Heulandite-Ca

(Ca,Na,K)5(Si27Al9)O72 · 26H2O
IMA status
  • Approved
  • Grandfathered
IMA symbol
Hul-Ca
IMA approved
1997
Also known as
  • Heulandiet-Ca

History

The name on this page honours a dealer, not a discoverer. Heulandite remembers John Henry Heuland (1778–1856), a mineral collector and dealer who lived and traded in England. The "-Ca" tagged onto it is something else entirely. It is a modern label, added more than a century later, that records which element sits inside the crystal. The two halves of the name come from two very different worlds.

The mineral itself was first noticed in 1818. The German mineralogist August Breithaupt pulled it apart from stilbite, a look-alike it had been confused with, and called it euzeolite — "beautiful zeolite". A zeolite is a mineral built around an open, cage-like framework of silicon, aluminium and oxygen. Water and loose metal atoms sit tucked into the gaps. Breithaupt's name did not stick.

Four years later, the English mineralogist Henry James Brooke reached the same conclusion on his own. In 1822 he named the mineral heulandite, after Heuland. Heuland had an international reputation in his trade, yet no portrait of him is known to survive.

For most of the next two centuries, heulandite was treated as a single mineral species. That changed in 1997. The International Mineralogical Association, the body that decides what counts as a distinct mineral, reclassified heulandite as a series rather than one species. The framework is the same throughout, but the loose atoms inside it vary. Whichever element dominates gives the specimen its full name — heulandite-Ca when calcium leads, then heulandite-Na, -K and -Sr for sodium, potassium and strontium. A barium-led member, heulandite-Ba, was added to the list in 2002. The mineral catalogued here, heulandite-Ca, is the calcium-dominant member of that series.

Industrial & practical applications

Heulandite-Ca earns its keep mostly on a collector's shelf. Like other zeolites, it has a useful trick. The loose calcium, sodium and potassium atoms inside its open framework swap freely for other dissolved metals passing through. That swapping is called cation exchange. It is what makes the mineral useful in water softeners.

The same property drives the bulk industrial work, but that work rarely falls to heulandite itself. Natural zeolites are cheap, selective and easy to maintain, which suits them to stripping pollutants out of water. They pull ammonium and heavy metals such as lead, cadmium and copper from wastewater. Heulandite is one of the acid-resistant, high-silica zeolites used this way. In farming and animal husbandry, though, the cheaper and more abundant zeolite clinoptilolite does most of the soil-conditioning and cattle-feed work.

The high-value jobs almost all use manufactured zeolites, not mined ones. These are the molecular sieves that sort gases by size, the catalysts that crack petroleum, and the ion-exchange beds in detergents. More than two hundred synthetic zeolites have been reported, made in a uniform, phase-pure state that a natural crystal cannot match. Natural heulandite-Ca is left, for the most part, to collectors and to mineralogists studying the zeolite framework.

Where it forms, where it's found

Geological setting

Cavities in basalt and as a devitrification product from volcanic glasses.

Type locality
Strathclyde
  1. Scotland
  2. UK
279recorded occurrences
Source · OpenStreetMap

Varieties

Physical

Hardness
123456789103.5 – 4/ 10 MOHS
  1. 1Talc
  2. 2Gypsum
  3. 3Calcite
  4. 4Fluorite
  5. 5Apatite
  6. 6Orthoclase
  7. 7Quartz
  8. 8Topaz
  9. 9Corundum
  10. 10Diamond
Lustre
Vitreous · Pearly
Transparency
Transparent
Colour
White · colorless · red · yellow · brown · green
Streak
White
Tenacity
brittle
Cleavage
Perfect

Perfect on the (010)

Fracture
Irregular/Uneven · Sub-Conchoidal
Density
2.1 g/cm³

Optical

Optical type
Biaxial (+) · 2V measured = 10 – 48° · 2V calc = 76°
Refractive index
1.491 – 1.512
Surface relief
Moderate
Principal indices
nα 1.491 – 1.505 · nβ 1.493 – 1.503 · nγ 1.5 – 1.512
Dispersion
r > v distinct
Extinction
Z = b; X ∧ a = 0°-34°; Y ∧ c = 0°-32°.
Michel-Lévy diagramhighlighted lineδ = 0.0080
Attainable Michel-Lévy rangeΔ ∈ [0, t·δmax]80 nm1st order
Δ = 0Δmax
Thin-section mosaic70 grains · random 3D orientations
PPLpleochroism per grain
XPLindependent extinctions · rotate the stage
Interference simulatorsingle grain · PPL ↔ XPL
PPLpleochroism only · colour blends on rotation
XPLinterference colour · extinct every 90°
Retardation80 nm
Order1st order
XPL colour

Crystallography

Crystal system
Monoclinic
Space group
C2/m
Cell parameters
a = 17.73 Å · b = 17.82 Å · c = 7.43 Å
Cell angles
β = 116.33 °
Ratio a:b:c
1 : 1.005 : 0.419
Z
2
Morphology

Rhombic prisms, or coffin-shaped tabular crystals, granular, massive. Often in curved aggregates.

Twinning

(100) is twin and contact plane.

Comment

Merkle & Slaughter (1967). The reduced cell has beta ~113°. May be triclinic due to Al-Si ordering.

Crystal structure

Chemical composition

Constituent elements
Mass composition breakdown
ElementAtoms At. mass g/mol Mass g/molMass share
8OOxygenOxygen9815.9991567.902
50.06%
14SiSiliconSilicon2728.085758.295
24.21%
13AlAluminiumAluminium926.982242.838
7.75%
20CaCalciumCalcium540.078200.390
6.40%
19KPotassiumPotassium539.098195.490
6.24%
11NaSodiumSodium522.990114.950
3.67%
1HHydrogenHydrogen521.00852.416
1.67%
Total3132.281100.00%

Mass share = atoms × atomic mass ÷ molar mass × 100

From IMA formula

Synonyms

  • Heulandiet-Ca

In other languages

German
Heulandit-Ca
Italian
Heulandite-Ca
Chinese
钙片沸石

Classification

Strunz
10th ed.

9.GE.05

  • 9SilicatesClass
  • 9.GTektosilicates with zeolitic H2O; zeolite familyDivision
  • 9.GEChains of T10O20 TetrahedraGroup
  • 9.GE.05Heulandite-CaSpecies
Dana
8th ed.

77.01.04.01

  • 77Tectosilicates ZeolitesClass
  • 77.01Zeolite group - True zeolitesType
  • 77.01.04Heulandite and related speciesGroup
  • 77.01.04.01Heulandite-CaSpecies

Group, growth & confusion

In the same group
4 members
Often grow together
2 minerals

Literature, links & citation

Citations
  1. 1968Merkle, A. B., Slaughter, M. (1968) Determination and refinement of the structure of heulandite. American Mineralogist, 53 (7-8) 1120-1138
  2. 1972Alberti, A. (1972) On the crystal structure of the zeolite heulandite. TMPM Tschermaks Mineralogische und Petrographische Mitteilungen, 18 (2). 129-146 doi:10.1007/bf01081798DOI: 10.1007/bf01081798
  3. 1997Coombs, Douglas S., Alberti, Alberto, Armbruster, Thomas, Artioli, Gilberto, Colella, Carmine, Galli, Ermanno, Grice, Joel D., Liebau, Friedrich, Mandarino, Joseph A., Minato, Hideo, et al. (1997) Recommended nomenclature for zeolite minerals; report of the Subcommittee on Zeolites of the International Mineralogical Association, Commission on New Minerals and Mineral Names. The Canadian Mineralogist, 35 (6). 1571-1606
  4. 1998Esenli, Fahri, Kumbasar, Isik (1998) X-Ray Diffraction Intensity Ratios I(111)/I(3¯11) of Natural Heulandites and Clinoptilolites. Clays and Clay Minerals, 46 (6) 679-686 doi:10.1346/ccmn.1998.0460608DOI: 10.1346/ccmn.1998.0460608
  5. 2001Comodi, Paola, Gatta, Giacomo Diego, Zanazzi, Pier Francesco (2001) High-pressure structural behaviour of heulandite. European Journal of Mineralogy, 13 (3) 497-505 doi:10.1127/0935-1221/2001/0013-0497DOI: 10.1127/0935-1221/2001/0013-0497
Cite this entry
@misc{mineral2026,
  author    = {Mineral Index editorial board},
  title     = {Heulandite-Ca — Mineral Index},
  year      = {2026},
  url       = {https://mineralindex.org/minerals/heulandite-ca-6988},
  note      = {Accessed 2026-05-11}
}