3.1.1 atomic structure (just things not too good at) Flashcards
john dalton
atoms were solid spheres that make up elements, different spheres for each element
JJ Thompson
plum pudding model , showing atoms contain electrons
Ernest Rutherford
conducted the alpha scattering gold foil experiment to produce nuclear model .
- fired positively charged alpha particles at a very thin sheet of gold
- Ppm suggested : most particles slightly deflected by positive ‘pudding’
- actually : most straight through (most atom is empty space) some deflected (positive centre)
Niels Bohr
adapted nuclear model , putting electrons in shells/ orbitals of fixed energy .
- they raised electrons in a ‘cloud’ around the nucleus spiral down into the nucleus , causing it to collapse
- when electrons move to a new shell, electromagnetic radiation ( with fixed energy/ frequency) is emitted (down shells) or absorbed (up shells/ away from nucleus)
then
scientists discovered that not all electrons in the same shell have the same energy so refined the model to include sub shells. Not a perfect model but is useful as it is simple and explains many experimental observations e.g. bonding and ionisation energy
mass number [A]
total number of protons + neutrons in the nucleus. Nucleons are responsible for almost all the mass as electrons have a tiny mass
atomic number [Z]
the number of protons in the nucleus. This also equals the number of electrons in the atom meaning atoms are electrically neutral. The number of electrons in the outer shell of an atom determines the chemical properties of the element , how it reacts and what sort of element it is : its chemical identity. All atoms of the same element have the same atomic number
relative atomic mass [Ar]
the average mass of an atom of an element , taking into account its naturally occurring isotopes , relative to 1/12th of the mass of an atom of carbon -12
why C-12
too small numbers so relative to C-12 takes into account the percentage abundances of the isotopes
how to work it out
Ar = (isotope mass number x % abundance) / sum of % isotope abundance
relative isotopic mass
mass of an atom of an isotope relative to 1/12th the mass of an atom of carbon -12 . Always a whole number
relative molecular mass [Mr]
average mass of a molecule in relation to 1/12 the mass of a carbon -12 atom
how to calculate
Mr = sum of Ar in formula for the molecule
isotope
an atom of the same element with the same number of protons (atomic number) and a different number of neutrons (so different mass number)
about their properties
- same chemical properties as they have the same electron configuration
- slightly different physical properties as they depend on the mass of the atom e.g. density
radioactive?
isotopes can be radioactive if they are unstable (extra protons or neutrons in the nucleus creating extra energy)
- they emit radiation as they decay + the rate of decay is measured by half- life ( the time it takes for half of its radioactivity to decay)
- they have lots of uses e.g. : carbon dating. Carbon -14 isotope is radioactive with a long half life found in all living things . Scientists can work backwards to see how long a living organism has been dead for .
time of flight mass spectrometer
powerful instrumental technique that is useful for the accurate determination of relative isotopic masses and relative abundances. it determines the masses of separate atoms/molecules and is used by forensic scientists to help identify illegal drugs. can be used to work out relative atomic masses [Ar] to identify elements and relative molecular masses [Mr] .
It works by forming ions, then separating them according to the ratio of their charge: maths
stages of TOFMS
- ionisation
- acceleration
- ion drift
- detection
- data analysis