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e- mass
9.109 × 10-31 kg
e- charge
- 1.602 × 10-19 coulombs
p+ mass
1.673 × 10-27 kg
p+ charge
+ 1.602 × 10-19 coulombs
Thomson Model of Atom
Plum Pudding Model
Electrons randomly distributed throughout atom
mass/ pos. charge uniformly distributed throughout atom

α (alpha particle)
He2+
Rutherford’s Model of Atom
α- particle scattering experiment

Rutherford Observations
Most α- particles passed undeflected
Small fraction of α- particles deflected by some angles
Very few particles (1/20000) bounced back at 180°
Rutherford Conclusion
Most space in atom is empty
pos. charge in atom is present in small volume
pos. charge concentrated at centre of nucleus which has very small volume
Rutherford Results
Nucleus surrounded by e- revolving around it in orbits (solar system resemblance)
e- and nucleus held by electrostatic force of attraction (EFA)
pos. charge/most mass of atom concentrated in nucleus at centre
Nucleons: p+ and n0 in nucleus collectively
size of nucleus very small than size of atom
r nucleus = 10-15 m
r atom = 10-10 m
r atom
105 x r nucleus
Vol. atom
1015 x vol. nucleus
Radius of Nucleus
R = Ro(A)1/3
Ro = 1.2 × 10-15 m
A = mass number
Penetration Power
α < ß < γ
ß = 100x
γ = 1000x
Atomic Nuber (Z)
no. of p+
no of e-
Mass Number (A)
n + p
neutrons formula
A-Z (mass - atomic nos)
Charged atom
Z = no of e + charge on atom
Isotopes
Same Z, diff. A
change in neutrons
has diff. physical properties
same chemical properties (e- are same)
Isobars
same A, diff Z
diff. elements
diff. chemical and physical properties
Average Atomic Mass (AAM)
Case 1 - Isotope %:
mass = m
% = x
AAM = (m1x1)+(m2x2)+(m3x3)/100
Case 2 - Isotope fraction:
mass = m
fraction = f
AAM = m1f1 + m2f2 + m3f3

Mass Spectrometry
measures mass of isotopes
see picture for sample pattern graph

Isoelectronic
Species w same no of e-
Isotones
Species w same no of n0
Isodiaphers
Species w same diff. of n0 and p+ (n-p)
n-p ≠ 0
Isosters
Species w same no of atoms + same no of e-