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Ionic solid · carbonate salt

Calcium carbonate

CaCO₃

Calcium carbonate is an ionic solid composed of Ca²⁺ cations and CO₃²⁻ anions in a 1:1 ratio. The carbonate ion is internally covalent and resonance-delocalized, while the solid as a whole is an extended ionic crystal rather than a collection of discrete CaCO₃ molecules.

Material distinction: limestone, chalk and marble are rocks or materials rich in calcium carbonate, not synonyms for one perfectly pure microscopic crystal.
Essentials

CaCO₃ is a formula unit for an ionic crystal.

The simplest correct picture separates calcium ions from carbonate ions. There is no need to invent a covalent Ca–CO₃ molecule to explain the 1:1 stoichiometric ratio.

Calcium two plus and carbonate two minus shown as the charge-balanced components of calcium carbonate
Beginner view: Ca²⁺ and CO₃²⁻ combine in a 1:1 ratio so the solid is electrically neutral.
Two bonding levels

Ionic between ions; covalent within carbonate.

The C–O bonding inside CO₃²⁻ is covalent and delocalized. Interactions between Ca²⁺ and carbonate ions organize the extended crystal.

Detail

The carbonate ion is trigonal planar and resonance-delocalized.

A single Lewis structure can draw one C=O and two C–O⁻ bonds, but the isolated carbonate ion is better understood through resonance: the three C–O positions are equivalent by symmetry.

Trigonal planar carbonate ion with carbon at the centre and three oxygen atoms, labelled resonance-delocalized
Detail view: the geometry is trigonal planar; resonance avoids treating one oxygen as permanently special.
Crystal polymorphs

CaCO₃ can crystallize in more than one structure.

Calcite and aragonite have the same chemical formula but different crystal structures. Formula alone therefore does not specify the complete solid-state arrangement.

Read the formula

CaCO3 is a compact statement of composition.

Subscripts count atoms in the chemical formula unit. Atom percentages and mass percentages answer different questions because the constituent elements have different atomic masses.

1 Cacalcium atom
1 Ccarbon atom
3 Ooxygen atoms

Percentages are calculated from standard relative atomic masses and rounded for display.

Understand

Acid converts carbonate into carbon dioxide and water.

Carbonate consumes protons. The resulting carbonic-acid chemistry leads to CO₂ and H₂O, which is why carbonate minerals effervesce in acid.

Overall ionic reaction calcium carbonate plus acid gives calcium ions carbon dioxide and water
Gas evolution is a macroscopic clue to the underlying acid–carbonate chemistry.
Geochemical link

Solubility depends strongly on chemical environment.

Pure-water solubility is limited, but dissolved CO₂, pH and complexation can shift carbonate equilibria and change how readily calcium carbonate dissolves or precipitates.

Reference identifiers

Names and identifiers that pin down the chemical identity.

FormulaCaCO₃
CAS Registry Number471-34-1
PubChem CID10112
Standard InChIInChI=1S/CH2O3.Ca/c2-1(3)4;/h(H2,2,3,4);/q;+2/p-2
Advanced

Push past the first model without losing the simple picture.

Are calcite and aragonite different compounds?

They have the same stoichiometric formula CaCO₃ but different crystal structures. They are polymorphs: different solid forms of the same composition.

Why is carbonate drawn with resonance?

No single conventional Lewis structure makes all three C–O positions equivalent. Resonance is a bookkeeping device for the delocalized electronic structure.

Is every white calcium-carbonate material pure CaCO₃?

No. Natural and commercial materials can contain other minerals, water, organic matter or processing additives.

Constituent elements

Connect the compound back to the periodic table.