Nuclear Radiation Natural Radioactivity Nuclear Equations

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Presentation transcript:

Nuclear Radiation Natural Radioactivity Nuclear Equations Producing Radioactive Isotopes Half-Life Nuclear Fission and Fusion

Subatomic Particles Protons- plus charge In the nucleus Neutrons- neutral Electrons - negative charge Outside the nucleus

Nuclear Symbols Mass number (p+ + no) Element symbol Atomic number (number of p+)

RADIOACTIVITY Nuclei of unstable isotopes called radioisotopes gain stability by undergoing changes These changes are always accompanied by large amounts of energy Discovery of radioactivity dealt a blow to Dalton’s theory that atoms are indivisible

Radiation Radiation comes from the nucleus of an atom. Unstable nucleus emits a particle or energy  alpha  beta  gamma

Same as a helium nucleus Alpha Particle Same as a helium nucleus (He) 4 2 He or  Two protons Two neutrons

Beta Particle  e or  1 An electron emitted from the nucleus e or  1 A neutron in the nucleus breaks down 1 1 0 n H + e 0 1 -1

Gamma  Radiation Pure radiation Like an X-ray but comes from the nucleus

Radiation Protection Shielding alpha – paper, clothing beta – lab coat, gloves gamma- lead, thick concrete Limit time exposed Keep distance from source

Radiation Protection

Balancing Nuclear Equations In the reactants and products Atomic numbers must balance and Mass numbers must balance

Alpha decay

Beta decay 234Th ® 234Pa + 0e 90 91 1 beta particle

No change in atomic or mass number Gamma radiation No change in atomic or mass number 11B 11B + 0  5 5 0 boron atom in a high-energy state

Types of Radioactive Decay gamma ray production (g): positron production : electron capture: (inner-orbital electron is captured by the nucleus) e 1

Types of Radiation

Learning Check NR1 Write the nuclear equation for the beta emitter Co-60.

Solution NR1 Write the nuclear equation for the Beta emitter Co-60. 60Co 60Ni + 0 e 27 28 -1

Half-Life of a Radioisotope The time for the radiation level to fall (decay) to one-half its initial value decay curve 8 mg 4 mg 2 mg 1 mg initial 1 half-life 2 3

Examples of Half-Life Isotope Half life C-15 2.4 sec Ra-224 3.6 days I-125 60 days C-14 5700 years U-235 710 000 000 years

Learning Check NR3 The half life of I-123 is 13 hr. How much of a 64 mg sample of I-123 is left after 26 hours?

Solution NR3 t1/2 = 13 hrs 26 hours = 2 x t1/2 Amount initial = 64mg Amount remaining = 64 mg x ½ x ½ = 16 mg

Nuclear Fission Fission large nuclei break up 235U + 1n 139Ba + 94Kr + 3 1n + 92 0 56 36 0 Energy

Fission

Nuclear Fusion Fusion small nuclei combine 2H + 3H 4He + 1n + 1 1 2 0 1 1 2 0 Occurs in the sun and other stars Energy

Learning Check NR4 Indicate if each of the following are Fission (2) fusion Nucleus splits Large amounts of energy released Small nuclei form larger nuclei Hydrogen nuclei react Energy

Solution NR4 Indicate if each of the following are Fission (2) fusion 1 Nucleus splits 1 + 2 Large amounts of energy released 2 Small nuclei form larger nuclei 2 Hydrogen nuclei react

Energy and Mass Nuclear changes occur with small but measurable losses of mass. The lost mass is called the mass defect, and is converted to energy according to Einstein’s equation: DE = Dmc2 Dm = mass defect DE = change in energy c = speed of light Because c2 is so large, even small amounts of mass are converted to enormous amount of energy.