Simultaneous And Series Disintegration

Simultaneous And Series Disintegration

Edited By Vishal kumar | Updated on Jul 02, 2025 07:01 PM IST

Simultaneous and series disintegration are fundamental concepts in nuclear physics that describe the decay processes of unstable nuclei. In simultaneous disintegration, a single nucleus decays into two or more different products at the same time, whereas in series disintegration, a nucleus undergoes a sequence of decays, producing intermediate products before reaching a stable state. These processes are essential for understanding the behaviour of radioactive materials, which have practical applications in fields such as medical imaging and treatment, nuclear energy production, and radiocarbon dating in archaeology. In this article, we will discuss the concept of Simultaneous decay, series decay and related examples it.

This Story also Contains
  1. Simultaneous Decay
  2. Series Decay
  3. Solved Examples Based on Simultaneous and Series Disintegration
  4. Summary

Simultaneous Decay

Simultaneous decay, also known as simultaneous disintegration, occurs when a single unstable nucleus decays into two or more different products at the same time. This process is less common compared to series decay, where a nucleus undergoes a series of decays, but it provides valuable insights into the behaviour of certain isotopes and the interactions between subatomic particles.

As we know due to radioactive disintegration, a radio nuclide transforms into its daughter nucleus. Depending on the nuclear structure and its instability, a parent nucleus may undergo either $\alpha-$ or $\beta$-emission. Sometimes a parent nucleus may undergo both types of emission simultaneously.

If an element decays to different daughter nuclei with different decay constants etc. for each decay mode, then the effective decay constant of the parent nuclei can be given as

$\lambda_{e f f}=\lambda_1+\lambda_2+\lambda_3, \ldots$

Similarly, a radioactive element with decay constant $\lambda$ which decays by both $\alpha-$ and $\beta-$ decays given that the probability for an $\alpha$--emission is $\mathrm{P}_1$ and that for $\beta-$ emission is $\mathrm{P}_2$ the decay constant of the element can be split for individual decay modes. Like in this case the decay constants for $\alpha$ - and $\beta-$ decay separately can be given as

$\begin{aligned} & \lambda_\alpha=P_1 \lambda \\ & \lambda_\beta=P_2 \lambda\end{aligned}$

Series Decay

Series decay, also known as decay chains or radioactive series, refers to a sequence of radioactive decays where a parent isotope decays into a daughter isotope, which in turn decays into another isotope, and this process continues until a stable isotope is formed. This type of decay is fundamental in understanding the transformation and stability of elements over time.

Accumulation of Radioactive Elements in Radioactive Series

The accumulation of radioactive elements in a radioactive series, also known as a decay chain, occurs as a parent isotope decays into a series of daughter isotopes until a stable isotope is reached. Each step in the decay chain involves a specific type of radioactive decay (alpha, beta, or gamma decay) and results in the formation of a new element.

A radioactive element decays into its daughter nuclei until a stable element appears. Consider a radioactive series.

$A_1 \xrightarrow{\lambda_1} A_2 \xrightarrow{\lambda_2} A_3 \xrightarrow{\lambda_3} \ldots$

A radioactive element $A_1$ disintegrates to form another radioactive element $A_2$ which in turn disintegrates to another element $A_3$ and so on. Such decays are called Series or Successive Disintegration.

Here, the rate of disintegration of $A_1=$ Rate of formation of $A_2$
$
\begin{gathered}
\frac{-d N_{A 1}}{d t}=\frac{d N_{A 2}}{d t}=\lambda_1 N_{A 1} \\
\frac{-d N_{A 2}}{d t}=\frac{d N_{A 3}}{d t}=\lambda_2 N_{A 2} \\
\frac{d N_{A 1}}{d t}=-\lambda_1 N_{A 1} \\
\frac{d N_{A 2}}{d t}=-\lambda_2 N_{A 2}
\end{gathered}
$

Therefore, net formation of $A_2=$ Rate of disintegration of $A_1$ - Rate of disintegration of $A_2$
$
=\lambda_1 N_{A 1}-\lambda_2 N_{A 2}
$

If the rate of disintegration of $A_1$ becomes equal to the Rate of disintegration of $A_{2 \text {, }}$ then it is called Radioactive equilibrium. So the equation becomes -
$
\Rightarrow \frac{\lambda_1}{\lambda_2}=\frac{N_{A 2}}{N_{A 1}}=\frac{T_{a v g 2}}{T_{a v g 1}}=\frac{\left(T_{\frac{1}{2}}\right)_2}{\left(T_{\frac{1}{2}}\right)_1}
$

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Solved Examples Based on Simultaneous and Series Disintegration

Example 1: The half-life of radioactive substances is 1620 years and 405 years for $\alpha$ emission and $\beta$ emission respectively. Time (in years) during which half of the sample will decay if both $\alpha$ and $\beta$ emission are simultaneous is:

1) 324

2) 405

3) 1620

4) 2025

Solution:

The effective decay constant is when nuclei decay into more than one product at one time.

$
\begin{aligned}
\lambda & =\lambda_1+\lambda_2=\frac{0.693}{T}=\frac{0.693}{T_1}+\frac{0.693}{T_2} \\
\frac{1}{T} & =\frac{1}{T_1}+\frac{1}{T_2} \\
\frac{1}{T} & =\frac{1}{1620}+\frac{1}{405} \\
\frac{1}{T} & =\frac{5}{1620}
\end{aligned}
$

OR $T=324$ years
Hence, the answer is option(1).

Example 2: A radioactive nuclei with a decay constant of $0.5 / \mathrm{s}$ is being produced at a constant rate of 100 nuclei/s. If at $t=0$, there were no nuclei, the time when there are 50 nuclei is :
1) 1 s
2) $2 \ln \left(\frac{4}{3}\right) \mathrm{s}$
3) $\ln 2 s$
4) $\ln \left(\frac{4}{3}\right) s$

Solution:

At any time
$
t: \frac{d N}{d t}=N_o-\lambda N
$
$N_o=$ Rate of production
$
\begin{aligned}
& -\lambda N=\text { Rate of decay } \\
& { }_o^N \int \frac{d N}{N_o-\lambda N}=\int_o^t d t \\
& \text { or } \frac{-1}{\lambda} \ln N_o-\lambda N \int_o^N=t \\
& \text { or } \ln \left(\frac{N_o-\lambda N}{N_o}\right)=-\lambda t \\
& 1-\frac{\lambda N}{N_o}=e^{-\lambda t} \\
& \text { or } N=\frac{N_o}{\lambda}\left(1-e^{-\lambda t}\right) \\
& \text { or }
\end{aligned}
$
given $N=50, N_o=100, \lambda=0.5$
$
\begin{aligned}
& \Rightarrow 50=\frac{100}{0.5}\left(1-e^{-\lambda t}\right) \\
& \frac{1}{4}=1-e^{-0.5 t} \text { or } \frac{3}{4}=e^{-0.5 t}
\end{aligned}
$
taking log;
$
\ln \left(\frac{4}{3}\right)=0.5 t
$
or $t=2 \ln \frac{4}{3} s$

Hence, the answer is the option (2).

Example 3: A radioactive nucleus decays by two different processes. The half-life of the first process is 5 minutes and that of the second process is 30 s . The effective half-life of the nucleus is calculated to be $\frac{\alpha}{11} \mathrm{~s}$. The value of $\alpha$ is $\qquad$ .

1) 300

2) 400

3) 500

4) 600

Solution:

$\begin{aligned} & \frac{\mathrm{dN}}{\mathrm{dt}}=-\left(\lambda_1+\lambda_2\right) \mathrm{N} \\ & \lambda_{\text {eq }}=\lambda_1+\lambda_2 \\ & \frac{1}{\mathrm{t}_{\frac{1}{2}}}=\frac{1}{300}+\frac{1}{30}=\frac{11}{300} \\ & \mathrm{t}_{1 / 2}=\left(\frac{300}{11}\right) \mathrm{sec}\end{aligned}$

Hence, the answer is option (1).

Example 4: A radioactive nucleus undergoes a series of decay according to the scheme
$
\mathrm{A} \xrightarrow{\alpha} \mathrm{A}_1 \xrightarrow{\beta} \mathrm{A}_2 \xrightarrow{\alpha} \mathrm{A}_3 \xrightarrow{\gamma} \mathrm{A}_4
$

If the mass number and atomic number of $A$ are 180 and 72 respectively, these numbers of $\mathrm{A}_4$ are:

1) 172, 69

2) 177, 69

3) 171, 69

4) 172, 68

Solution:

Decrease in mass number due to two $\alpha=2 \times 4=8$
Decrease in charge number due to two $\alpha=4$
Increase in charge number due to one $\beta=1$
Net decrease in charge number $=4-1=3$
$\gamma$ affects neither.
$\therefore \quad$ For $A_4, A=180-8=172$
$
Z=72-3=69
$

Hence, the answer is the option (1).

Example 5: The mean lives of a radioactive sample are 30 years and 60 years for $\alpha$ emission and $\beta$-emission respectively. If the sample decays both by $\alpha$-emission and -emission simultaneously, the time after which, only one-fourth of the sample remains:

1) 14 years

2) 20 years

3) 28 years

4) 45 years

Solution:

Here, $\lambda_{(\alpha+\beta)}=\lambda_\alpha+\lambda_\beta$
$
\begin{aligned}
& \frac{1}{\tau}=\frac{1}{\tau_\alpha}+\frac{1}{\tau_\beta} \quad\left(\text { As } \lambda=\frac{1}{\tau}\right) \\
& \Rightarrow \frac{1}{\tau}=\frac{1}{30}+\frac{1}{60}=\frac{1}{20} \\
& \therefore \quad \tau=20 \text { years }
\end{aligned}
$

Now, $\mathrm{T}_{1 / 2}=\ln (2) \tau=13.86$ years
One-fourth of the sample will remain after 2 half-life $=27.72$ years.
Hence, the answer is the option (3).

Summary

Simultaneous and series disintegration are crucial concepts in nuclear physics that describe the decay processes of unstable nuclei. Simultaneous decay involves a single nucleus decaying into multiple products at the same time, providing insights into the behaviour of certain isotopes. In contrast, series decay, or radioactive series, involves a sequence of decays where a parent isotope transforms into a series of daughter isotopes until a stable form is achieved.

Frequently Asked Questions (FAQs)

1. How does series disintegration differ from simultaneous disintegration?
Series disintegration involves a sequence of radioactive decays, where a parent nucleus decays into a daughter nucleus, which then decays further into other nuclei. This process continues until a stable nucleus is reached. In contrast, simultaneous disintegration occurs when a nucleus splits into multiple fragments at once.
2. What is a decay chain?
A decay chain is a series of radioactive decays that occur sequentially, starting from a parent nucleus and ending with a stable nucleus. Each step in the chain involves the decay of one nucleus into another, with the process continuing until a stable isotope is reached. Decay chains are examples of series disintegration.
3. What is the significance of half-life in series disintegration?
Half-life is crucial in series disintegration as it determines the rate at which each step in the decay chain occurs. In a series of decays, each nuclide has its own half-life, which affects the overall rate of the decay chain. Understanding half-lives helps predict the abundance of intermediate nuclides and the time required to reach the stable end product.
4. What is transient equilibrium in a decay series?
Transient equilibrium occurs in a decay chain when the half-life of the parent nucleus is longer than, but not significantly longer than, the half-life of its daughter. In this case, the ratio of parent to daughter nuclei approaches a constant value over time, but the absolute amounts of both continue to decrease.
5. How does the concept of secular equilibrium apply to series disintegration?
Secular equilibrium occurs in a decay chain when the half-life of the parent nucleus is much longer than that of its daughters. In this state, the decay rate of each daughter nuclide becomes equal to that of the parent, creating a balance where the amount of each daughter remains constant over time, despite ongoing decay.
6. What is simultaneous disintegration in radioactive decay?
Simultaneous disintegration occurs when a radioactive nucleus decays into two or more daughter nuclei at the same time. This process is different from sequential decay, where one decay product forms and then subsequently decays. In simultaneous disintegration, the parent nucleus splits into multiple fragments simultaneously.
7. Can you explain the concept of branching in radioactive decay?
Branching in radioactive decay occurs when a radioactive nucleus can decay through multiple pathways. Each pathway has a certain probability, and the sum of all branching probabilities equals 100%. For example, a nucleus might have a 70% chance of decaying by beta emission and a 30% chance of decaying by alpha emission.
8. What is the importance of conservation laws in simultaneous and series disintegration?
Conservation laws, particularly those of energy, momentum, and charge, must be obeyed in all nuclear processes. In simultaneous and series disintegration, these laws govern the possible decay modes, the energies of emitted particles, and the characteristics of daughter nuclei. They are fundamental to understanding and predicting decay processes.
9. What is the role of gamma radiation in series disintegration?
Gamma radiation often accompanies alpha and beta decays in series disintegration. It does not change the atomic or mass number but represents the release of excess energy as the nucleus transitions from an excited state to a lower energy state. Gamma emission helps stabilize the nucleus after particle emission.
10. How do branching ratios affect the products of a decay series?
Branching ratios determine the proportion of nuclei that decay through different pathways. In a decay series, these ratios influence the relative abundances of different daughter nuclei and can lead to multiple possible end products. Understanding branching ratios is crucial for predicting the composition of decay products over time.
11. How does the concept of radioactive equilibrium apply to dating techniques?
Radioactive equilibrium, particularly secular equilibrium, is important in radiometric dating techniques. When a system reaches equilibrium, the ratio of parent to daughter isotopes becomes constant. This principle is used in dating methods like uranium-lead dating, where the equilibrium state can provide information about the age of geological samples.
12. How does the shell model of the nucleus explain the stability patterns observed in decay series?
The shell model of the nucleus explains why certain nuclei are more stable than others, based on the filling of nuclear energy levels. In decay series, nuclei tend to decay towards configurations with filled shells, which are more stable. This model helps explain why certain numbers of protons or neutrons (magic numbers) lead to increased stability in decay chains.
13. What is the role of isomeric transitions in decay series?
Isomeric transitions occur when an excited nucleus in a metastable state decays to a lower energy state of the same nucleus. In decay series, these transitions can create branching points where the decay can proceed through different paths. Isomeric transitions often involve gamma emission or internal conversion and can significantly affect the overall decay scheme.
14. How do delayed neutron emissions affect the progression of a decay series?
Delayed neutron emissions occur when certain neutron-rich nuclei, formed as products of fission or other nuclear reactions, emit neutrons after their initial decay. In a decay series, these emissions can create branching points and affect the neutron economy of the system. Understanding delayed neutrons is crucial in nuclear reactor physics and in predicting the behavior of complex decay chains.
15. What is the significance of the "missing" stable astatine isotope in the natural decay series?
Astatine is the heaviest halogen, and interestingly, it has no stable isotopes. In natural decay series, particularly the uranium and thorium series, astatine isotopes appear as short-lived intermediates. The absence of a stable astatine isotope is due to the interplay between nuclear and atomic forces, highlighting the limits of nuclear stability for heavy elements.
16. What is the significance of the island of stability in the context of decay series for superheavy elements?
The island of stability is a theoretical region in the chart of nuclides where superheavy elements might have significantly longer half-lives due to nuclear shell effects. For decay series involving superheavy elements, reaching this island could result in unexpected longevity for certain isotopes. This concept is crucial in the ongoing search for and study of new superheavy elements and their decay properties.
17. How does the atomic number change during series disintegration?
In series disintegration, the atomic number changes differently depending on the type of decay at each step. Alpha decay decreases the atomic number by 2, beta minus decay increases it by 1, and beta plus decay decreases it by 1. The final atomic number depends on the specific sequence of decays in the chain.
18. What is the difference between artificial and natural radioactive series?
Natural radioactive series occur in nature and typically start with long-lived isotopes like uranium-238 or thorium-232. Artificial radioactive series are created in laboratories, often starting with man-made isotopes. While natural series end in stable lead isotopes, artificial series can have various endpoints depending on the starting nucleus.
19. How does the mass number change during a decay series?
The mass number changes differently for various decay types in a series. Alpha decay reduces the mass number by 4, while beta decay (both β- and β+) does not change the mass number. The total change in mass number from the beginning to the end of a decay series depends on the number and type of decays that occur.
20. How does the binding energy per nucleon relate to the stability of nuclei in a decay chain?
The binding energy per nucleon generally increases as a decay chain progresses towards more stable nuclei. Nuclei with higher binding energy per nucleon are more stable. In a decay series, each step typically results in daughter nuclei with slightly higher binding energy per nucleon, explaining why the series tends towards more stable configurations.
21. What is the significance of the N/Z ratio in predicting decay modes in a series?
The neutron-to-proton (N/Z) ratio is an important factor in nuclear stability. As a decay series progresses, nuclei tend to adjust their N/Z ratio towards the line of stability. This trend can help predict likely decay modes: nuclei with too many neutrons tend to undergo β- decay, while those with too many protons often undergo β+ decay or electron capture.
22. How do decay constants relate to the rate of series disintegration?
Decay constants (λ) represent the probability of decay per unit time for a given isotope. In series disintegration, each step has its own decay constant. The overall rate of the series is influenced by these individual decay constants, with the slowest decay often being the rate-limiting step in the entire process.
23. What is the Bateman equation and how is it used in series disintegration?
The Bateman equation is a mathematical model that describes the abundance of nuclei in a decay chain over time. It takes into account the decay constants of all nuclei in the series and provides a way to calculate the amount of each isotope at any given time. This equation is crucial for analyzing complex decay chains and predicting the evolution of nuclear abundances.
24. What is the difference between isobaric and isotonic decays in a series?
Isobaric decays occur between nuclei with the same mass number (A) but different atomic numbers (Z). These typically involve beta decay or electron capture. Isotonic decays, on the other hand, occur between nuclei with the same number of neutrons but different numbers of protons. Understanding these distinctions is important for tracking the progression of nuclei through a decay series.
25. What is the role of neutrinos in beta decay processes within a decay series?
Neutrinos play a crucial role in beta decay processes, which are common in decay series. In β- decay, an antineutrino is emitted along with an electron, while in β+ decay, a neutrino is emitted with a positron. Neutrinos carry away energy and angular momentum, ensuring conservation laws are obeyed. Their presence explains the continuous energy spectrum of beta particles.
26. How does the concept of Q-value apply to simultaneous and series disintegration?
The Q-value represents the energy released in a nuclear reaction or decay. In simultaneous disintegration, the Q-value is the total energy released when the parent nucleus splits. In series disintegration, each step has its own Q-value. The sum of these Q-values gives the total energy released in the entire decay chain. Q-values help determine which decay modes are energetically possible.
27. What is the significance of branching fractions in predicting the outcome of a decay series?
Branching fractions indicate the probability of different decay modes for a given nucleus. In a decay series, these fractions determine the relative abundances of different daughter nuclei at each step. By considering branching fractions, scientists can predict the likely paths a decay series will follow and the expected proportions of various end products.
28. How do internal conversion electrons differ from beta particles in a decay series?
Internal conversion electrons are emitted when an excited nucleus transfers energy directly to an orbital electron, ejecting it from the atom. Unlike beta particles, which come from the nucleus itself, internal conversion electrons originate from the electron shells. This process competes with gamma emission in decay series and affects the overall energy distribution of emitted particles.
29. What is the importance of the valley of stability in understanding decay series?
The valley of stability is a region on the chart of nuclides where the most stable isotopes lie. Decay series tend to progress towards this valley. Understanding the valley of stability helps predict the direction of decay: nuclei above the valley (neutron-rich) tend to undergo β- decay, while those below (proton-rich) undergo β+ decay or electron capture. This concept is crucial for mapping out possible decay paths.
30. How does the Geiger-Nuttall law relate to alpha decay in a series?
The Geiger-Nuttall law relates the decay constant (or half-life) of an alpha-emitting nucleus to the energy of the emitted alpha particle. In a decay series involving alpha decays, this law helps predict the relative rates of different alpha decay steps. It shows that nuclei emitting higher-energy alpha particles generally have shorter half-lives.
31. How does the concept of radioactive disequilibrium apply to environmental studies?
Radioactive disequilibrium occurs when the activity ratios of parent and daughter nuclides in a decay series deviate from their equilibrium values. This concept is important in environmental studies, as it can indicate recent changes in the system. For example, disequilibrium in uranium series isotopes can provide information about geological processes or water movement in aquifers.
32. What is the significance of the actinide and lanthanide series in natural decay chains?
The actinide and lanthanide series are groups of elements that include many radioactive isotopes involved in natural decay chains. Actinides, such as uranium and thorium, are particularly important as they form the starting points of natural decay series. Understanding these series is crucial for nuclear physics, geochemistry, and radiometric dating techniques.
33. What is the role of electron capture in decay series, and how does it differ from β+ decay?
Electron capture occurs when a proton-rich nucleus captures an inner-shell electron, converting a proton to a neutron. Unlike β+ decay, which emits a positron, electron capture only emits a neutrino. In decay series, electron capture competes with β+ decay for proton-rich nuclei. It becomes more prevalent for heavier elements where the electron's proximity to the nucleus increases the capture probability.
34. How does the concept of radioactive secular equilibrium apply to dating techniques like radium-lead dating?
Secular equilibrium in the uranium-radium decay series is crucial for radium-lead dating. In this technique, the equilibrium between uranium, radium, and lead isotopes is used to determine the age of samples. When secular equilibrium is established, the decay rate of radium equals that of its uranium parent. Deviations from this equilibrium can indicate recent geological processes or sample disturbance.
35. How do nuclear shell effects influence the stability and decay modes in heavy element decay series?
Nuclear shell effects, based on the nuclear shell model, significantly influence the stability and preferred decay modes of heavy elements. Nuclei with "magic numbers" of protons or neutrons (like 82 protons for lead) show enhanced stability. In decay series of heavy elements, these shell effects can lead to longer-lived isotopes or preferential decay modes, affecting the overall progression of the decay chain.
36. What is the role of spontaneous fission in the decay series of very heavy elements?
Spontaneous fission becomes an increasingly important decay mode for very heavy elements, competing with alpha decay. In decay series of transuranic elements, spontaneous fission can create branching points, leading to a diverse array of fission products. This process is particularly significant for elements beyond uranium and plays a crucial role in the study of superheavy elements.
37. How does the concept of nuclear isomers affect the progression of decay series?
Nuclear isomers are excited states of atomic nuclei with relatively long half-lives. In decay series, the presence of isomers can create additional decay pathways. Some isomers may decay by gamma emission to the ground state, while others might undergo particle emission, leading to different daughter nuclei. This phenomenon adds complexity to decay chains and can affect the overall decay progression.
38. What is the importance of branching decay in the thorium series, and how does it differ from the uranium series?
The thorium decay series, starting with Th-232, exhibits significant branching, particularly at the Ac-228 stage. This branching creates multiple decay paths, leading to different intermediate nuclides before ultimately ending at Pb-208. In contrast, the uranium series (U-238) has less pronounced branching. Understanding these differences is crucial for geochemical studies and dating techniques using these series.
39. How do relativistic effects influence decay processes in very heavy elements?
Relativistic effects become significant for electrons in very heavy elements, affecting their atomic and nuclear properties. These effects can influence electron capture rates and the energetics of decay processes. In decay series of superheavy elements, relativistic effects can alter decay modes and rates, potentially leading to unexpected stability patterns or decay pathways.
40. How does the concept of radioactive equilibrium apply to the production of radioisotopes for medical applications?
Radioactive equilibrium, particularly transient equilibrium, is crucial in the production of medical radioisotopes. For example, in a generator system like Mo-99/Tc-99m, the longer-lived parent (Mo-99) decays to the shorter-lived daughter (Tc-99m) used in medical imaging. Understanding the equilibrium dynamics allows for optimal timing of radioisotope extraction and use in medical procedures.
41. What is the role of cluster decay in heavy element decay series?
Cluster decay is a rare type of radioactive decay where an atomic nucleus emits a small cluster of neutrons and protons (heavier than an alpha particle but lighter than a fission fragment). In heavy element decay series, cluster decay can provide alternative pathways, competing with alpha decay and spontaneous fission. This process is important in understanding the decay mechanisms of very heavy nuclei.
42. How does the concept of effective half-life apply to decay series in biological systems?
Effective half-life combines the physical half-life of a radioisotope with its biological half-life (the time taken for an organism to eliminate half of a substance). In decay series involving biologically active elements

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