Nuclear Chemistry. The Nucleus. Isotopes. Slide 1 / 43. Slide 2 / 43. Slide 3 / 43

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Slide 1 / 43 Nuclear Chemistry The Nucleus Slide 2 / 43 Remember that the nucleus is comprised of the two nucleons, protons and neutrons. The number of protons is the atomic number. The number of protons and neutrons together is effectively the mass of the atom. Isotopes Slide 3 / 43 Not all atoms of the same element have the same mass due to different numbers of neutrons in those atoms. There are, for example, three naturally occurring isotopes of uranium: Uranium-234 Uranium-235 Uranium-238

Radioactivity Slide 4 / 43 It is not uncommon for some nuclides of an element to be unstable, or radioactive. We refer to these as radionuclides. There are several ways radionuclides can decay into a different nuclide. Slide 5 / 43 Types of Radioactive Decay Alpha Decay Slide 6 / 43 Alpha decay is the loss of an α-particle (a helium nucleus). 238 92 4 2He 234 4 U 90 U + He 2

Beta Decay Slide 7 / 43 Beta decay is the loss of a β-particle (a high energy electron). 0-1β or 0-1 e 131 53 131 0 I Xe + e 54-1 Positron Emission Slide 8 / 43 Some nuclei decay by emitting a positron, a particle that has the same mass as but an opposite charge to that of an electron. 11 6 0 1e 131 0 C 54 B + e 1 Gamma Emission Slide 9 / 43 This is the loss of a g-ray, which is high-energy radiation that almost always accompanies the loss of a nuclear particle. 0 # 0

Electron Capture (K-Capture) Slide 10 / 43 Addition of an electron to a proton in the nucleus is known as electron capture or K-capture. The result of this process is that a proton is transformed into a neutron. 1 1 1 p + e n 1-1 0 Neutron-Proton Ratios Slide 11 / 43 Any element with more than one proton (i.e., anything but hydrogen) will have repulsions between the protons in the nucleus. A strong nuclear force helps keep the nucleus from flying apart. Neutron-Proton Ratios Slide 12 / 43 Neutrons play a key role stabilizing the nucleus. Therefore, the ratio of neutrons to protons is an important factor.

Neutron-Proton Ratios Slide 13 / 43 For smaller nuclei (Z 20) stable nuclei have a neutron-to-proton ratio close to 1:1. Neutron-Proton Ratios Slide 14 / 43 As nuclei get larger, it takes a greater number of neutrons to stabilize the nucleus. Slide 15 / 43

Stable Nuclei Slide 16 / 43 The shaded region in the figure, the so-called belt of stability, shows what nuclides would be stable. Stable Nuclei Slide 17 / 43 Nuclei above this belt have too many neutrons. They tend to decay by emitting beta particles. Stable Nuclei Slide 18 / 43 Nuclei below the belt have too many protons. They tend to become more stable by positron emission or electron capture.

Slide 19 / 43 Stable Nuclei There are no stable nuclei with an atomic number greater than 83. Nuclei with such large atomic numbers tend to decay by alpha emission. Radioactive Series Slide 20 / 43 Large radioactive nuclei cannot stabilize by undergoing only one nuclear transformation. They undergo a series of decays until they form a stable nuclide (often a nuclide of lead). Some Trends Slide 21 / 43 Nuclei with 2, 8, 20, 28, 50, or 82 protons or 2, 8, 20, 28, 50, 82, or 126 neutrons tend to be more stable than nuclides with a different number of nucleons.

Some Trends Slide 22 / 43 Nuclei with an even number of protons and neutrons tend to be more stable than nuclides that have odd numbers of these nucleons. Nuclear Transformations Slide 23 / 43 Nuclear transformations can be induced by accelerating a particle and colliding it with the nuclide. Particle Accelerators Slide 24 / 43 These particle accelerators are enormous, having circular tracks with radii that are miles long.

Kinetics of Radioactive Decay Slide 25 / 43 Nuclear transmutation is a first-order process. The kinetics of such a process, you will recall, obey this equation: ln N t = -kt Kinetics of Radioactive Decay Slide 26 / 43 The half-life of such a process is: 0.693 k = t 1/2 Comparing the amount of a radioactive nuclide present at a given point in time with the amount normally present, one can find the age of an object. Measuring Radioactivity Slide 27 / 43 One can use a device like this Geiger counter to measure the amount of activity present in a radioactive sample. The ionizing radiation creates ions, which conduct a current that is detected by the instrument.

Kinetics of Radioactive Decay Slide 28 / 43 A wooden object from an archeological site is subjected to radiocarbon dating. The activity of the sample that is due to 14C is measured to be 11.6 disintegrations per second. The activity of a carbon sample of equal mass from fresh wood is 15.2 disintegrations per second. The half-life of 14C is 5715 yr. What is the age of the archeological sample? Kinetics of Radioactive Decay Slide 29 / 43 First we need to determine the rate constant, k, for the process. 0.693 k 0.693 k = t 1/2 = 5715 yr 0.693 5715 = k 1.21x10 4 yr -1 = k Kinetics of Radioactive Decay Now we can determine t: Slide 30 / 43 ln N t = -kt N 0 11.6 ln = -1.21x10 4 15.2 ln 0.763 = -1.21x10 4 6310 yr = t

Energy in Nuclear Reactions Slide 31 / 43 There is a tremendous amount of energy stored in nuclei. Einstein s famous equation, E = mc 2, relates directly to the calculation of this energy. Energy in Nuclear Reactions Slide 32 / 43 In the types of chemical reactions we have encountered previously, the amount of mass converted to energy has been minimal. However, these energies are many thousands of times greater in nuclear reactions. Energy in Nuclear Reactions Slide 33 / 43 For example, the mass change for the decay of 1 mol of uranium-238 is 0.0046 g. The change in energy, ΔE, is then ΔE = (Δm) c 2 ΔE = ( 4.6 x 10 6 kg)(3.00 x 10 8 m/s) 2 ΔE = 4.1 x 10 11 J

Nuclear Fission Slide 34 / 43 How does one tap all that energy? Nuclear fission is the type of reaction carried out in nuclear reactors. Nuclear Fission Slide 35 / 43 Bombardment of the radioactive nuclide with a neutron starts the process. Neutrons released in the transmutation strike other nuclei, causing their decay and the production of more neutrons. Nuclear Fission Slide 36 / 43 This process continues in what we call a nuclear chain reaction.

Nuclear Fission Slide 37 / 43 If there are not enough radioactive nuclides in the path of the ejected neutrons, the chain reaction will die out. Nuclear Fission Slide 38 / 43 Therefore, there must be a certain minimum amount of fissionable material present for the chain reaction to be sustained: critical mass. Nuclear Reactors Slide 39 / 43 In nuclear reactors the heat generated by the reaction is used to produce steam that turns a turbine connected to a generator.

Nuclear Reactors Slide 40 / 43 The reaction is kept in check by the use of control rods. These block the paths of some neutrons, keeping the system from reaching a dangerous supercritical mass. Nuclear Fusion Slide 41 / 43 Fusion would be a superior method of generating power. The good news is that the products of the reaction are not radioactive. The bad news is that in order to achieve fusion, the material must be in the plasma state at several million kelvins. Nuclear Fusion Slide 42 / 43 Tokamak apparati like the one shown at the right show promise for carrying out these reactions. They use magnetic fields to heat the material.

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