Deck 5: Some Basic Nuclear Physics
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Deck 5: Some Basic Nuclear Physics
1
A simple method of calculating the age of the earth is based on the natural 

At the time the earth was created the ratio of uranium isotopes was
64
65
66
64
6566
2

54 3
Tabulate the number of neutrons, protons, and electrons for neutral atoms of 

The superscript gives
these elements to be 
these elements to be 
4
The total binding energy is a useful property for comparing the relative 

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5
Calculate the energy associated with the β+ decay process in equation (5.19).
Note: be careful counting electrons.
Note: be careful counting electrons.
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6
The measured decay rates of a radioactive material as a function of time are
shown in the table below.
(a) Calculate the half-life of the decay.
(b) Show that a semilogarithmic plot of the decay rate as a function of time is linear.
(c) Derive an analytical form of the linear relationship for part (b).
shown in the table below.
(a) Calculate the half-life of the decay.
(b) Show that a semilogarithmic plot of the decay rate as a function of time is linear.
(c) Derive an analytical form of the linear relationship for part (b).

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7
Using the energy stated in the text for the process in equation (5.28),
calculate the atomic mass of
calculate the atomic mass of

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8

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9
Calculate the energy associated with the process in equation (5.18)
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10
Assume carbon


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11

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12
Using the reaction energy given in the text for equation (5.27) calculate the 

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13
At t = 0 there are
nuclei of a particular nuclide in a sample. The 
nuclei of a particular nuclide in a sample. The 
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14

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15

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16

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17

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18

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19
Nuclide A has a half-life of 4 days, and nuclide B has a half-life of 16 days. 

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20
(a) Write the equation for the α-decay of


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