Problem 7
Question
If the half-life of a radioisotope is 20,000 years, then a sample in which three-quarters of that radioisotope has decayed is _______ years old. a. 15,000 b. 26,667 \(c .30,000\) d. 40,000
Step-by-Step Solution
Verified Answer
d. 40,000 years
1Step 1: Understand the definition of half-life
A half-life is the time required for a quantity to reduce to half its initial value. For a radioisotope, it is the time taken for half of the radioactive atoms to decay.
2Step 2: Calculate the number of half-lives for three-quarters decay
If three-quarters of the radioisotope has decayed, it means one-quarter of the original amount remains. This is equivalent to saying that the original quantity has halved once (leaving one-half), and then halved again (from one-half to one-quarter). Thus, the number of half-lives that have passed is 2.
3Step 3: Calculate the sample age
Each half-life for this radioisotope is 20,000 years. Since 2 half-lives have passed, the age of the sample is \(2 \times 20,000 = 40,000\) years.
Key Concepts
Radioisotope DecayRadioactive Decay CalculationNuclear Physics Concepts
Radioisotope Decay
Radioisotopes are atoms with unstable nuclei that lose their excess energy through a process known as decay. Over time, these atoms transform into different elements or isotopes that are stable. This behavior is central to understanding radioisotope behavior and its applications in fields like medical diagnostics and environmental dating, such as carbon dating.
Radioactive decay is a random process at the level of single atoms, meaning it's impossible to predict when a particular atom will decay. However, on a statistical level we can predict the decay of a large number of atoms, which is expressed in terms of half-life. The half-life of a radioisotope is the time it takes for half of the radioactive atoms in a sample to decay. This concept helps us to gauge the age or growth of materials over large periods of time.
Radioactive decay is a random process at the level of single atoms, meaning it's impossible to predict when a particular atom will decay. However, on a statistical level we can predict the decay of a large number of atoms, which is expressed in terms of half-life. The half-life of a radioisotope is the time it takes for half of the radioactive atoms in a sample to decay. This concept helps us to gauge the age or growth of materials over large periods of time.
- Radioisotopes transform into more stable forms over time.
- The process is predictable statistically, based on the concept of half-life.
- This principle is useful in various scientific and industrial applications.
Radioactive Decay Calculation
Calculating radioactive decay involves using the half-life information to determine how long a process has been occurring. For instance, if you know a material's half-life, you can determine how long it has been decaying based on how much remains.
In the given exercise, three-quarters of a radioisotope has decayed, which implies one-quarter remains intact. To determine the age, we must understand how many half-lives it takes to reach one-quarter of the original amount.
In the given exercise, three-quarters of a radioisotope has decayed, which implies one-quarter remains intact. To determine the age, we must understand how many half-lives it takes to reach one-quarter of the original amount.
- Each half-life decreases the remaining quantity by half.
- From full to one-half is one half-life, and from one-half to one-quarter is another.
- Thus, two half-lives mean the sample has been around for twice the half-life duration.
Nuclear Physics Concepts
Nuclear physics helps to explain the behavior of radioactive materials. It encompasses principles such as nuclear decay, half-life, and atomic transformations. At its core, nuclear physics explores how unstable atoms release energy to become stable. By studying this, we can better understand phenomena within various scientific disciplines.
The nucleus of an atom holds protons and neutrons together with significant forces. However, when it comes to radioisotopes, these nuclei can become unstable due to an imbalance of these internal components. To reach stability, energy is released in the form of radiation, a process known as decay.
The nucleus of an atom holds protons and neutrons together with significant forces. However, when it comes to radioisotopes, these nuclei can become unstable due to an imbalance of these internal components. To reach stability, energy is released in the form of radiation, a process known as decay.
- Nuclear decay: Process of releasing energy to stabilize an atom.
- Half-life: Time needed for half of a radioactive sample to decay.
- Applications: Used widely in medicine, archaeology, and more.
Other exercises in this chapter
Problem 5
In which type of rock are you more likely to find a fossil? a. basalt, a dark, fine-grained volcanic rock b. limestone, composed of sedimented calcium carbonate
View solution Problem 6
Which of the following is a fossil? a. an insect encased in 10 -million-year-old tree sap b. a woolly mammoth frozen in Arctic permafrost for the last 50,000 ye
View solution Problem 8
Did Pangea or Gondwana form first?
View solution Problem 11
Homologous structures among major groups of organisms may differ in _______ a. size b. shape c. function d. all of the above
View solution