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An introduction to nuclear chemistry, including the discovery of X-rays and radioactivity, the work of Marie Curie and E.O. Lawrence, and important terms such as half-life, decay series, and nuclear fission. It also covers types of radiation, half-life problems, and nuclear equations. a useful study material for students interested in nuclear chemistry.
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radioactivity the spontaneous breakdown of atomic nuclei, accompanied by the release of some form of radiation (also called radioactive decay )
half-life time required for half of a radioactive sample to decay
transmutation one element being converted into another by a nuclear change
nuclides isotopes of elements that are identified by the number of their protons and neutrons
decay series the sequence of nuclides that an element changes into until it forms a stable nucleus
radioactive using half-life information to determine dating the age of objects. C-14/C-12 is common for organic artifacts. Uranium is common for rocks.
nuclear fission large nucleus breaking down into pieces of about the same mass
nuclear fusion two or more light nuclei blend to form one or more larger nuclei
Alpha particles are the same as a helium nucleus,
4 2 He, with a mass of 4 amu. It travels about 1/10th^ the speed of light and is the most easily stopped of the three particles (a sheet of paper will stop them). It is the least dangerous. Beta particles are high speed electrons, (^) −^01 e, with a mass of 0.00055 amu and travel at nearly the speed of light. They can be stopped by a sheet of aluminum. It is more penetrating and therefore more dangerous than alpha. Gamma rays are extremely high energy light, γ, with no mass, and are the most penetrating (several cm’s of lead are needed to stop them). They can cause severe damage.
In each half-life problem there are basically four variables:
Question : If you have 0.25 g of a radioactive substance with a half life of 3 days, how long ago did you have 64 grams? Answer: Draw the chart to determine the number of half- lives to get from the ending amount to the starting amount… each half-life is worth 3 days… 24 days.
Half-Life The time it takes for half of a radioactive substance to decay. The decay graph has a characteristic shape:
time
The time it takes for the amount of substance or the activity of the substance to drop to half is the same WHEREVER you start on the graph. This is a first-order reaction. Half-lives can range from microseconds to thousands of years and is characteristic of each substance.
Memorize the symbols for the important particles alpha beta positron neutron 4 2 He^
0 − 1 e^
0
1 0 n Decay means the particle is on the right side of the equation: example: alpha decay of U- 238 238 92 U^ →^
4 2 He +^
234 90 Th The 234 and 90 are calculated… the Th is found on the periodic table (find the element with atomic # = 90). Several neutrons can be shown together and written as… 3(^10 n) and would be counted as 30 n in the equation.
Certain values of p+’s and n°’s in the nucleus are stable. A nucleus can be unstable (radioactive) for 3 reasons:
When a problem involves whole numbers of half-lives, divide by 2 to determine the amounts involved. For other situations, the following equations are useful:
ln t
0
= kt and the special case for half-life, t½, where by
definition, [A]t = ½[A] 0 ln 2 = 0.693= kt½ [A] is the concentration (or activity) of the radioactive substance, t = time, k = the rate constant (the same that is in Rate Laws). Note: if you know the half-life, you can calculate the rate constant and vice-versa.
Once a nucleus decays, the daughter isotope is often unstable as well. Many decays may occur before a stable nucleus is formed. A classic example is U-238 that decays through 14 steps into stable Pb-206. Each step has a characteristic decay particle and half-life. This characteristic decay series is the method used to verify the identity of newly formed atoms. The fact that daughter products can be even more radioactive than the parent isotope adds to the problem of nuclear waste and its storage/disposal.
An useful characteristic of decay particles are that they ionize the air they pass through by striking atoms and knocking off electrons. Geiger counters use this idea. As radioactive particles pass through a chamber with two electrodes, ionized particles migrate to the + and - electrodes and complete the circuit. Smoke Detectors use a tiny piece of radioactive Am to keep a circuit flowing due to ionized particles. Smoke particles attract ionized particles, break the circuit, & set off the alarm. Brushes are kept ionized by tiny bits of radioactive material to more easily attract tiny bits of dust.
Uranium, Z=92, is the largest naturally-occurring element. Larger atoms were manufactured. Elements 93 and 94 were formed in atomic bomb tests and identified by Seaborg. Glenn Seaborg and Al Ghiorso at UC Berkeley were able to use E. O. Lawrence’s cyclotron to make larger atoms (95-103).
Some of these new elements have uses in the medical field as well as helping to further the understanding of the nucleus. For many of the larger elements, however, only a few atoms or even one atom formed. They were identified by their characteristic decay series.
As of July 2000, 118 is the largest element.