Nuclear Chemistry and Radiation Review

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Comprehensive vocabulary flashcard set covering nuclear chemistry fundamentals, nuclear decay equations, radiation types, biological radiation effects, radiocarbon dating, medical imaging/therapy, food irradiation, nuclear fission, reactors, waste management, and nuclear fusion.

Last updated 6:20 PM on 9/8/26
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289 Terms

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Atomic Number (ZZ)

The number of protons contained in the nucleus of an atom, which uniquely defines the element.

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Mass Number (AA)

The total sum of protons and neutrons present in the nucleus of an atom.

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Neutrons Calculation Formula

Number of neutrons=Mass number (A)Atomic number (Z)\text{Number of neutrons} = \text{Mass number } (A) - \text{Atomic number } (Z)

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Isotopes

Atoms of the same element that have the same number of protons but a different number of neutrons.

<p>Atoms of the same element that have the same number of protons but a different number of neutrons.</p>
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Stable Isotopes

Isotopes that do not undergo spontaneous decay; there are 264264 known stable isotopes among all elements.

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Naturally Occurring Unstable Isotopes

Isotopes found in nature that spontaneously emit radiation; there are 300300 known naturally occurring unstable isotopes.

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Radioisotope

An unstable radioactive isotope that spontaneously emits energy/radiation to form a more stable nucleus.

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Radioactivity

The nuclear radiation spontaneously emitted by an unstable radioactive isotope.

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Artificial Isotopes

Radioactive isotopes synthesized artificially in laboratory settings by nuclear bombardment.

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Carbon-12 Nuclear Symbol

612C^{12}_6\text{C}, representing an atom with 66 protons and 66 neutrons.

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Carbon-13 Nuclear Symbol

613C^{13}_6\text{C}, representing an atom with 66 protons and 77 neutrons.

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Carbon-14 Nuclear Symbol

614C^{14}_6\text{C}, representing an atom with 66 protons and 88 neutrons.

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Sulfur-30 Symbol Notation

1630S^{30}_{16}\text{S}, indicating 1616 protons and 1414 neutrons.

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Iodine-131 Symbol Notation

53131I^{131}_{53}\text{I}, indicating 5353 protons and 7878 neutrons.

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Alpha Particle (α\alpha)

A high-energy, heavy particle containing 22 protons and 22 neutrons, identical to a helium nucleus.

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Alpha Particle Symbols

α\alpha or 24He^4_2\text{He}, possessing a charge of +2+2 and a mass number of 44.

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Beta Particle (β\beta)

A high-energy electron emitted from a radioactive nucleus when a neutron converts into a proton.

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Beta Particle Symbols

β\beta or 10e^0_{-1}\text{e}, possessing a charge of 1-1 and a negligible mass number of 00.

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Beta Particle Formation Reaction

01n11p+10e^1_0\text{n} \rightarrow ^1_1\text{p} + ^0_{-1}\text{e}, converting a neutron into a proton and an electron.

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Positron (β+\beta^+)

The antiparticle of a beta particle, possessing a charge of +1+1 and a mass equal to an electron.

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Positron Symbols

β+\beta^+ or +10e^0_{+1}\text{e}, possessing a charge of +1+1 and an effective mass number of 00.

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Positron Formation Reaction

11p01n++10e^1_1\text{p} \rightarrow ^1_0\text{n} + ^0_{+1}\text{e}, converting a proton into a neutron and a positron.

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Gamma Ray (γ\gamma)

High-energy electromagnetic radiation released from a radioactive nucleus with no mass and no charge.

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Proton Symbol

11p^1_1\text{p} or 11H^1_1\text{H}, having a charge of +1+1 and a mass number of 11.

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Neutron Symbol

01n^1_0\text{n}, having zero charge and a mass number of 11.

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Alpha Radiation Shielding

Requires paper, clothing, or human skin to block; alpha particles have the greatest mass among emitted particles.

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Beta Radiation Shielding

Requires heavy clothing, lab coats, or gloves to block; beta particles have light mass.

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Gamma Radiation Shielding

Requires dense lead shielding or a thick concrete wall to block due to its extreme high energy.

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Radiation Protection Factors

Reducing exposure time, increasing distance from the radiation source, and using proper shielding.

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Radioactive Decay

The process by which an unstable radioactive nucleus emits radiation, changing into a new nucleus.

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Nuclear Equation Balancing Rules

The sum of mass numbers (AA) and atomic numbers (ZZ) must be equal on both sides of the equation.

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Alpha Emission

Nuclear decay in which an alpha particle (24He^4_2\text{He}) is emitted, reducing mass number by 44 and atomic number by $$2$.

<p>Nuclear decay in which an alpha particle ($$^4_2\text{He}$$) is emitted, reducing mass number by $$4$$ and atomic number by $$2$.</p>
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Uranium-238 Alpha Decay Equation

92238U90234Th+24He^{238}_{92}\text{U} \rightarrow ^{234}_{90}\text{Th} + ^4_2\text{He}

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Americium-241 Alpha Decay Equation

95241Am93237Np+24He^{241}_{95}\text{Am} \rightarrow ^{237}_{93}\text{Np} + ^4_2\text{He}

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Radium-226 Alpha Decay Product

Radon-222 (86222Rn^{222}_{86}\text{Rn}), formed via 88226Ra86222Rn+24He^{226}_{88}\text{Ra} \rightarrow ^{222}_{86}\text{Rn} + ^4_2\text{He}.

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Einsteinium-252 Alpha Decay Product

Berkelium-248 (97248Bk^{248}_{97}\text{Bk}), produced by losing 44 mass units and 22 protons.

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Beta Emission

Nuclear decay emitting a beta particle (10e^0_{-1}\text{e}); 11 neutron is converted to 11 proton, increasing atomic number by 11.

<p>Nuclear decay emitting a beta particle ($$^0_{-1}\text{e}$$); $$1$$ neutron is converted to $$1$$ proton, increasing atomic number by $$1$$.</p>
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Potassium-42 Beta Decay Equation

1942K2042Ca+10e^{42}_{19}\text{K} \rightarrow ^{42}_{20}\text{Ca} + ^0_{-1}\text{e}

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Cobalt-60 Beta Decay Equation

2760Co2860Ni+10e+γ^{60}_{27}\text{Co} \rightarrow ^{60}_{28}\text{Ni} + ^0_{-1}\text{e} + \gamma

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Thorium-234 Beta Decay Product

Protactinium-234 (91234Pa^{234}_{91}\text{Pa}), formed by 90234Th91234Pa+10e^{234}_{90}\text{Th} \rightarrow ^{234}_{91}\text{Pa} + ^0_{-1}\text{e}.

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Tin-126 Beta Decay Result

Antimony-126 (51126Sb^{126}_{51}\text{Sb}), according to 50126Sn51126Sb+10e^{126}_{50}\text{Sn} \rightarrow ^{126}_{51}\text{Sb} + ^0_{-1}\text{e}.

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Zinc-69 Beta Decay Result

Gallium-69 (3169Ga^{69}_{31}\text{Ga}), according to 3069Zn3169Ga+10e^{69}_{30}\text{Zn} \rightarrow ^{69}_{31}\text{Ga} + ^0_{-1}\text{e}.

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Iron-59 Beta Decay Equation

2659Fe2759Co+10e^{59}_{26}\text{Fe} \rightarrow ^{59}_{27}\text{Co} + ^0_{-1}\text{e}

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Positron Emission

Nuclear decay emitting a positron (+10e^0_{+1}\text{e}); 11 proton is lost and 11 neutron is gained, decreasing atomic number by $$1$.

<p>Nuclear decay emitting a positron ($$^0_{+1}\text{e}$$); $$1$$ proton is lost and $$1$$ neutron is gained, decreasing atomic number by $$1$.</p>
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Manganese-49 Positron Decay Equation

2549Mn2449Cr++10e^{49}_{25}\text{Mn} \rightarrow ^{49}_{24}\text{Cr} + ^0_{+1}\text{e}

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Boron-8 Positron Decay Product

Beryllium-8 (48Be^{8}_{4}\text{Be}), formed by 58B48Be++10e^{8}_{5}\text{B} \rightarrow ^{8}_{4}\text{Be} + ^0_{+1}\text{e}.

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Mercury-178 Positron Decay Equation

80178Hg79178Au++10e^{178}_{80}\text{Hg} \rightarrow ^{178}_{79}\text{Au} + ^0_{+1}\text{e}

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Platinum-190 Alpha Decay Equation

78190Pt76186Os+24He^{190}_{78}\text{Pt} \rightarrow ^{186}_{76}\text{Os} + ^4_2\text{He}

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Gamma Emission

Nuclear decay releasing high-energy gamma rays (γ\gamma), causing no change in atomic or mass numbers.

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Metastable Isotope

An unstable isotope (like 4399mTc^{99\text{m}}_{43}\text{Tc}) in a higher-energy state that decays by gamma emission to a more stable state.

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Technetium-99m Gamma Emission Equation

4399mTc4399Tc+γ^{99\text{m}}_{43}\text{Tc} \rightarrow ^{99}_{43}\text{Tc} + \gamma

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Half-Life (t1/2t_{1/2})

The time required for one-half of a sample of a radioactive isotope to undergo nuclear decay.

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Half-Life Independence

The half-life of a radioisotope is a physical property independent of sample size, temperature, and pressure.

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Cobalt-60 Half-Life

5.27years5.27\,\text{years}; emits beta particles and gamma rays used in cancer radiation therapy.

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Carbon-14 Half-Life

5730years5730\,\text{years}; naturally occurring beta emitter used in archaeological radiocarbon dating.

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Potassium-40 Half-Life

1.3×109years1.3 \times 10^9\,\text{years}; naturally occurring radioisotope emitting beta and gamma radiation.

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Radium-226 Half-Life

1600years1600\,\text{years}; naturally occurring alpha emitter.

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Strontium-90 Half-Life

38.1years38.1\,\text{years}; naturally occurring alpha emitter.

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Uranium-238 Half-Life

4.51×109years4.51 \times 10^9\,\text{years} (or 4.5×109y4.5 \times 10^9\,\text{y}); naturally occurring alpha emitter.

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Chromium-51 Half-Life

28days28\,\text{days}; medical gamma emitter.

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Iodine-131 Half-Life

8.05days8.05\,\text{days} (or 8d8\,\text{d}); medical beta and gamma emitter used for thyroid studies.

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Iron-59 Half-Life

44days44\,\text{days}; medical beta and gamma emitter.

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Radon-222 Half-Life

3.8days3.8\,\text{days} (or 3.82days3.82\,\text{days}); naturally occurring gaseous alpha emitter.

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Technetium-99m Half-Life

6.0hours6.0\,\text{hours}; widely used diagnostic medical gamma emitter.

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<p>Phosphorus-32 Half-Life</p>

Phosphorus-32 Half-Life

14days14\,\text{days}; decays by beta emission into Sulfur-32.

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Iodine-131 Decay Mass Calculation (32 days)

A 100.mg100.\,\text{mg} sample of Iodine-131 (t1/2=8.0dayst_{1/2} = 8.0\,\text{days}) decreases to 6.25mg6.25\,\text{mg} after 44 half-lives (32days32\,\text{days}).

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Strontium-90 Decay Calculation (152.4 years)

A 36mg36\,\text{mg} sample of Strontium-90 (t1/2=38.1yearst_{1/2} = 38.1\,\text{years}) decreases to 2.3mg2.3\,\text{mg} after 44 half-lives (152.4years152.4\,\text{years}).

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Iodine-123 Decay Calculation (26 hours)

A 64mg64\,\text{mg} sample of Iodine-123 (t1/2=13ht_{1/2} = 13\,\text{h}) decreases to 16mg16\,\text{mg} after 22 half-lives (26hours26\,\text{hours}).

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Technetium-99m Decay Calculation (24 hours)

A 120.0mg120.0\,\text{mg} sample of Technetium-99m (t1/2=6.0ht_{1/2} = 6.0\,\text{h}) decreases to 7.5mg7.5\,\text{mg} after 44 half-lives (24.0hours24.0\,\text{hours}).

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Decay Half-Life Determination (0.36 g to 90 mg)

Decreasing from 0.36g0.36\,\text{g} (360mg360\,\text{mg}) to 90mg90\,\text{mg} requires 22 half-lives; if elapsed time is 22min22\,\text{min}, the half-life is 11min11\,\text{min}.

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Radiocarbon Dating

A technique using the decay of Carbon-14 (t1/2=5730yearst_{1/2} = 5730\,\text{years}) relative to Carbon-12 to determine the age of organic artifacts.

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Carbon-14 Living Organism Equilibrium

In living organisms, the ratio of radioactive Carbon-14 to stable Carbon-12 remains constant through atmospheric exchange.

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Carbon-14 Decay Post-Mortem

When an organism dies, Carbon-14 intake stops, and existing Carbon-14 continuously decays without being replenished.

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Dead Sea Scrolls Age Calculation

Determined to be 2000years2000\,\text{years} old; calculating 2000years5730years=0.35\frac{2000\,\text{years}}{5730\,\text{years}} = 0.35 half-lives passed.

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Transuranium Elements

Artificial, synthetic elements with atomic numbers greater than 9292 (Z>92Z > 92).

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Synthesis of Elements up to Z = 101

Produced by bombarding target nuclei with light particles such as alpha particles (α\alpha) or neutrons (n\text{n}).

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Synthesis of Elements beyond Z = 101

Requires bombardment of target nuclei with heavier nuclear projectile ions.

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Maximum Synthesized Element Atomic Number

Elements up to atomic number 118118 have been synthesized in laboratory settings.

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Neptunium Synthesis Reaction

92238U+12H92239U+11H^{238}_{92}\text{U} + ^2_1\text{H} \rightarrow ^{239}_{92}\text{U} + ^1_1\text{H}, followed by beta decay of Uranium-239 to Neptunium-239.

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Uranium-239 Half-Life and Decay

t1/2=23.5minutest_{1/2} = 23.5\,\text{minutes}; decays by beta emission to form Neptunium-239 (93239Np^{239}_{93}\text{Np}).

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Neptunium-239 Half-Life and Decay

t1/2=2.33dayst_{1/2} = 2.33\,\text{days}; decays by beta emission to form Plutonium-239 (94239Pu^{239}_{94}\text{Pu}).

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Plutonium-239 Half-Life

t1/2>24,100yearst_{1/2} > 24,100\,\text{years}; a radioactive transuranium element produced from Neptunium decay.

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Transmutation

The nuclear process where a stable nucleus is converted into a radioactive or different nucleus by bombardment with particles.

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Boron-10 Alpha Bombardment Reaction

24He+510B713N+01n^4_2\text{He} + ^{10}_5\text{B} \rightarrow ^{13}_7\text{N} + ^1_0\text{n}, yielding radioactive Nitrogen-13 and a neutron.

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Technetium-98 Neutron Bombardment

Bombarding 4398Tc^{98}_{43}\text{Tc} with a neutron while releasing an alpha particle produces Rhodium-95 (4195Nb^{95}_{41}\text{Nb} or product nucleus).

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Background Radiation

Radiation received during normal daily life from natural and man-made background sources.

<p>Radiation received during normal daily life from natural and man-made background sources.</p>
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Natural Background Radiation Share

Constitutes 82%82\% of total average background radiation exposure in the United States.

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Man-made Background Radiation Share

Constitutes 18%18\% of average exposure, with medical X-rays (11%11\%) and nuclear medicine (4%4\%) as main contributors.

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Potassium-40 Exposure in Humans

0.01%0.01\% of potassium is Potassium-40; a 60kg60\,\text{kg} person has ~20mg20\,\text{mg} of Potassium-40 decaying inside their body.

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Radon Gas Formation

Radon (Rn\text{Rn}) is a radioactive noble gas continuously formed in the earth via the decay of naturally occurring Uranium.

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Radon Background Contribution

Radon accounts for 55%55\% of all background radiation exposure in the United States.

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Radon Decay Chain Hazard

Inhaled Radon-222 decays into non-gaseous alpha-emitting daughter nuclei (Polonium-218, Lead-214) that linger in lungs and damage tissue.

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EPA Indoor Radon Limit

4pCi/L4\,\text{pCi/L} (picoCuries per liter) of air.

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Affected Homes by Radon Contamination

Approximately 8 million8\text{ million} homes in the United States are affected by radon contamination.

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Curie (Ci)

A unit measuring radioactivity equal to 3.7×1010 disintegrations/second3.7 \times 10^{10}\text{ disintegrations/second}.

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Sub-Curie Unit Conversions

1Ci=1,000mCi1\,\text{Ci} = 1,000\,\text{mCi} (millicuries) and 1Ci=1,000,000μCi1\,\text{Ci} = 1,000,000\,\mu\text{Ci} (microcuries).

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Becquerel (Bq)

The SI unit of radioactivity defined as 1 disintegration/second1\text{ disintegration/second} (1Ci=3.7×1010Bq1\,\text{Ci} = 3.7 \times 10^{10}\,\text{Bq}).

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Rad (Radiation Absorbed Dose)

A unit measuring the amount of radiation energy absorbed by one gram of a substance.

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Rem (Radiation Equivalent for Man)

A measure of radiation dose that factors in both absorbed energy and potential tissue damage (1rem1\,\text{rem} produces equal tissue damage regardless of radiation type).

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Average Annual Radiation Dose

The average annual radiation dose absorbed per person is approximately 0.27rem0.27\,\text{rem}.