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This middle school science passage introduces students to the concept of radioactive decay, aligning with NGSS standard MS-PS1-3. It explains how unstable atomic nuclei release radiation to become more stable, the role of parent and daughter isotopes, and how decay chains result in one element transforming into another. The passage uses real-life examples like uranium decaying to lead and carbon-14 decaying to nitrogen-14, and discusses applications in archaeology and environmental science. Academic vocabulary is embedded and supported by a glossary. The resource includes a Spanish translation, a simplified differentiated version for accessibility, a multiple-choice quiz, and graphic organizers. All resources are audio integrated, supporting diverse learners and building foundational knowledge about atomic structure and nuclear processes.
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Radioactive Decay
Radioactive decay is a natural process that changes the identity of elements over time. It is responsible for the way uranium in rocks can eventually turn into lead, and for how scientists use carbon-14 to date ancient bones and artifacts. Understanding radioactive decay helps explain the age of the Earth, the origin of some elements, and even how smoke detectors work. This passage explores how and why radioactive decay happens, and why it is important for science and society.
The Mechanism of Radioactive Decay Atoms are made of protons and neutrons in a central nucleus, surrounded by electrons. Some nuclei are unstable because they have too many or too few neutrons compared to protons. These unstable nuclei are called radioisotopes or radioactive isotopes. To reach a more stable state, they release radiation—energy or particles that escape from the nucleus. During this process, the parent isotope changes into a different element called the daughter isotope. For example, a uranium-238 nucleus (the parent) emits particles and becomes lead-206 (the daughter) after a series of decays. This series is known as a decay chain. Each step in the chain involves the nucleus losing particles or energy, gradually transforming into a more stable element.
Decay Chains and Predictable Patterns While the decay of a single atom is random, scientists can predict how a large group of atoms will behave. The half-life of a radioisotope is the time it takes for half of the atoms in a sample to decay. For uranium-238, the half-life is about 4.5 billion years. This means that after 4.5 billion years, only half of the original uranium remains, and the rest has become other elements through decay. Carbon-14, which is used to date ancient organic materials, decays into nitrogen-14 with a half-life of 5,730 years. By measuring the ratio of parent to daughter isotopes, scientists can calculate the age of rocks, fossils, and artifacts with remarkable accuracy. Decay chains can involve several steps and different elements before reaching a stable isotope.
Applications and Broader Implications Radioactive decay has many uses beyond dating ancient objects. In medicine, radioisotopes are used to diagnose and treat diseases. Environmental scientists use the decay of certain isotopes to track pollution and study climate change. The energy released during radioactive decay can be harnessed in nuclear power plants to generate electricity. However, the radiation produced can also be harmful, so safe handling and disposal of radioactive materials is important for health and the environment. The study of radioactive decay connects to larger scientific principles, like the conservation of mass and energy, and helps us understand the dynamic and ever-changing nature of matter in the universe.
Interesting Fact: A single gram of radium releases about 0.0001 calories of energy per second through radioactive decay—enough to glow in the dark!
What is radioactive decay?
A process where unstable nuclei release radiation to become more stable.A way atoms form molecules.The process by which atoms gain electrons.A method for making electricity from water.
Which part of the atom is involved in radioactive decay?
NucleusElectronsProtons onlyNeutrons only
What is a parent isotope?
The original, unstable atom before decayThe new atom formed after decayAn atom that never decaysA molecule that contains two atoms
What does the term 'half-life' mean in the passage?
The time it takes for half of a group of radioactive atoms to decayThe time for an atom to become an electronThe time it takes for a rock to formThe period when atoms stop moving
Which of these is an example of a decay chain described in the passage?
Uranium-238 changing to lead-206 through several stepsWater evaporating from a lakeIron rusting in the airOxygen forming during photosynthesis
What is the main reason scientists use the ratio of parent to daughter isotopes?
To calculate the age of rocks, fossils, or artifactsTo make electricity from waterTo measure the temperature of the EarthTo count the number of electrons
In what way is radioactive decay useful in medicine?
It helps diagnose and treat diseasesIt makes water boil fasterIt prevents plants from growingIt turns lead into gold
What is the role of radiation in radioactive decay?
Radiation is energy or particles released as unstable atoms become stableRadiation is the process of atoms gaining electronsRadiation creates new elements directlyRadiation is used only in power plants
True or False: The half-life of carbon-14 is 5,730 years.
TrueFalse
True or False: The decay of a single atom is predictable and always happens at the same time.
TrueFalse
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