because they are neutron rich Nuclides beyond the line of stability (with Z > 83) are unstable because they have too many total protons 2F-5 (of 15) There are 284 known stable nuclides Neutrons Protons Even Odd Even 166 53 Odd 57 8 Most of the stable nuclides have even numbers of protons and neutrons 2F-6 (of 15) NUCLEAR DECAY – The process in which a radioactive nuclide turns into a more stable nuclide The type of decay depends on whether the radioactive nuclide has too many total protons, if it is neutron rich, or if it is neutron poor 2F-7 (of 15) (1) ALPHA DECAY (α) – The release of a helium-4 nucleus (4He2+) from a radioactive nucleus to become more stable α’s are emitted from radioisotopes beyond the line of stability, those with too many total protons (Z > 83 or A > 200) 238 U 92 → 4 α 2 + 234 Th 90 A and Z are always conserved in nuclear changes Alpha particles can be stopped by the outermost layer of skin 2F-8 (of 15) (2) BETA MINUS DECAY (β-) – The release of an electron from a radioactive nucleus to become more stable β-’s are emitted from radioisotopes that are to the right of the line of stability, those that are neutron rich Essentially a neutron decays into a proton and an electron 14 6 C → 0 -1 β- + 14 7 N Beta particles penetrate about 1 cm into the body 2F-9 (of 15) (3) ELECTRON CAPTURE (EC) – An electron is captured by the nucleus to become more stable EC occurs in radioisotopes to the left of the line of stability, those that are neutron poor Essentially an electron and a proton turn into a neutron 7 4 Be + 2F-10 (of 15) 0 -1 e- → 7 3 Li (4) POSITRON DECAY (β+) – The release of an electron with a positive charge from a nucleus to become more stable β+’s are just like electrons, but with a positive charge An electron is matter, but a β+ is ANTIMATTER When a β+ and β- meet, they are ANNIHILATED, meaning all of their mass is converted into energy A β+/β- annihilation forms 2 equal energy EM radiation photons 2F-11 (of 15) (4) POSITRON DECAY (β+) – The release of an electron with a positive charge from a nucleus to become more stable β+’s are emitted from radioisotopes to the left of the line of stability, those that are neutron poor Essentially a proton decays into a neutron and an antimatter electron 11 6 C → 2F-12 (of 15) 0 1 β+ + 11 5 B (5) GAMMA DECAY (γ) – The release of any high energy photon of electromagnetic radiation γ’s are emitted along with other forms of decay, or when an excited nucleus releases energy 40 K 19 163m Ho 67 → → 0 -1 β- + 0 0 γ + 40 Ca 20 163 67 + 0 γ 0 Ho Gamma rays are deeply penetrating 2F-13 (of 15) 2F-14 (of 15) (6) SPONTANEOUS FISSION – When a large nucleus (Z > 80) breaks into two, approximately equal halves Several neutrons, and lots of energy are released when nuclei fission 239 U 92 → 116 Ru 44 + 120 Cd 48 + 3 10n 239 U 92 → 118 Rh 45 + 119 Ag 47 + 2 10n Daughter Products usually very radioactive, and always different 2F-15 (of 15) THE RATE OF NUCLEAR DECAY Each radioisotope undergoes nuclear decay at its own unique rate HALF-LIFE (t1/2) – The time required for half of the radioisotopes in a sample to decay The shorter the half-life, the more unstable the radioisotope Half-life for 125I = 60 days At 0 days: 16 125I atoms 60 days: 8 125I atoms At 120 days: 4 125I atoms At 180 days: 2 125I atoms At 240 days: 1 125I atom At 2G-1 (of 17) Half-lives range from 1 x 10-21 seconds for 18Na 5 x 1015 years for 142Ce Common half-lives 5,730 years for 14C 4.5 x 109 years for 238U 2G-2 (of 17) THE DECAY EQUATION n = n0e-kt n0 = k = t = n = at time 0, number of atoms of a radioisotope (or g or disintegrations/time) decay constant of a radioisotope (disintegrations atom-1 time-1) time of decay at time t, number of atoms of a radioisotope (or g or disintegrations/time) 2G-3 (of 17) Half-life (t1/2) is the time needed so that ½ of n0 disintegrates n = n0e-kt n0 = n0e-kt1/2 ___ 2 1 = e-kt1/2 ___ 2 ln (1/2) = -kt1/2 ln 2 = kt1/2 ln 2 = t1/2 _____ k 2G-4 (of 17) or ln 2 = k _____ t1/2 THE DECAY EQUATION n = n0e-kt 2G-5 (of 17) n = n0e- (ln2/t1/2)t Calculate the mass of 110Ag remaining after 2.00 minutes if you start with 1.00 g 110Ag and its half-life is 24 seconds. n = n0e-(ln2/t1/2)t n and no can be anything proportional to the number of the radioactive atoms: (1) grams, (2) moles, (3) disintegrations per time, (4) percentages, or of course (5) atoms = (1.00 g)e-(ln2/24 s)(120. s) = 0.031 g 2G-6 (of 17) Starting with 2.00 g of a radioisotope, after 1.00 hour only 0.63 g remain. Calculate the half-life. n = n0e-(ln2/t1/2)t n = e-(ln2/t1/2)t ___ n0 ln (n/n0) = -(ln2/t1/2)t t1/2 = -(ln2)t __________ ln (n/n0) 2G-7 (of 17) = (ln2)t __________ ln (n0/n) = (ln2)(1.00 h) _____________________ ln (2.00 g/0.63 g) = 0.60 h CARBON DATING In the atmosphere 14 N 7 + 1 n 0 → 14 C 6 14 6C + O2 → 14 CO2 6 + 1 H 1 The carbon in all living organisms has the same percentage of 14C that the atmosphere has 15.3 dist. min-1 g-1 of carbon When an organism dies, it stops taking in 14C, so the percentage starts dropping 2G-8 (of 17) An axe with an elk antler sleve produces 4.8 cpm g-1 of carbon. How old is the axe? n = n0e-(ln2/t1/2)t n = e-(ln2/t1/2)t ___ n0 ln (n/n0) = -(ln2/t1/2)t t1/2 ln (n0/n) = t ______________ ln 2 2G-9 (of 17) = (5,730 y) ln (15.3 cpm g-1/4.8 cpm g-1) _______________________________________________ ln 2 = 9,600 y Much older objects can be dated with radioisotopes of longer half-lives 238U decays to 206Pb, so a material containing uranium can be dated by measuring the amount of 206Pb compared to 238U 2G-10 (of 17) A rock weighing 4.267 g contains 1.023 g 238U and 0.112 g 206Pb. Calculate the age of the rock. t1/2 ln (n0/n) = t = (4.5 x 109 y) ln (1.152 g/1.023 g) ______________ _______________________________________ ln 2 = 7.7 x 108 y ln 2 t1/2 = 4.5 x 109 y n = 1.023 g n0 = the original mass of 238U 0.112 g 206Pb x mol 206Pb x 1 mol 238U ______________ ______________ 206 g 206Pb 1 mol 206Pb = 0.129 g + 1.023 g = 1.152 g 2G-11 (of 17) x 238 g 238U _____________ mol 238U STABILITY OF NUCLEI Mass of proton + electron : Mass of neutron : 1.007825 amu 1.008665 amu Calculate the mass of a 23Na atom. 11 p+ + e12 n 11 x 1.007825 amu 12 x 1.008665 amu = = 11.086075 amu 12.103980 amu = 23.190055 amu Mass spectrometer data Mass 23Na 2G-12 (of 17) : 22.989773 amu BINDING ENERGY – The mass of an atom that has been converted into energy to hold the nucleus together Mass loss of a 23Na atom: 23.190055 amu – 22.989773 amu = 0.200282 amu Through E = mc2 mass units can be converted into energy units 1.000 amu = 1.492 x 10-10 J = 9.315 x 108 eV = 931.5 MeV 2G-13 (of 17) (Joule) (Electron Volt) (Million Electron Volt) 0.200282 amu x 931.5 MeV ______________ = 186.6 MeV 1.000 amu This is the BINDING ENERGY of the 23Na nucleus The stability of a nucleus is measured by its BINDING ENERGY PER NUCLEON 186.6 MeV ________________ 23 nucleons 2G-14 (of 17) = 8.113 MeV/nucleon Calculate the binding energy per nucleon for 56Fe if it has a mass of 55.934930 amu. 26 p+ + e30 n 26 x 1.007825 amu 30 x 1.008665 amu = = 26.203450 amu 30.259950 amu = 56.463400 amu 56.463400 amu – 55.934930 amu = 0.528470 amu 0.528470 amu x 931.5 MeV x 2G-15 (of 17) 1 ______________ _______________ 1.000 amu 56 nucleons = 8.791 MeV/nucleon 56Fe is the most stable atom When large atoms break down they release energy When small atoms combine they release energy 2G-16 (of 17) FUSION – The combining of small nuclei to produce large nuclei Fusion occurs in stars 4 11 H → 4 2 He Very high temperatures or pressure are needed to overcome the repulsion of the positive hydrogen nuclei Fusion releases much more energy than fission Stars can fuse atoms to create even atomic numbered elements all the way up to 56Fe 2G-17 (of 17) NUCLEAR REACTORS Nuclear reactions release over 100 times more energy than chemical reactions 235U is used as a fuel 235 U 92 236U + 1 0 n → 236 U 92 decays by spontaneous fission CHAIN REACTION – When at least one neutron per fission produces a new 236U 2G’-1 (of 4) Not enough neutrons are captured for a chain reaction Enough neutrons are captured to just maintain a chain reaction So many neutrons are captured the chain reaction is an explosion CRITICAL MASS – The minimum amount of 235U needed to support a chain reaction 2G’-2 (of 4) Water – Acts as a MODERATOR to slow down the neutrons, as a COOLANT to keep the reactor core from overheating, and as PROTECTION because it absorbs radiation Cd or B Control Rods – Absorb neutrons to control the rate of the chain reaction Fuel Elements – Metal casings containing 235U Reactor Core 2G’-3 (of 4) San Onofre Nuclear Generating Station Heat from the nuclear fission boils water, and steam turns a turbine, which produces electricity Used up full elements contain radioactive daughter products, which must be disposed of safely 2G’-4 (of 4)