Ch. 11- Nuclear Chemistry Flashcards
radioactive decay
the disintegration of an unstable atomic nucleus with spontaneous emission of radiation
radioisotopes
atoms or ions with radioactive nuclei
cosmic rays
extremely high-energy radiation from outer space
background radiation
constantly occurring radiation from cosmic rays, and from natural radioactive isotopes in air, water, soil, and rocks
ionizing radiation
radiation that produces ions as it passes through matter; examples= x-rays & nuclear radiation
is our exposure to background radiation harmful?
no, the total amount of background radiation to which the average person is exposed is less than 0.5% of the amount that causes symptoms of radiation sickness
how can high levels of ionizing radiation be harmful?
- damages live tissue (white blood cells are most vulnerable)
- affects bone marrow, causing less red blood cells to be reduced, resulting in anemia
- induces leukemia
- causes mutations in DNA
alpha decay
emission of an alpha particle by a radioactive nucleus
beta decay
emission of a beta particle by a radioactive nucleus
why is beta decay complicated?
in beta decay, a neutron within the nucleus is converted into a proton (which remains in the nucleus) and an electron (which is ejected)
gamma decay
emission of a gamma ray by a radioactive nucleus
biggest difference between gamma decay & alpha/beta decay
different from alpha & beta decay because gamma radiation has no charge and no mass; A (nucleon #) & Z (atomic #) of emitting atom is changed
positron
a positively charged particle with the mass of an electron
positron emission
a type of radioactive decay that can be envisioned by the change of a proton in the nucleus into a neutron & a positron, with the positron being emitted from the nucleus
what is it about positron emission & electron capture that differentiates them from the 3 common types of radioactive decay (alpha/beta/gamma)?
they both result in a decrease of 1 in atomic number, but with no change in nucleon number
what happens after positron emission?
the original nucleus has 1 fewer proton & 1 more neutron than it had before, and the emitted positron quickly encounters an electron where both particles are then annihilated & turned into energy (specifically, 2 gamma rays)
electron capture (EC)
a type of radioactive decay in which a nucleus absorbs an electron from the first or second shell of the atom, causing the electron to combine with a proton to form a neutron
what happens after EC?
eventually an electron from a higher shell drops to the level vacated by the captured electron, which releases an x-ray
half-life
the length of time required for one-half of the radioactive nuclei in a sample to decay
half-life
the length of time required for one-half of the radioactive nuclei in a sample to decay
becquerel (Bq)
a measure of the rate of radioactive decay (isotope’s activity); 1 Bq = 1 disintegration per second
becquerel (Bq)
a measure of the rate of radioactive decay (isotope’s activity); 1 Bq = 1 disintegration per second
carbon-14 dating
a radioisotopic technique for determining the age of artifacts, based on the half-life of carbon-14
carbon-14 dating
a radioisotopic technique for determining the age of artifacts, based on the half-life of carbon-14
which carbon isotopes do we have on Earth & how much of each?
carbon-12 (99%) & carbon-13 (1%)
explain the process in which carbon-14 is formed & concentrated in Earth’s atmosphere & living things
nitrogen is abundant in Earth’s upper atmosphere & cosmic rays are constantly raining down on Earth
- cosmic rays collide with particles in Earth’s atmosphere, emitting high energy neutrons
- emitted neutrons collide with nitrogen atoms, which emits a proton, resulting in formation of carbon-14
- carbon-14 becomes concentrated in CO2 in Earth’s upper atmosphere
- CO2 is then introduced to living things via photosynthesis
what is the half-life of carbon-14?
5730 years
how old must an object be for carbon-14 dating to be accurate?
100-50,000 years old
transmutation
the conversion of one element into another
tracers
radioisotopes used to trace the movement of substances or locate the sites of activity in physical, chemical, and biological systems