TOPIC 2 Flashcards
Atomic Theories
Dalton
1803
Thompson
1904
Rutherford
1911
Bohr
1913
Schrödinger
1926
Rutherfords gold foil experiment
Rutherford recalled that “it was as if you fired a 15-inch shell at a piece of tissue paper and it came back and hit you”
He shot a beam of alpha particles coming from a radioactive source at a sheet of gold foil, and a with a detector identified that some of the particles were deflected by small angles, indicating a small concentrated positive charge; he concluded that a small, dense nucleus (positively charged) was causing the deflections.
Mass number and Atomic number
Atoms of and element are characterized by 2 numbers
A = Mass Number = p+ + n• = number of nucleones (particles in the nucleus of the atom)
Mass number A can only be given for an atom of an element (not an element as a whole) and must always be a whole number.
Z = Atomic Number = p+ = position of an element in the P.T. = nuclear charge
Atoms are…
Neutral.
This means that they have the same amount of p+ and e-
Relative mass and charge of e-, p+ and n•
p+ n• e-
Relative mass 1 1 0
Charge +1 0 -1
No unit, its mass in comparison with themselves.
The e- has mass, because its matter, but in comparison to the p+ and n• its nearly neutral.
Ions
Ions are formed when the number of p+ in an atom is no longer balanced by the number of e- in the atom.
They are chemically charged elements
When an atom loses e-, a + ion is formed
- cation
When an atom gains e-, a - ion is formed
- anion
Isotopes
Atoms of the same element with different mass number
They have the same atomic number, and the same chemical properties, but different number of n• and different physical properties.
Mass number (Ar)
Mass number is called the relative atomic mass of an element (Ar).
The Ar of an element takes into account the relative abundances of its isotopes.
“The Ar of an element is the average of its isotopes, considering their abundances.”
Ar = ?
Ar = A x %abundance / 100
A = mass number
Schrödinger’s model of the atom
He introduces atomic orbitals: an atomic orbital is a region around the nucleus in which we are most likely to find and e- (95% - 99%)
ORBIT AND ORBITAL ARE DIFFERENT
(Orbit is a fixed path [main energy level’s - Bohr’s model of the atom])
Schrödinger stated that e- do not move in set paths around the nucleus, but in waves. Its impossible to know the exact location of an e-; instead, we have “clouds of probability ” calles orbitals, in which we are more likely to find e-
Atomic orbitals characteristics
Any orbital can hold a maximum of two e- of opposite spin.
Atomic orbitals are found within a specific energy sub-level, within a main energy level.
Main and Sub energy levels
Types of sub-levels
S: 1 orbital: 2e- max
P: 3 orbitals: 6e- max
D: 5 orbitals: 10e- max
F: 7 orbitals: 14e- max
Main energy levels
1) 2e- max
s: 2e-
2)
8e- max
s: 2e-
p: 6e-
3) 18e- max
s: 2e-
p: 6e-
d: 10e-
4) 32e- max
s: 2e-
p: 6e-
d: 10e-
f: 14e-
5)
s
p
d
f
n)
…
For the same main energy level ‘n’, the energy of the sub-levels increases as s<p<d<f
“Rule of rain”
Oder in which we fill the orbitals and sub-levels
(Tabla)
Num: main energy level (Bohr)
Letter: energy sub-levels (Schrödinger)
1s
2s 2p
3s 3p 3d
4s 4p 4d 4f
5s 5p 5d 5f
Increasing energy—>
As the e- jumps away from the nucleus, the electromagnetic force of attraction towards it decreases. As a result, it become less stable, therefore accounting for a higher energy.
e- configuration
Full ground state (normal e- configuration- no excited e-)
Condensed (use the noble gas previous to the element to reduce the configuration, then continue until reaching the element on the P.T.)
e- configuration of ions
When + ions are formed, we first remove e- with the highest energy (highest main energy level)
The e- configuration of - ions is determined by simply adding the e- into the next available electron orbital.