Topic 4: Atomic Structure Flashcards
Describe John Dalton’s atomic model
In 1804, John Dalton agreed with Democritus that matter was made up of tiny spheres (“atoms”) that couldn’t be broken up, but he reckoned that each element was made up of a different type of “atom”.
Describe J.J. Thompson’s atomic model
Nearly 100 yrs after Dalton, Thompson discovered that particles called electrons could be removed from atoms. So Dalton’s theory was not quite right. He also suggested that atoms were spheres of positive charge with negative electrons stuck in them - The Plum Pudding Model
What experiment did Rutherford do in 1909 and what conclusions did he come to?
He tried firing a beam of alpha particles at a thin gold foil - the alpha scattering experiment.
From the plum pudding model, they expected the particles to pass straight through the gold, or only be slightly deflected.
Although most did go straight through, some were deflected at steeper angles than expected and a few were sent back the way they came - something the plum pudding model couldn’t explain.
Because a few were deflected back, they realised that most of the mass of an atom is concentrated at the centre in a tiny nucleus.
This nucleus must have a positive charge since it repelled some of the alpha particles
They also realised that most of an atom is just empty space because nearly all of the particles passed straight through.
What did Neils Bohr state about an atom?
He stated that electrons orbiting the nucleus do so at certain distances called energy levels. His theoretical calculations agreed with the experimental data.
What did James Chadwick prove in 1932?
He proved the existence of the neutron, which explained the imbalance between the atomic and mass numbers.
The radius of an atom
1 x 10^-10
The radius of a nucleus (atomic)
1 x 10^-14, less than 1/10,000 of the radius of an atom
the number of protons = …?
The number of electrons
What are isotopes?
Isotopes of an element are atoms with the same number of protons but a different number of neutrons.
Define radioactive decay
Radioactive decay is when unstable isotopes decay into other elements and give out radiation as they try to become more stable.
The mass number of an atom = …?
The number of protons + number of neutrons.
Alpha Particle Radiation:
x2 Protons x2 Neutrons \+2 Charge Up to 10cm in air Stopped by paper Strongly ionising
Beta particle radiation:
Consists of fast-moving electrons released by the nucleus -1 charge Around 1m in air Stopped by 5+mm of aluminium Weakly ionising
Gamma Ray Radiation
Consists of electromagnetic waves No charge Can travel km's in air Stopped by about 60cm of lead or a couple of metres of concrete. Very weakly ionising
The form of nuclear equations
atom before decay —-> atom after decay + radiation emmitted
The golden rule for nuclear equations:
the total mass and atomic numbers MUST be EQUAL on both sides
Alpha decay:
Large unstable nuclei can emit an alpha particle
Four particles are removed from the nucleus so THE MASS NUMBER FALLS BY 4
x2 protons are removed from the nucleus so THE ATOMIC NUMBER DROPS BY TWO
As the atomic number has fallen by 2, A NEW ELEMENT HAS FORMED.