Ca4Fe4H2O30Si10
This compound is a complex silicate mineral containing calcium and iron. It belongs to a group of minerals often found in geological formations and is primarily studied for its structural characteristics in mineralogy.

Key Properties
Cross-validated computational properties for Ca4Fe4H2O30Si10, aggregated across 3 databases.
Band GapEnergy needed to move an electron from the valence band to the conduction band. Lower or zero values tend to behave more metallic; larger gaps are more insulating or semiconducting.
Energy Above HullThermodynamic distance from the most stable set of competing phases. 0 eV/atom is on the convex hull; small positive values may still be experimentally accessible.
StabilityA plain-language summary of the best reported energy-above-hull result. It reflects whether the lowest-energy structure is on, near, or far from the stability hull.
StructuresCount of reported calculated crystal structures for this formula, including alternate polymorphs, source databases, and observed space groups.
Reported Structures
Lowest-energy structures reported for Ca4Fe4H2O30Si10, ranked by energy above hull.
| Space GroupSymmetry classification of the crystal arrangement. The number is the international space-group index. | Crystal SystemBroad lattice family, such as cubic, tetragonal, monoclinic, or triclinic, derived from unit-cell symmetry. | Band Gap (eV)Electronic gap calculated for this specific reported structure, measured in electronvolts. | E above hull (eV/atom)Thermodynamic distance from the convex hull for this structure, normalized per atom. Lower is generally more stable. | E/atom (eV)Computed total energy normalized per atom. Use energy above hull, not this value alone, when comparing stability. | Density (g/cm³)Mass per relaxed crystal volume, reported in grams per cubic centimeter. |
|---|---|---|---|---|---|
| P-1 (No. 2) | triclinic | 1.88 | 0.0061 | -7.953 | 3.25 |
| No. 0 | unknown | — | — | — | 1.63 |
| P-1 (No. 2) | — | — | — | — | — |
| P-1 (No. 2) | — | — | — | — | — |
Applications
Where Ca4Fe4H2O30Si10 is used.
Frequently Asked Questions
Common questions about Ca4Fe4H2O30Si10, answered from cross-validated data.
What is Ca4Fe4H2O30Si10?
This compound is a complex silicate mineral containing calcium and iron. It belongs to a group of minerals often found in geological formations and is primarily studied for its structural characteristics in mineralogy.
What is Ca4Fe4H2O30Si10 used for?
What is the band gap of Ca4Fe4H2O30Si10?
Is Ca4Fe4H2O30Si10 a metal, semiconductor, or insulator?
Is Ca4Fe4H2O30Si10 thermodynamically stable?
What is the crystal structure of Ca4Fe4H2O30Si10?
What is the density of Ca4Fe4H2O30Si10?
How many polymorphs of Ca4Fe4H2O30Si10 are known?
What elements does Ca4Fe4H2O30Si10 contain?
Where does the data for Ca4Fe4H2O30Si10 come from?
Data sources & attribution
- materials_project — Data from the Materials Project. Cite: Jain et al., APL Materials 1, 011002 (2013).
- cod — Data from the Crystallography Open Database. Cite: Grazulis et al., Nucleic Acids Res. 40, D420 (2012).
- aflow — Data from AFLOW. Cite: Curtarolo et al., Comp. Mater. Sci. 58, 218 (2012).
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