chapter 11 radioactiv e elements. accidental discovery of nuclear radiation in 1896, french...
TRANSCRIPT
Chapter 11
Radioactive
Elements
Accidental Discovery of Nuclear Radiation
• In 1896, French scientist Henri Becquerel accidentally left some uranium samples on a photographic plate & found outlines of the substance on the film
• at first, he thought the uranium was giving off X-rays because the photographic paper had been exposed to sunlight
• but when it worked without the sun, he hypothesized that the uranium had given off some invisible energy that had never been detected before, later called radiation
Background Info•it was known that certain substances glowed when exposed to sunlight (fluorescent)
•but his experiment worked even when it wasn’t sunny
•he determined that the element uranium was the source of nuclear radiation
Other Discoveries of
Nuclear Radiation•Later, in 1898, Marie Curie & her husband, Pierre, discovered two other radioactive elements they named polonium & radium
An element that gives off nuclear radiation is said to
be radioactive.Properties include:1.nuclear radiation from radioactive
elements will alter photographic film
2.they produce fluorescence3.electric charge can be found in the
air surrounding radioactive elements
4.nuclear radiation damages cells in most organisms
Fluorescence
The Nucleus• contains protons & neutrons held
together by strong forces• strong forces are short-range forces
that only work over a very short distance; therefore, the bigger the nucleus, the farther apart the protons & neutrons
• as long as the protons & neutrons remain together due to the strong force, the nucleus remains stable
• the bigger the nucleus, the more unstable it becomes
Radioactivity•when the strong force is not large enough to hold the nucleus together tightly, the nucleus can decay & give off matter & energy
•this process where the nucleus breaks apart or decays is called radioactivity
•all elements with 83 or more protons are radioactive
Binding Energy
•the energy required to break up the nucleus
•if the binding energy within the nucleus is weak, the nucleus is unstable & will break apart or decay
Unstable•synthetic elements are unstable & decay quickly after being created in the laboratory
•many isotopes of elements (no matter the nucleus size) are also radioactive
•they are sometimes called radioisotopes
Isotopes
•an atom of an element that has the same number of protons, but a different number of neutrons
•many elements can have both radioactive & nonradioactive isotopes (see pg. 271 for examples)
3 Types of Nuclear Radiation
•alpha radiation (particles)
•beta radiation (particles)
•gamma radiation (waves of energy)
3 Types of Radiation
Alpha Particles•made of 2 protons + 2 neutrons•has an electric charge of +2•had an atomic mass of 4•more massive & most electric charge• lose energy more quickly when
interacting with matter• least penetrating (cannot pass
through a piece of paper)•very damaging to biological
molecules within the body
Alpha Decay•when an atom loses an alpha
particle, it is no longer the same element because the number of protons is different
• the new element formed has an atomic number two less than the original radioactive element, and a mass number that is four less (it lost two neutrons too)
Transmutation
•the process of changing one element to another through nuclear decay
•the atomic mass at the beginning of the equation must equal the atomic mass at the end
How Smoke Detectors Work
•when alpha radiation passes through matter, they exert an electrical force on the electrons
• this force pulls the electrons away fro the atoms, giving the atom a positive charge (cation)
How Smoke Detectors Work•some smoke detectors will give off
alpha particles to ionized the surrounding air
•normally, an electrical current can pass through the ionized air to form a circuit
•when smoke particles enter the ionized air, they absorbs the ions & electrons, thus breaking the circuit causing the alarm to go off
Beta Particles•move much faster than alpha
particles & are more penetrating• these particles are stopped by Al
foil•when a neutron in an unstable
nucleus decays into a proton, it emits an electron called the beta particle
•process is known as beta decay•caused by weak forces
Beta Decay/Transmutation
•now that an extra proton was produced in the beta decay, the atom changes to another element
•although the atom of this new element has a different atomic number, it still has the same atomic mass because the atom lost a neutron & gained a proton
Beta Decay
Gamma Rays•most penetrating form of radiation•not made of protons, electrons, or
neutrons•carry electromagnetic waves of
energy•have no mass, no charge•move at the speed of light•stopped by thick, dense materials
such as lead or concrete
Gamma Decay•alpha & beta decay are
accompanied by gamma decay, the release of a gamma ray from the nucleus
•since there is no mass or charge, the nucleus does not change into a different nucleus
•since energy leaves, the nucleus moves to a lower energy state
Electromagnetic Spectrum
Decay Series•the series of steps by which a radioactive nucleus decays into a nonradioactive nucleus
•spontaneous breakdown continues until a stable nucleus is formed
Artificial Transmutation
•bombard atomic nuclei with neutrons, alpha particles, or other nuclear “bullets”
•done in particle accelerators because of the need to hit the target nuclei with enough force with these high-energy particles
Particle Accelerator
Artificial Transmutation
• first done by Ernest Rutherford who discovered the nucleus of the atom
• Italian scientist Enrico Fermi was the first to use neutrons instead of charged particles
• neutrons cause the nucleus to disintegrate, get trapped inside or pass right through
• can be used to produce radioactive isotopes of natural elements (iodine)
Radioactive Half-Life
•a measure of the time required by the nuclei of an isotope to decay
• the half-life of a radioactive isotope is the amount of time it takes for half the nuclei in a sample of the isotope to decay
• time varies from isotope to isotope
• the nucleus left after the isotope decays is called the daughter nucleus
Radioactive Dating•the ages of materials such
as rocks & fossils can be dated using radioactive isotopes & their half-lives
•different isotopes are useful in dating different types of materials
Half-Life Decay of Uranium
Radioactive Dating1. determine the amount of
radioactive isotope & its daughter nucleus in a sample
2. calculate the number of half-lives that would have passed to create that amount of daughter nucleus compared to remaining isotope
3. that gives you the amount of time that has passes since the object formed