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  • Radioactive Decay: Understanding the Path to Atomic Stability
    The elements that continue to decay until they finally become stable are called radioactive isotopes.

    Here's a breakdown:

    * Isotopes: Atoms of the same element with the same number of protons but different numbers of neutrons.

    * Radioactive isotopes: Isotopes with unstable nuclei. The instability is due to an imbalance in the ratio of protons to neutrons.

    * Decay: Radioactive isotopes release energy and particles to transform into a more stable state. This process is called radioactive decay.

    Examples of radioactive isotopes and their decay products:

    * Uranium-238 decays through a series of steps to eventually become lead-206.

    * Carbon-14 decays into nitrogen-14.

    * Iodine-131 decays into xenon-131.

    Key points about radioactive decay:

    * Half-life: The time it takes for half of the radioactive atoms in a sample to decay. Each radioactive isotope has its own specific half-life.

    * Types of decay: There are several types of radioactive decay, including alpha decay, beta decay, and gamma decay. Each type involves the emission of different particles and energy.

    * Applications: Radioactive isotopes have many applications in medicine, industry, and research, such as medical imaging, dating fossils, and tracing chemical reactions.

    Note: Not all isotopes are radioactive. Some isotopes are stable and do not decay.

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