Maricite

Maricite
Marićite from the Rapid Creek area of northern Yukon, Canada
General
Category	Phosphate mineral
Formula (repeating unit)	NaFe2+PO4
Strunz classification	08.AC.20
Crystal symmetry	Orthorhombic dipyramidal H-M symbol: (2/m 2/m 2/m) Space group: Pmnb
Unit cell	a = 6.867 Å, b = 8.989 Å, c = 5.049 Å; Z=4
Identification
Color	Dark gray, brown to pale brown, nearly colorless
Crystal habit	Radial aggregates, nodular
Crystal system	Orthorhombic
Cleavage	None observed
Fracture	Irregular/uneven, splintery
Tenacity	Brittle
Mohs scale hardness	4 - 4.5
Luster	Sub-vitreous, greasy
Streak	White to light gray white
Diaphaneity	Transparent to translucent
Specific gravity	3.66
Optical properties	Biaxial (-)
Refractive index	nα = 1.676 nβ = 1.695 nγ = 1.698
Birefringence	δ = 0.022
Pleochroism	None
2V angle	Measured: 44°
Dispersion	r>v, weak
Ultraviolet fluorescence	Not fluorescent
References	[1][2][3]

Maricite or marićite is a sodium iron phosphate mineral (NaFe²⁺PO₄), that has two metal cations connected to a phosphate tetrahedron. It is structurally similar to the much more common mineral olivine. Maricite is brittle, usually colorless to gray, and has been found in nodules within shale beds often containing other minerals.

Maricite is most commonly known to be found in the Big Fish River area of the Yukon Territory, Canada, but it has also been found in Eastern Germany, as well as inside of various meteorites around the world. Maricite is named after Luka Maric of Croatia, (1899–1979), the longtime head of the mineralogy and petrography departments at the University of Zagreb.

Maricite is a sodium iron phosphate from the extremely diverse phosphate mineral group. In 1977 maricite was discovered in the Big Fish River area, Yukon Territory, Canada (Fleischer, Chao, and Mandarino, 1979). This is an important geologic location that has provided the discovery of several new phosphate minerals. Maricite is recognized for its possible use in sodium ion battery research as well as its role as a reaction product inside of fossil-fired electrical power generating station boilers which experience corrosion (Bridson, et al., 1997; Ong, et al., 2011).

Composition

Maricite is a member of the phosphate mineral group. Phosphate minerals have one or more metal cations bonded to the phosphate anion PO₄. (Hawthorne, F.C., 1998). In maricite the metals bonded to PO₄ are sodium and iron (Sturman, et al., 1977). The empirical formula for maricite is NaFePO₄ and it has a molar mass of 173.81 g/mol (Yahia, et al., 2008; Tremaine, Xiao, 1999). The general formula for maricite is ABPO₄, (Yahia, et al., 2008). The chemical composition was originally found by Dr. Corlett from the Department of Geological Sciences at Queen’s University, Kingston, Ontario. The formula was determined using electron microprobe analysis, and the resulting formula was found to be, Na 0.91(Fe 0.89 Mn 0.07 Mg 0.03)P 1.02 O 4.00 (Sturman, et al., 1977) when normalized to four oxygen atoms. The weight percentages were determined using six different points on a thin section and averaging the percentages of each oxide in all of the samples. The results in weight percent average of oxides are as follows: Na₂O 16.5%, MgO 0.8%, CaO 0.0%, MnO 3.1%, FeO 37.4%, P₂O₅ 42.5%, with a total of 100.3%. When looking at these results, one may determine that the majority of the oxide weight composition is made of FeO with P₂O₅ making up almost the same weight percentage. There is a significant percentage of the Na₂O oxide and an insignificant percentage of the CaO oxide (~0). It is clear from looking at the oxide content of the mineral that the main components are going to be sodium, iron, phosphorus, and oxygen. The oxide factor may be used to determine the weight percentages of the individual elements as follows, 1 sodium atom totaling ~13% of composition, 1 iron atom totaling ~32% of composition, 1 phosphorus atom totaling ~18% of composition, and 4 oxygen atoms totaling ~37% of composition (Sturman, et al., 1977).

Structure

Maricite is an ionic double metal phosphate, with a space filling capacity of about 70% (Le Page, and Donnay, 1977). The structure of maricite contains a sodium cation enclosed by ten oxygen anions within 10 Å, in an irregular coordination. There is (2+2+2) type distorted tetrahedron around the iron (Bridson, et al., 1997). The Å distances between iron and oxygen are between 2.33-2.93. The phosphate tetrahedron is almost regular, with 2 short bonds and 2 longer bonds (Bridson, et al., 1997). The iron atom has four surrounding oxygen atoms giving it tetrahedral coordination. Half of the oxygen atoms are coordinated with two sodium atoms, two iron atoms, and one phosphorus atom while the other half are coordinated with three sodium atoms, one iron atom and one phosphorus atom (Bridson, et al., 1997). The structure of maricite has been compared to the structure of olivine, (Lee, et al., 2011). The structures of the two minerals are similar because they both contain PO₄ in their atomic make-up (Moreau, et al., 2010). However, the M1 and M2 sites for LiFePO₄ and NaFePO₄ have reverse occupancies making their structures different (Lee, et al., 2011). In olivine, the M1 site holds the alkali metal while the M2 site holds the transition metal, whereas in maricite, the M1 site holds the transition metal and the M2 site holds the alkali metal (Ong, et al., 2011).

Physical properties

Maricite (NaFePO₄), is found in elongated grains up to 15 cm long in the [100] direction. The grains are radial to sub parallel in structure. Maricite is usually colorless to gray, but is sometimes a pale brown color and it has a white streak. It has a vitreous luster due to its low values of refractive indices, α = 1.676 β = 1.695 γ = 1.698, and its opacity is transparent to translucent (Fleisher, et al., 1979). Maricite has no cleavage or pleochroism, and it does not fluoresce in UV light. Maricite has a hardness of 4-4.5 and a density of 3.64. The mineral is brittle, with an uneven splintery fracture. It is a member of the orthorhombic crystal class and the biaxial negative optical class and has a 2V calculation of 43°. The Hermann-Mauguin notation symbol is 2/m 2/m 2/m, and it is in the Pmnb space group. Yvon Le Page and Gabrielle Donnay determined that the cell dimensions are a 6.864(2), b 8.994(2), and c 5.049(1). J. A. Mandarino determined the d-spacings using x-ray powder diffraction and Bragg’s law to be 2.574 at an intensity of 100, 2.729 at an intensity of 90, 2.707 at an intensity of 80, 1.853 at an intensity of 60, 3.705 at an intensity of 40, 2.525 at an intensity of 30, and 1.881 also at an intensity of 30 (Fleisher, et al., 1979; Sturman, et al., 1977).

Geologic occurrence

Maricite was first discovered in the Big Fish River area near the eastern border of the Yukon Territory around Latitude 68° 30’ N and Longitude 136° 30’ W. This area is a kulanite-baricite-peniksite type locality composed mostly of bedded shales and sideritic limestones. Maricite has been found in nodules up to 15 cm long within the shale beds. Some of the nodules contained only one mineral, while others contained several different minerals. Very few of the nodules consisted of only maricite. Most of the samples which contained maricite also had quartz, ludlamite, vivianite, pyrite and/or wolfeite. When samples which appeared to only contain maricite were examined closely in a thin section, there were small inclusions of ludlamite, quartz, and vivianite present along the fractures (Sturman, et al., 1977). The other location which formations of maricite have been found is Saxony, Germany (Thomas, R. and Webster J.D., 2000). Both this location and the Big Fish River Canada location are situated just north of convergent plate boundaries. Both areas consist of mountains and hills which are made of metamorphic and igneous rocks (Thomas, R. and Webster J.D., 2000; Sturman, et al., 1977). Maricite has also been discovered in meteorites found in Eastern Antarctica, Uttar Pradesh, India and Avannaa, Greenland (Johnson, et al., 2001; Kracher, et al., 1977; Partridge, et al., 1990).

History

Maricite was named by Darko Sturman and Joseph Mandarino in honor of Luka Maric. Maric was the longtime head of the department of mineralogy and petrography at the University of Zagreb in Croatia. The name Maricite was approved in 1977 by the commission on new minerals and mineral names. It is unclear exactly why the mineral was named in honor of Maric, but he did author several geology books including one entitled Magmatiti u Uzhem Podruchju Rudnika Bor u Istochnoj Srbiji, which is Croatian for Magmatites in the Narrower Ore Deposit Region of the Bor Mine (Sturman, et al., 1977).

See also

• Lithium iron phosphate

References

• Bridson, J. Quinlan, S.E. and Tremaine, P.R. (1998). Synthesis and crystal structure of maricite and sodium iron (111) hydroxyphosphate. Chem mater.Volume 10. Pages 763-768.
• Fleischer, M., Chao, G.Y. and Mandarino, J.A. (1979). New mineral names. American Mineralogist.Volume 64. Pages 652-659.
• Hawthorne, F.C. (1998). Structure and chemistry of phosphate minerals. Mineralogical Magazine. Volume 62. Pages 141-164.
• Johnson, C.L., D.S. Lauretta, and P.R. Buseck, A High-resolution Transmission Electron Microscopy Study of Fine-Grained Phosphates in Metal From the Bishunpur LL3.1 Ordinary Chondrite, 63rd Annual Meteoritical Society Meeting (5303.pdf)
• Lauretta, Dante S., Peter R. Buseck, and Thomas J. Zega (2001) Opaque minerals in the matrix of the Bishunpur (LL3.1) chondrite: constraints on the chondrule formation environment. Geochimica et Cosmochimica Acta: 65(8) (15 April 2001): 1337-1353.
• Kracher, Kurat, A.G. and Buchwald, V.F. (1977). Cape York: the extraordinary mineralogy of an ordinary iron meteorite and its implications for the genesis of III AB irons. Geochemical Journal. Volume 11. Pages 207-217.
• Lee, T.K., Ramesh, T.N., Nan, F., Botton, G. and Nazur, L.F. (2011). Topochemical synthesis of sodium metal phosphate olivines for sodium-ion batteries. Chem mater.Volume 23. Pages 3593-3600.
• Le Page, Y. and Donnay, G. (1977). The crystal structure of the new mineral maricite, NaFePO4. The Canadian Mineralogist. Volume 15. Pages 518-521.
• Moreau, P., Guyomard, D. and Boucher, F. (2010). Structure and stability of sodium intercalculated phases in olivine FePO4. Chem Mater.Volume 22. Pages 4126-4128.
• Ong, S.P., Chevrier, V.L., Hautier G., Jain A., Moore, C., Kim, S., Ma, X. and Cedar, G. (2011). Voltage, stability and diffusion barrier differences between sodium-ion and lithium ion intercalculation materials. Energy and Environmental Science. Volume 4. Pages 3680-3688.
• Sturman, B.D., Mandarino, J.A. and Corlett, M.I. (1977). Maricite, a sodium iron phosphate, from the Big Fish River area, Yukon Territory, Canada. The Canadian Mineralogist.Volume 15. Page 396.
• Thomas, R. and Webster J.D. (2000). Strong tin enrichment in a pegmatite-forming melt. Mineralium Deposita. Volume 35. Pages 570-582.
• Tremaine, P.R. and Xiao Caibin. (1999). Enthalpies of formation and heat capacity functions for maricite, NaFePO4(cr), and sodium iron (I I I ) hydroxyphosphate, Na3Fe(PO4)2.(Na4/3O)(cr). Journal of Chemical Thermodynamics. Volume 31. Pages 1307-1320.
• Partridge, T., Reimold, W.U. and Walraven, F. (1990). The Pretoria Zoutpan Crater: First results from the 1988 drilling project. Meteoritics. Volume 25. Page 396-398.
• Yahia, B.H., Gaudin, E. and Darriet, J. (2008). Synthesis, structures and magnetic properties of the new vandates AgMnVO4 and RbMnVO4. Journal of Solid State Chemistry. Volume 181. Pages 3103-3109.

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