Archerite
About Archerite
Unique Identifiers
IMA Classification of Archerite
Classification of Archerite
8 : PHOSPHATES, ARSENATES, VANADATES
A : Phosphates, etc. without additional anions, without H2O
D : With only large cations
37 : ANHYDROUS ACID PHOSPHATES, ARSENATES AND VANADATES
1 : Miscellaneous
19 : Phosphates
1 : Phosphates of the alkali metals
Mineral Symbols
| Symbol | Source | Reference for Standard |
|---|---|---|
| Aht | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Physical Properties of Archerite
Optical Data of Archerite
Based on recorded range of RI values above.
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.
Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.
Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.
Chemistry of Archerite
Crystallography of Archerite
Crystal Structure
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| ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
|---|---|---|---|---|---|---|---|
| 0009154 | Archerite | Frazer B C, Pepinsky R (1953) X-ray analysis of the ferroelectric transition in KH2PO4 Acta Crystallographica 6 273-285 | ![]() | 1953 | synthetic | 0 | 126 |
| 0009155 | Archerite | Frazer B C, Pepinsky R (1953) X-ray analysis of the ferroelectric transition in KH2PO4 Acta Crystallographica 6 273-285 | ![]() | 1953 | synthetic, low-temperature form | 0 | 116 |
| 0019080 | Archerite | Ono Y, Yamada N, Hikita T (1991) Structure refinements of the mixed crystal K0.78(NH4)0.22H2PO4 in the temperature range from 20 K to 250K Journal of the Physical Society of Japan 60 2673-2677 | 1991 | synthetic | 0 | 20 | |
| 0013167 | Archerite | Nelmes R J, Meyer G M, Tibballs J E (1982) The crystal structure of tetragonal KH2PO4 and KD2PO4 as a function of temperature Journal of Physics C: Solid State Physics 15 59-75 | 1982 | 0 | 293 | ||
| 0013166 | Archerite | Nelmes R J, Meyer G M, Tibballs J E (1982) The crystal structure of tetragonal KH2PO4 and KD2PO4 as a function of temperature Journal of Physics C: Solid State Physics 15 59-75 | 1982 | 0 | 293 | ||
| 0013165 | Archerite | Nelmes R J, Meyer G M, Tibballs J E (1982) The crystal structure of tetragonal KH2PO4 and KD2PO4 as a function of temperature Journal of Physics C: Solid State Physics 15 59-75 | 1982 | 0 | 293 | ||
| 0013164 | Archerite | Nelmes R J, Meyer G M, Tibballs J E (1982) The crystal structure of tetragonal KH2PO4 and KD2PO4 as a function of temperature Journal of Physics C: Solid State Physics 15 59-75 | 1982 | 0 | 293 | ||
| 0017377 | Archerite | West J (1930) A quantitative X-ray analysis of the structure of potassium dihydrogen phosphate (KH2PO4) _cod_database_code 1010458 Zeitschrift fur Kristallographie 74 306-335 | ![]() | 1930 | 0 | 293 | |
| 0015150 | Archerite | Levy H A, Peterson S W, Simonsen S H (1954) Neutron diffraction study of the ferroelectric modification of potassium dihydrogen phosphate Physical Review 93 1120-1121 | 1954 | 0 | 113 |
X-Ray Powder Diffraction
| d-spacing | Intensity |
|---|---|
| 5.09 Å | (10) |
| 3.72 Å | (100) |
| 3.01 Å | (10) |
| 2.91 Å | (80) |
| 2.64 Å | (20) |
| 2.34 Å | (10) |
| 1.982 Å | (10) |
| 1.953 Å | (50) |
Geological Environment
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Stage 10a: Neoproterozoic oxygenation/terrestrial biosphere | <0.6 |
| 52 : Guano- and urine-derived minerals | <0.4 |
Type Occurrence of Archerite
Synonyms of Archerite
Other Language Names for Archerite
Common Associates
| 2 photos of Archerite associated with Biphosphammite | NH4(H2PO4) |
Related Minerals - Strunz-mindat Grouping
| 8.AD. | 'Unnamed (Monoclinic polymorph of ximengite)' | Bi(PO4) |
| 8.AD. | Keplerite | Ca9(Ca0.5◻0.5)Mg(PO4)7 |
| 8.AD. | Mazorite | Ba3(PO4)2 |
| 8.AD. | Deynekoite | Ca9◻Fe3+(PO4)7 |
| 8.AD. | Monazite-(Gd) | Gd(PO4) |
| 8.AD.05 | Nahpoite | Na2(PO3OH) |
| 8.AD.10 | Weilite | Ca(HAsO4) |
| 8.AD.10 | Švenekite | Ca(H2AsO4)2 |
| 8.AD.10 | Monetite | Ca(PO3OH) |
| 8.AD.15 | Biphosphammite | NH4(H2PO4) |
| 8.AD.20 | Phosphammite | (NH4)2(PO3OH) |
| 8.AD.25 | Buchwaldite | NaCa(PO4) |
| 8.AD.30 | Schulténite | Pb(HAsO4) |
| 8.AD.35 | Dreyerite | Bi(VO4) |
| 8.AD.35 | Wakefieldite-(La) | La(VO4) |
| 8.AD.35 | Anningite-(Ce) | (Ca0.5Ce4+0.5)(VO4) |
| 8.AD.35 | Pretulite | Sc(PO4) |
| 8.AD.35 | Wakefieldite-(Ce) | Ce(VO4) |
| 8.AD.35 | Wakefieldite-(Y) | Y(VO4) |
| 8.AD.35 | Xenotime-(Yb) | Yb(PO4) |
| 8.AD.35 | 'Chernovite-(Ce)' | (Ce,Y)(AsO4) |
| 8.AD.35 | Xenotime-(Gd) | Gd(PO4) |
| 8.AD.35 | Chernovite-(Y) | Y(AsO4) |
| 8.AD.35 | Xenotime-(Y) | Y(PO4) |
| 8.AD.35 | Wakefieldite-(Nd) | Nd(VO4) |
| 8.AD.40 | Pucherite | Bi(VO4) |
| 8.AD.45 | Ximengite | Bi(PO4) |
| 8.AD.50 | 'UM2005-35-VO:CaFePSiTh' | (Th,Ca)(VO4,SiO4,PO4) |
| 8.AD.50 | Rooseveltite | Bi(AsO4) |
| 8.AD.50 | Gasparite-(Ce) | Ce(AsO4) |
| 8.AD.50 | Monazite-(Sm) | Sm(PO4) |
| 8.AD.50 | Monazite-(Ce) | Ce(PO4) |
| 8.AD.50 | Monazite-(La) | La(PO4) |
| 8.AD.50 | Monazite-(Nd) | Nd(PO4) |
| 8.AD.50 | Gasparite-(La) | La(AsO4) |
| 8.AD.50 | Cheralite | CaTh(PO4)2 |
| 8.AD.55 | Tetrarooseveltite | Bi(AsO4) |
| 8.AD.60 | Chursinite | [Hg2]2+Hg2+2[AsO4]2 |
| 8.AD.65 | Clinobisvanite | Bi(VO4) |
| 8.AD.70 | Gurimite | Ba3(VO4)2 |
| 8.AD.75 | Picaite | NaCa[AsO3OH][AsO2(OH)2] |
Radioactivity
| Element | % Content | Activity (Bq/kg) | Radiation Type |
|---|---|---|---|
| Uranium (U) | 0.0000% | 0 | α, β, γ |
| Thorium (Th) | 0.0000% | 0 | α, β, γ |
| Potassium (K) | 28.7307% | 8,907 | β, γ |
For comparison:
- Banana: ~15 Bq per fruit
- Granite: 1,000–3,000 Bq/kg
- EU exemption limit: 10,000 Bq/kg
Note: Risk is shown relative to daily recommended maximum exposure to non-background radiation of 1000 µSv/year. Note that natural background radiation averages around 2400 µSv/year so in reality these risks are probably extremely overstated! With infrequent handling and safe storage natural radioactive minerals do not usually pose much risk.
Note: The mass selector refers to the mass of radioactive mineral present, not the full specimen, also be aware that the matrix may also be radioactive, possibly more radioactive than this mineral!
Activity: –
| Distance | Dose rate | Risk |
|---|---|---|
| 1 cm | ||
| 10 cm | ||
| 1 m |
The external dose rate (D) from a radioactive mineral is estimated by summing the gamma radiation contributions from its Uranium, Thorium, and Potassium content, disregarding daughter-product which may have a significant effect in some cases (eg 'pitchblende'). This involves multiplying the activity (A, in Bq) of each element by its specific gamma ray constant (Γ), which accounts for its unique gamma emissions. The total unshielded dose at 1 cm is then scaled by the square of the distance (r, in cm) and multiplied by a shielding factor (μshield). This calculation provides a 'worst-case' or 'maximum risk' estimate because it assumes the sample is a point source and entirely neglects any self-shielding where radiation is absorbed within the mineral itself, meaning actual doses will typically be lower. The resulting dose rate (D) is expressed in microsieverts per hour (μSv/h).
D = ((AU × ΓU) + (ATh × ΓTh) + (AK × ΓK)) / r2 × μshield
Other Information
Internet Links for Archerite
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References for Archerite
Localities for Archerite
Showing 8 localities.
Locality List
- This locality has map coordinates listed.
- This locality has estimated coordinates.
ⓘ - Click for references and further information on this occurrence.
? - Indicates mineral may be doubtful at this locality.
- Good crystals or important locality for species.
- World class for species or very significant.
(TL) - Type Locality for a valid mineral species.
(FRL) - First Recorded Locality for everything else (eg varieties).
All localities listed without proper references should be considered as questionable.
Australia | |
| R Bottrill collection |
| Mineralogical Magazine 39 (1973) | |
| Bridge (1977) |
Bahamas | |
| Onac B.P. et al. (2009) |
Egypt | |
| Mahmoud et al. (2022) |
Namibia | |
| Martini (1994) +1 other reference |
Saudi Arabia | |
| Saudi Geological Survey Open-File ... +1 other reference |
United Arab Emirates | |
| Audra et al. (2017) |






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The
Petrogale Cave, Madura Roadhouse, Dundas Shire, Western Australia, Australia