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The 163 pages that link to Radioactive decay, each with the reason it gives.

• Radiocarbon datingNarrower topic: Carbon-14 loss follows a predictable statistical decay rate.

• Radiometric datingNarrower topic: Dating relies on predictable decay to convert parent isotopes into measurable daughter products.

• Half-lifeNarrower topic: Half-life measures the rate at which this process removes nuclei from a sample.

• Island of stabilityNarrower topic: The island predicts relative resistance to the decay processes that limit neighboring nuclei.

• Beta decayNarrower topic: Beta decay is one of its principal decay modes.

• Ernest RutherfordNarrower topic: Rutherford measured decay and used its products to identify radioactive transformations.

• GeochronologyNarrower topic: This physical process supplies the clocks used in radiometric dating.

• Uranium–lead datingNarrower topic: Uranium–lead ages rely on predictable nuclear transformations over geological time.

• Gamma rayNarrower topic: Many gamma rays accompany radioactive decay as daughter nuclei shed excess energy.

• PlutoniumNarrower topic: Decay determines plutonium’s isotope-specific heat output, radiation, and persistence.

• Nuclear medicineNarrower topic: Decay determines the emissions used for imaging and the dose delivered over time.

• Electron captureNarrower topic: Electron capture is one mode within this broader class of nuclear transformations.

• RadonNarrower topic: Radon is continually replenished as uranium and thorium decay.

• Carbon-14Narrower topic: Carbon-14 disappears through this general nuclear process.

• Decay chainNarrower topic: Each link in a decay chain is a radioactive transformation.

• RadiopharmaceuticalNarrower topic: Decay type and timing determine the detectable emissions and usable lifetime.

• Rutherford scatteringNarrower topic: Radioactive sources supplied the alpha particles used to probe foil atoms.

• Spontaneous fissionNarrower topic: Spontaneous fission is one possible decay mode among several.

• Potassium-40Narrower topic: Potassium-40 changes into argon-40 or calcium-40 through radioactive decay.

• TennessineNarrower topic: Decay chains from tennessine isotopes provided the main evidence for their production.

• U–Pb datingNarrower topic: U–Pb clocks rely on decay rates that remain stable over geological time.

• BismuthNarrower topic: Bismuth-209’s eventual decay revised the element’s long-standing status as stable.

• Spent nuclear fuelNarrower topic: Decay changes spent fuel’s isotopic inventory and radiation levels over time.

• Uranium–thorium datingNarrower topic: The measured isotope changes follow predictable decay rates.

• Edwin McMillanNarrower topic: Following decay products let researchers infer the identity of short-lived transuranium nuclei.

• FleroviumNarrower topic: Every observed flerovium isotope disappears through nuclear decay.

• Rubidium–strontium datingNarrower topic: The method’s clock is the steady decay of rubidium-87.

• Uranium-series datingNarrower topic: The method turns predictable nuclear decay into an elapsed-time estimate.

• Absolute datingNarrower topic: Radiometric ages rely on decay occurring at a predictable rate.

• ActiniumNarrower topic: Actinium’s radioactivity arises from unstable nuclei transforming into other nuclides.

• Cobalt-60Narrower topic: Cobalt-60's beta and gamma emissions are stages of radioactive decay.

• Irène Joliot-CurieNarrower topic: The induced isotopes were identified through their characteristic decay after irradiation.

• Frédéric Joliot-CurieNarrower topic: The induced isotopes were recognized through their characteristic decay after the bombardment stopped.

• Isotope hydrologyNarrower topic: Radioactive decay provides the clock behind isotope-based water dating.

• PoloniumNarrower topic: Polonium’s radioactivity is a particular instance of this nuclear process.

• Radiogenic heatNarrower topic: Radiogenic heat is the portion of decay energy that becomes thermal energy.

• RadionuclideNarrower topic: Radionuclide decay is a specific instance of this broader nuclear process.

• Rubidium-87Narrower topic: The isotope’s long-term change is an instance of radioactive decay.

• Strontium-90Narrower topic: It is the general process governing strontium-90’s transformation and activity over time.

• Depleted uraniumNarrower topic: Decay chains produce the radiation and decay products relevant to depleted uranium exposure.

• Nuclear chemistryNarrower topic: It describes how unstable nuclei studied in nuclear chemistry change without external intervention.

• Superheavy element researchNarrower topic: Researchers identify many new nuclei through their characteristic sequences of radioactive decays.

• Dirty bombNarrower topic: The source’s decay determines its radiation emissions and how its activity changes over time.

• ProtactiniumNarrower topic: Protactinium's scarcity and isotope diversity are consequences of this broader nuclear process.

• Atomic batteryNarrower topic: It supplies the energy that every atomic battery’s conversion chain begins with.

• BohriumNarrower topic: Bohrium’s radioactive isotopes are identified through their decay chains.

• Decay productNarrower topic: Decay products arise when an unstable parent nucleus transforms.

• Elizabeth RonaNarrower topic: Decay governed the changing quantities and signals in Rona’s radioactive samples.

• K–Ar datingNarrower topic: K–Ar ages rely on the predictable decay rate of potassium-40.

• Radium and Radon in the EnvironmentNarrower topic: Decay produces radium and radon and determines their rates of formation and disappearance.