What is radioactivity and half-life? | Nuclear Physics | Visual Explanation

Dr. Paulien Moyaert
9 Jun 202204:42

Summary

TLDRIn this educational video, Pauline, a Belgian nuclear medicine resident, delves into the concepts of radioactivity, radioactive decay, and half-life. She explains how an imbalance in protons and neutrons leads to instability and decay, emitting radiation. The half-life, the time for half of a radioactive substance to decay, is highlighted with the example of Iodine-131, used in treating hyperthyroidism, and Carbon-14 in carbon dating. The video concludes with the significance of half-life in understanding radioactive decay rates.

Takeaways

  • 🧬 The balance of protons and neutrons in an atomic nucleus determines its stability.
  • 📊 Elements with fewer protons, like those near the top of the periodic table, are stable if they have an equal number of protons and neutrons, such as carbon-12.
  • 🔬 As the number of protons increases, more neutrons are needed for stability, as seen in lead-207 with 82 protons and 125 neutrons.
  • ☢️ Unstable nuclei, with too many protons or too few neutrons, undergo radioactive decay, emitting radiation.
  • 📡 Radioactive decay is a spontaneous and random process, making it impossible to predict which nucleus will decay next, but statisticians can determine when half will have decayed.
  • ⏳ The half-life of a radioactive material is the time required for its activity to reduce to half of its initial value.
  • 🌡 Iodine-131 is a radioactive isotope used to treat hyperthyroidism and has a half-life of approximately eight days, undergoing beta decay to become xenon-131.
  • 📉 After each half-life period, the amount of radioactive iodine decreases by half, while the remaining decays into xenon.
  • 🔍 The concept of half-life can be applied whether measuring in atoms or grams, with the same decay principle.
  • 🗓️ Archaeologists use half-life in carbon dating to determine the age of organic objects, as carbon-14 decays into nitrogen-14.
  • 🔚 Radioactive decay continues indefinitely, though the amount of a radioactive substance may become very small, it never completely disappears.

Q & A

  • What is the main topic of the video?

    -The main topic of the video is to explain the concepts of radioactivity, radioactive decay, and half-life, and to provide an example of how half-life is used in everyday life.

  • What determines the stability of a nucleus?

    -The balance of protons and neutrons in a nucleus determines whether it will be stable or unstable. Too many neutrons or protons can upset this balance, making the nucleus unstable.

  • Why are elements with fewer protons generally stable?

    -Elements with fewer protons, such as those near the top of the periodic table, are stable if they have the same number of neutrons and protons, as seen in carbon-12, which has 6 protons and 6 neutrons.

  • What happens when a nucleus has too many protons or too few neutrons?

    -Unstable nuclei with too many protons or too few neutrons will disintegrate or decay by emitting radiation, a process known as radioactive decay.

  • What is radioactivity?

    -Radioactivity is the amount of radiation released by a material that can undergo radioactive decay.

  • How is radioactive decay described in the video?

    -Radioactive decay is described as a spontaneous and random process where it is not possible to predict which particular nucleus will decay next, but a certain number will decay in a given time.

  • What is half-life and how is it related to radioactive decay?

    -Half-life is the time it takes for half of the unstable nuclei in a radioactive material to decay, which is a measure of the rate of radioactive decay.

  • Can you provide an example of a radioactive isotope mentioned in the video?

    -Iodine-131 is an example of a radioactive isotope mentioned in the video, which undergoes beta decay to become stable xenon-131.

  • What is the half-life of iodine-131 and how is it used?

    -The half-life of iodine-131 is approximately eight days, and it is commonly used to treat hyperthyroidism.

  • How does the concept of half-life apply to dating organic objects?

    -Archaeologists use half-life in a process known as carbon dating to determine the age of organic objects, by measuring the amount of carbon-14 remaining in the object.

  • What happens to the amount of a radioactive substance over time?

    -The amount of a radioactive substance decreases over time as it decays, but it never drops to zero completely, even though the amount might become very small.

Outlines

00:00

🔬 Radioactivity and Nuclear Stability

Pauline, a Belgian nuclear medicine resident, introduces the concept of radioactivity, radioactive decay, and half-life. She explains that the balance of protons and neutrons in an atomic nucleus determines its stability, with too many or too few leading to instability and decay. Elements with fewer protons, like those near the top of the periodic table, are generally stable if they have an equal number of neutrons and protons, as exemplified by carbon-12. However, as the number of protons increases, more neutrons are required for stability, as seen in lead-207. Unstable nuclei undergo radioactive decay, emitting radiation, and are considered radioactive. The amount of radiation emitted is referred to as radioactivity.

⏱ Understanding Radioactive Decay and Half-Life

The script delves into radioactive decay as a spontaneous and random process, where it's impossible to predict which specific nucleus will decay next. However, statistically, scientists can determine when half of the unstable nuclei will have decayed, defining this time span as the half-life. The half-life is the period required for the activity of a radioactive source to reduce to half its initial value. An example using iodine-131 illustrates how half-life works, showing that after eight days, half of the iodine atoms decay into xenon, and the process continues in a predictable manner regardless of the sample size, be it measured in atoms or grams.

🌿 Practical Applications of Half-Life: Carbon Dating

The video concludes with a practical application of half-life in archaeology, specifically in carbon dating to determine the age of organic objects. It explains that when organisms die, they stop producing carbon-14, and through beta decay, carbon-14 turns into nitrogen-14. Knowing the half-life of carbon-14, scientists can calculate the time elapsed since the organism's death. The summary emphasizes the importance of half-life in understanding nuclear instability and its predictable decay rate, which is crucial in various scientific fields.

Mindmap

Keywords

💡Radioactivity

Radioactivity refers to the property of certain materials to spontaneously emit radiation as a result of their unstable atomic nuclei. In the video, it is the fundamental concept that leads to the discussion of radioactive decay and half-life, illustrating how unstable nuclei release radiation, making the material radioactive.

💡Radioactive Decay

Radioactive decay is the process by which an unstable atomic nucleus loses energy by emitting radiation. The video explains that this decay is spontaneous and random, and it's the mechanism by which materials like iodine-131 transform into other elements, such as xenon-131, through beta decay.

💡Half-Life

Half-life is the time required for half of the radioactive nuclei in a sample to decay. The video uses the concept of half-life to demonstrate how the activity of a radioactive source decreases over time, using iodine-131 as an example where its half-life is approximately eight days.

💡Nucleus

The nucleus of an atom consists of protons and neutrons at its center. The stability of the nucleus is determined by the balance between the number of protons and neutrons it contains. The video mentions that an imbalance can lead to instability and subsequent radioactive decay.

💡Protons

Protons are subatomic particles with a positive electric charge found in the nucleus of an atom. The video explains that the number of protons in an element determines its identity on the periodic table and influences the stability of the nucleus, requiring a corresponding number of neutrons for stability.

💡Neutrons

Neutrons are subatomic particles with no electric charge that are also located in the nucleus of an atom. The video script indicates that the number of neutrons needed for a stable nucleus increases with the number of protons, and an imbalance can result in instability and radioactive decay.

💡Iodine-131

Iodine-131 is a radioactive isotope of iodine mentioned in the video that has a half-life of approximately eight days. It undergoes beta decay to become stable xenon-131 and is used in medical treatments for hyperthyroidism, illustrating the practical application of half-life in everyday life.

💡Beta Decay

Beta decay is a type of radioactive decay in which a neutron in an unstable nucleus is transformed into a proton, releasing an electron in the process. The video uses iodine-131 as an example of an isotope that undergoes beta decay to form xenon-131.

💡Xenon-131

Xenon-131 is a stable isotope formed as a result of the beta decay of iodine-131. The video script uses this transformation to explain the concept of radioactive decay and the practical measurement of half-life in a sample.

💡Carbon Dating

Carbon dating is a method used by archaeologists to determine the age of organic objects based on the half-life of carbon-14. The video explains that during beta decay, carbon-14 turns into nitrogen-14, and by knowing the half-life of carbon-14, scientists can estimate when an organism died.

💡Carbon-14

Carbon-14 is a radioactive isotope of carbon used in carbon dating. The video script explains that when an organism dies, it stops incorporating carbon-14, and by measuring the remaining amount of carbon-14, scientists can estimate the time elapsed since the organism's death.

Highlights

Pauline introduces herself as a Belgian nuclear medicine resident.

The video aims to explain radioactivity, radioactive decay, and half-life.

Nucleus stability is determined by the balance of protons and neutrons.

Unstable nuclei with too many protons or too few neutrons undergo radioactive decay.

Radioactive decay is a spontaneous and random process.

Statistical methods are used to determine the half-life of a radioactive material.

Half-life is defined as the time for half of the unstable nuclei to decay.

Iodine-131 is used to treat hyperthyroidism and has a half-life of approximately eight days.

An example of iodine-131 decay shows how half-life affects the quantity of radioactive material over time.

The concept of half-life applies whether measuring in atoms or grams of radioactive material.

Archaeologists use half-life in carbon dating to determine the age of organic objects.

Carbon-14 undergoes beta decay to become nitrogen-14, which is key in carbon dating.

The half-life of carbon-14 is used to calculate the time since an organism's death.

Unstable nuclei will eventually decay at a predictable rate referred to as half-life.

The video concludes with a summary of the importance of half-life in understanding radioactive decay.

A call to action for viewers to like the video if they enjoyed it.

Transcripts

play00:00

[Music]

play00:08

hi everyone my name is pauline i am a

play00:10

belgian nuclear medicine resident and in

play00:12

this video i will explain to you what

play00:14

radioactivity radioactive decay and

play00:17

half-life is

play00:19

and at the end of the video i will give

play00:21

you an example of how half-life can be

play00:23

used in everyday life

play00:28

the balance of protons and neutrons in a

play00:31

nucleus determines whether a nucleus

play00:33

will be stable or unstable

play00:36

too many neutrons or protons can upset

play00:39

this balance making the nucleus unstable

play00:43

elements with fewer protons such as the

play00:45

ones near the top of the periodic table

play00:48

are stable if they have the same number

play00:50

of neutrons and protons

play00:52

for example carbon carbon 12 is stable

play00:55

and has 6 protons and 6 neutrons

play01:00

however as the number of protons

play01:02

increases more neutrons are needed to

play01:05

keep the nucleus stable

play01:07

for example lead 207 has 82 protons and

play01:11

125 neutrons

play01:17

unstable nuclei so nuclei with too many

play01:19

protons or too few neutrons will

play01:22

disintegrate or decay by emitting

play01:24

radiation

play01:25

this is called radioactive decay

play01:28

a material that can undergo radioactive

play01:30

decay is considered to be radioactive

play01:33

and the amount of radiation released by

play01:35

the material is its radioactivity

play01:40

radioactive decay is a spontaneous and

play01:42

random process

play01:44

it means that it is not possible to say

play01:46

which particular nucleus from a block of

play01:48

radioactive material will decay next but

play01:51

given that there are so many of them it

play01:54

is possible to say that a certain number

play01:56

will decay in a certain sign

play02:00

scientists can use statistical methods

play02:02

to tell when half of the unstable nuclei

play02:05

will have decayed

play02:06

this is called the half-life

play02:09

half-life is the time it takes for the

play02:11

activity of the source to fall to half

play02:13

its original value

play02:17

here's an example of how a radioactive

play02:19

sample is decaying over time

play02:21

iodine 131 is a radioactive isotope of

play02:25

iodine that is commonly used to treat

play02:27

hyperthyroidism

play02:29

iodine 131 undergoes beta decay to

play02:33

become stable xenon 131

play02:36

the half-life of this reaction is

play02:38

approximately eight days

play02:41

this means that if we have a sample of

play02:43

eight iodine atoms after eight days half

play02:46

of the atoms will have decayed to form

play02:49

xenon and half of the atoms will still

play02:51

be radioactive iodine

play02:54

after an additional eight days half of

play02:56

the still radioactive iodine atoms will

play02:59

decay leaving two atoms of iodine

play03:04

this same idea would apply if we

play03:05

measured our sample in grams instead of

play03:08

atoms

play03:09

if we started with 40 grams of iodine

play03:12

after one half life or eight days 20

play03:15

grams would have decayed into xenon and

play03:17

20 grams would still be radioactive

play03:20

after an additional half-life 10 grams

play03:23

of the original sample would still be

play03:25

iodine while the remaining 30 grams

play03:27

would have decayed into xenon

play03:30

note that this process continues and

play03:32

although the amount of iodine might get

play03:35

very small it does not drop to zero

play03:37

completely

play03:40

archaeologists use half-life to date the

play03:42

age of organic objects in a process

play03:45

known as carbon dating

play03:47

during beta decay carbon 14 becomes

play03:50

nitrogen 14. at the time of that

play03:53

organisms stop producing carbon 14.

play03:57

scientists know the half-life of carbon

play03:59

so they can figure out how long ago the

play04:01

organism died

play04:04

here's a quick summary

play04:06

if there are too many or too few

play04:07

neutrons for a given number of protons

play04:10

the resulting nucleus will be unstable

play04:12

and will undergo radioactive decay

play04:15

this decay occurs at a constant

play04:17

predictable rate that is referred to as

play04:19

half-life

play04:22

the half-life is the amount of time it

play04:23

takes for a given radioisotope to lose

play04:26

half of its radioactivity

play04:30

[Music]

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thank you so much for watching this

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video

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if you liked it please give it a thumbs

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up

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الوسوم ذات الصلة
RadioactivityNuclear MedicineHalf-LifeUnstable NucleiRadioactive DecayIodine-131Xenon-131Carbon DatingBeta DecayScience EducationMedical Treatment
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