Atom Calculator

Explore atomic structure: find protons, neutrons, electrons, mass number, and isotope notation for any element. Includes ion charges, isotope data, and periodic table reference.

Quick Select

Leave blank for most common isotope
5626Fe
IronTransition metal
Protons
26
Defines the element (atomic number Z)
Neutrons
30
Mass number (56) minus atomic number (26)
Electrons
26
Equal to protons in neutral atom
Mass Number (A)
56
Total nucleons (protons + neutrons)
Atomic Mass
55.845 amu
Weighted average of all natural isotopes
N/Z Ratio
1.154
Within band of stability
Net Charge
0 (neutral)
Neutral atom

Particle Composition

Protons
26
Neutrons
30
Electrons
26

Element Reference Table

ZSymbolNameAtomic MassCategory
1HHydrogen1.008Nonmetal
2HeHelium4.003Noble gas
3LiLithium6.941Alkali metal
4BeBeryllium9.012Alkaline earth
5BBoron10.81Metalloid
6CCarbon12.011Nonmetal
7NNitrogen14.007Nonmetal
8OOxygen15.999Nonmetal
9FFluorine18.998Halogen
10NeNeon20.18Noble gas
11NaSodium22.99Alkali metal
12MgMagnesium24.305Alkaline earth
13AlAluminium26.982Post-transition
14SiSilicon28.086Metalloid
15PPhosphorus30.974Nonmetal
16SSulfur32.06Nonmetal
17ClChlorine35.45Halogen
18ArArgon39.948Noble gas
19KPotassium39.098Alkali metal
20CaCalcium40.078Alkaline earth
Planning notes, formulas, and examples

About the Atom Calculator

Atoms are the fundamental building blocks of matter, composed of protons, neutrons, and electrons. The atomic number (Z) defines the element and equals the number of protons in the nucleus. The mass number (A) is the total of protons and neutrons. Electrons orbit the nucleus and determine chemical behavior — in a neutral atom, the number of electrons equals the number of protons.

Understanding atomic structure is essential for all of chemistry. The number of protons determines the element's identity, the number of neutrons defines the isotope, and the electron configuration governs chemical bonding and reactivity. Ions form when atoms gain or lose electrons, changing the net charge while keeping the same nucleus.

This calculator lets you look up any element by name, symbol, or atomic number and quickly see its subatomic particle counts, isotope notation, common ions, and key properties. You can adjust the mass number to explore different isotopes and modify the charge to see how ions form. It serves as a comprehensive atomic structure reference tool.

When This Page Helps

Quickly determine the subatomic structure of any element, including ions and specific isotopes. This is essential for chemistry students learning atomic theory, nuclear chemistry, and electron configuration.

How to Use the Inputs

  1. Enter an element symbol (e.g., Fe), name (e.g., Iron), or atomic number (e.g., 26).
  2. View the number of protons, neutrons, and electrons for the neutral atom.
  3. Adjust the mass number to explore different isotopes.
  4. Set an ion charge to see how electron count changes.
  5. Click preset elements to quickly load common examples.
  6. Review the nuclear notation and isotope information.
  7. Check the reference table for the first 36 elements.
Formula used
Atomic Number (Z) = number of protons = number of electrons (neutral atom) Mass Number (A) = protons + neutrons Neutrons (N) = A - Z Electrons in ion = Z - charge Isotope notation: ᴬ_Z X (e.g., ¹²₆C)

Example Calculation

Result: Fe³⁺: 26p, 30n, 23e⁻

Iron (Fe) has atomic number 26, so 26 protons. With mass number 56: neutrons = 56 - 26 = 30. As Fe³⁺ (lost 3 electrons): electrons = 26 - 3 = 23. The nuclear notation is ⁵⁶₂₆Fe³⁺.

Tips & Best Practices

  • The mass number (A) is always a whole number. The atomic mass on the periodic table is a weighted average and usually isn't.
  • For main group elements, common ion charges follow a pattern: Group 1 = +1, Group 2 = +2, Group 17 = -1, Group 16 = -2.
  • Transition metals can form multiple ions (e.g., Fe²⁺ and Fe³⁺) because of partially filled d-orbitals.
  • Radioactive isotopes decay by emitting alpha (²He), beta (electron), or gamma (photon) radiation.
  • The neutron-to-proton ratio determines nuclear stability. Light elements are stable near N/Z ≈ 1; heavy elements need N/Z ≈ 1.5.
  • Elements beyond uranium (Z > 92) are all synthetic and radioactive.

Subatomic Particles

The atom consists of a dense nucleus containing protons (positive charge, mass ≈ 1 amu) and neutrons (neutral, mass ≈ 1 amu), surrounded by electrons (negative charge, mass ≈ 1/1836 amu). The nucleus is incredibly small — about 10⁻¹⁵ m compared to the atom's 10⁻¹⁰ m — yet contains over 99.9% of the atom's mass.

Nuclear Stability and Isotopes

Not all combinations of protons and neutrons are stable. The band of stability shows which isotopes are stable versus radioactive. Light elements (Z < 20) tend to have N ≈ Z. Heavier elements require proportionally more neutrons for stability. Elements with even numbers of protons and/or neutrons tend to be more stable due to nuclear shell effects.

Applications of Isotopes

Isotopes have numerous practical applications: ¹⁴C dating in archaeology, ¹³¹I in thyroid treatment, ²³⁵U in nuclear power, ²H (deuterium) in NMR spectroscopy, and ¹⁸O in metabolic tracer studies. Stable isotope ratios are used in geochemistry, forensics, and food authentication.

Sources & Methodology

Last updated:

Frequently Asked Questions

  • The number of protons (atomic number Z) uniquely identifies the element. Changing the number of protons changes the element entirely (nuclear transmutation).