Lesson 1 · 20 min

Inside the atom: protons, neutrons and electrons

How did Rutherford find the nucleus? How do three particle counts pin down an atom or ion? And why is chlorine’s atomic mass 35.45 — a value no chlorine atom has?

In this lesson

  • State the charge, mass and location of protons, neutrons and electrons
  • Write a nuclide symbol and charge from the particle counts — and read the counts back
  • Explain what isotopes are and compute a relative atomic mass from abundances
  • Describe what Rutherford’s scattering experiment saw and how it revealed the nucleus

The periodic table gives chlorine a relative atomic mass of 35.45. Yet if you could weigh chlorine atoms one at a time, you would never find 35.45 — every chlorine atom weighs close to 35 or to 37. Where does a number that matches no atom come from? To answer, we first have to open the atom and see what is inside.

An atom that is almost empty

In 1909 Geiger and Marsden fired α particles (helium nuclei, charge +2) from a radioactive source at very thin metal foils. In the popular “plum pudding” model, positive charge was spread through the whole atom, so α particles should pass almost undisturbed. Most did go straight through — but about 1 in 8000 bounced back, deflected by more than 90°.

In 1911 Rutherford worked out what this meant: the atom’s positive charge and nearly all of its mass must sit in a tiny nucleus, with the electrons spread through the vast space around it. A nucleus has a radius of about 10−1510^{-15} m, the atom about 10−1010^{-10} m — if the atom were a football stadium, the nucleus would be a pea on the centre spot.

The three particles that build atoms
ParticleChargeMass / uWhere
proton p+11.00728in the nucleus
neutron n01.00866in the nucleus
electron e⁻−10.000549 (≈ 1/1836)outside the nucleus, filling almost all the volume
Source: CODATA 2018 recommended values (NIST); 1 u = 1.66054 × 10⁻²⁷ kg.

Predict first

A particle has 17 protons, 18 neutrons and 18 electrons. What is it?

Pick an answer and lock it in before you look. A wrong guess teaches more than no guess.

Three numbers pin a particle down

  • Atomic number Z = number of protons. It fixes the element: change one proton and you have a different element.
  • Mass number A = protons + neutrons. Electrons are too light to count.
  • Charge = protons − electrons. Losing electrons makes a cation; gaining them makes an anion.

A nuclide symbol puts the three numbers on three corners of the element symbol: mass number top left, atomic number bottom left, charge top right.

ZAXqA=Z+Nq=Z−ne{}^{A}_{Z}\mathrm{X}^{q}\qquad A = Z + N\qquad q = Z - n_\mathrm{e}
For example X1735X217235ClX−\ce{^{35}_{17}Cl-}: 17 protons, 18 neutrons, 18 electrons.
ZZ
atomic number (protons)
NN
number of neutrons
AA
mass number = protons + neutrons
nen_\mathrm{e}
number of electrons
qq
net charge (in units of e)
Protons · neutrons · electrons

Atom builder

Protons
6
Neutrons
6
Electrons
6
++++++−−−−−−
  • +proton (+)
  • neutron (neutral)
  • −electron (−)
The nucleus is enlarged ten-thousandfold; to scale it would be an invisible dot.
Z = 6 ¹²C Carbon · Nonmetal
Nuclide symbol
612C{}^{12}_{6}\mathrm{C}
Mass number A = Z + N
6 + 6 = 12
Net charge
6 − 6 = 0 neutral atom
Neutrons / protons
1.00

Stable nuclide · natural abundance 98.93 %

Stable isotopes of Carbon

Radioactive examples

Mass
≈ 12 u electrons carry only 0.027 %
Size
nuclear radius ≈ 2.7 fm, atom ≈ 76 pm: the atom is ~27,700× wider
Try
Element, mass number and charge follow directly from the particle counts. Stable nuclides and abundances: IUPAC isotopic compositions (2009/2013); half-lives: NUBASE2020. Nuclear radius from R ≈ 1.2 fm · A^(1/3); atomic size from the covalent radius. Shells are a Bohr-style sketch, and nucleon positions are illustrative.
Build ¹²C, then add two neutrons to make ¹⁴C: still carbon, but the nucleus is now unstable. Add or remove electrons and watch the charge; finally change the proton number — the whole element changes. Note the size row: the atom is tens of thousands of times wider than its nucleus.

Isotopes

Atoms with the same number of protons but different numbers of neutrons are isotopes of one element. They have the same electrons, so their chemistry is almost identical; only the mass differs, and whether the nucleus is stable. Hydrogen has three: protium X1X221H\ce{^{1}H} (no neutron), deuterium X2X222H\ce{^{2}H} (one) and radioactive tritium X3X223H\ce{^{3}H}. Carbon-12 and carbon-13 are stable, carbon-14 decays — archaeologists date objects with its half-life of about 5700 years.

Most elements occur as a mixture of isotopes, in proportions that are nearly the same all over the Earth. That is where 35.45 comes from.

The average a mass spectrometer weighs

A mass spectrometer turns atoms into singly charged ions, accelerates them in an electric field and bends them in a magnetic field. Light ions bend more than heavy ones, so each isotope lands in its own place, and the height of each peak is proportional to how many there are. An element’s relative atomic mass is the abundance-weighted mean of its isotope masses.

Ar=∑imi xiA_\mathrm{r} = \sum_i m_i\,x_i
Use abundances as fractions (all the xix_i add up to 1).
ArA_\mathrm{r}
relative atomic mass
mim_i
mass of isotope i (u)
xix_i
natural abundance of isotope i (fraction)
Mass-to-charge · abundance · atomic weight

Isotope mass spectrometer

35 · 75.76% 37 · 24.24%333435363738Mass m / u (singly charged ions, so m/z)020406080100Relative abundance / %

Atomic weight from the spectrum

IsotopeMass m / uAbundance x / %m·x / u
³⁵Cl34.9688575.7626.4924
³⁷Cl36.9659024.248.9605
Sum100.0035.4529
Ar(Cl)=∑imixi=34.969×0.7576+36.966×0.2424=35.453\begin{aligned}A_\mathrm{r}(\mathrm{Cl}) &= \sum_i m_i x_i \\ &= 34.969\times0.7576 + 36.966\times0.2424 \\ &= 35.453\end{aligned}

Standard atomic weight in the element table: 35.45 · difference 0.0029 (within natural variation and the table’s last digit)

Isotope masses from the AME2020 atomic-mass evaluation; abundances from the IUPAC representative isotopic compositions (real samples vary slightly). The mean Σ mᵢxᵢ is computed in the browser. Peaks are drawn as thin bars: a real instrument measures ions by m/z, its peaks have width, and equal ionisation and detector response is assumed for every isotope. X₂⁺ peaks assume the two atoms are drawn independently from the natural mixture.
Start with chlorine: two peaks, about 3 : 1. Switch to Cl₂⁺ — why three peaks now, roughly 9 : 6 : 1? Then look at bromine (two almost equal peaks) and tin (ten isotopes), and switch on the log scale to find the deuterium in hydrogen.

Worked example

Compute chlorine’s relative atomic mass

The mass spectrum of natural chlorine shows 75.76 % ³⁵Cl (34.969 u) and 24.24 % ³⁷Cl (36.966 u). Find chlorine’s relative atomic mass.

Concept check

What do ¹⁴C and ¹⁴N have in common?

Try the calculation

Boron has two stable isotopes: ¹⁰B (10.013 u, 19.9 %) and ¹¹B (11.009 u, 80.1 %). What is boron’s relative atomic mass?

Key takeaways

  • An atom is a tiny, dense nucleus (protons + neutrons) surrounded by electrons; Rutherford’s α-scattering experiment revealed the nucleus.
  • Proton number Z fixes the element, mass number A = Z + N, and charge = protons − electrons; ions come from gaining or losing electrons.
  • Isotopes share Z but differ in N: nearly identical chemistry, possibly different nuclear stability.
  • Relative atomic mass is the abundance-weighted mean Ar=∑mixiA_\mathrm{r} = \sum m_i x_i — which is why it is rarely a whole number.
Progress is stored only in this browser and never uploaded.

Data and references

  1. H. Geiger & E. Marsden, “On a Diffuse Reflection of the α-Particles”, Proc. R. Soc. Lond. A 82, 495 (1909).
  2. E. Rutherford, “The Scattering of α and β Particles by Matter and the Structure of the Atom”, Phil. Mag. 21, 669 (1911).
  3. E. Tiesinga et al., CODATA Recommended Values of the Fundamental Physical Constants: 2018, Rev. Mod. Phys. 93, 025010 (2021).
  4. M. Berglund & M. E. Wieser, “Isotopic compositions of the elements 2009 (IUPAC Technical Report)”, Pure Appl. Chem. 83, 397 (2011); J. Meija et al., “Isotopic compositions of the elements 2013”, Pure Appl. Chem. 88, 293 (2016).
  5. M. Wang et al., “The AME 2020 atomic mass evaluation (II)”, Chinese Phys. C 45, 030003 (2021); F. G. Kondev et al., “The NUBASE2020 evaluation of nuclear physics properties”, Chinese Phys. C 45, 030001 (2021).
  6. K. S. Krane, Introductory Nuclear Physics, Wiley (1988), ch. 3 (nuclear radius).