Childrenite
Fe2+Al(PO4)(OH)2·H2OIMA symbol: Chdgrandfathered
Childrenite is a phosphate, arsenate, or vanadate mineral with the formula Fe2+Al(PO4)(OH)2·H2O, crystallizing in the orthorhombic system. It has a calculated density of 3.168 g/cm3. Its streak is white.
Photos




Crystallography
| Crystal system | orthorhombic crystal systemWikidata (CC0) |
|---|---|
| Space group | B b e 2 |
| Cell (Å, °) | a = 10.395, b = 13.394, c = 6.918; α = 90, β = 90, γ = 90 |
| Cell volume | 963.197 ų, Z = 8 |
| Axial ratios | 0.7761:1:0.5165calculated from COD 9009311 |
| Source structure | COD 9009311 (Neues Jahrbuch fur Mineralogie, Monatshefte, 1984) — 1 of 2 structures |
Powder X-ray diffraction (calculated)
| d (Å) | 2.815 | 1.521 | 6.697 | 4.367 | 2.381 | 2.812 |
|---|---|---|---|---|---|---|
| I/I₀ | 100 | 50.9 | 44 | 35.5 | 33.2 | 32.5 |
xrd-v1: CuKa1 1.5406A, 2theta 5-90, top10, Imax=100, no DW/PO. Computed from COD 9009311; idealized occupancies, no preferred orientation.
Physical properties
| Density (calculated) | 3.168 g/cm³calculated from COD 9009311 |
|---|---|
| Streak | whitesingle sourceWikidata (CC0) |
Classification
| Nickel-Strunz (10th) | 8.DD.20Wikidata (CC0) |
|---|---|
| Nickel-Strunz (9th) | 8.DD.20Wikidata (CC0) |
| Dana (8th) | 42.7.1.1Wikidata (CC0) |