Ulexite

Ulexite has been recognized as a valid mineral since 1840, after George Ludwig Ulex, for whom the mineral was named, provided the first chemical analysis of the mineral. In a footnote on p. 51, the editor claimed that Ulex's mineral actually was the same mineral that the American chemist Augustus Allen Hayes had found in Chile in 1844: In 1857, Henry How, a professor at King's College in Windsor, Nova Scotia, discovered borate minerals in the gypsum deposits of the Lower Carboniferous evaporate deposits in the Atlantic Provinces of Canada where he noted the presence of a fibrous borate that he termed natro-boro-calcite, which was actually ulexite (Papezik and Fong, 1975). In 1963 ulexite's remarkable fiber optics qualities were explained by Weichel-Moore and Potter. == Chemistry ==

Ulexite is a borate mineral because its formula (NaCaB5O6(OH)6·5H2O) contains boron and oxygen. The isolated borate polyanion [B5O6(OH)6]3− has five boron atoms, therefore placing ulexite in the pentaborate group. Ulexite is a structurally complex mineral, with a basic structure containing chains of sodium, water and hydroxide octahedra. The chains are linked together by calcium, water, hydroxide and oxygen polyhedra and massive boron units. The boron units have a formula of [B5O6(OH)6]3– and a charge of −3. They are composed of three borate tetrahedra and two borate triangular groups. Ulexite decomposes/dissolves in hot water. == Morphology ==

Ulexite commonly forms small, rounded masses resembling cotton balls. Crystals are rare but will form fibrous, elongated crystals either oriented parallel or radial to each other. Crystals may also be acicular, resembling needles (Anthony et al., 2005). The point group of ulexite is 1, which means that the crystals show very little symmetry as there are no rotational axes or mirror planes. Ulexite is greatly elongated along [001]. The most common twinning plane is (010). Ulexite collected from the Flat Bay gypsum quarry in Newfoundland exhibits acicular "cotton balls" of crystals with a nearly square cross-section formed by the equal development of two pinacoids. The crystals are about 1–3 μm thick and 50–80 μm long, arranged in loosely packed, randomly oriented overlapping bundles (Papezik and Fong, 1975). In general, the crystals have six to eight faces with three to six terminal faces (Murdoch, 1940). == Optical properties ==

In 1956, John Marmon observed that fibrous aggregates of ulexite project an image of an object on the opposite surface of the mineral. This optical property is common for synthetic fibers, but not in minerals, giving ulexite the nickname "TV rock". According to Baur et al. (1957), this optical property is due to the reflections along twinned fibers, the most prominent twinning plane being on (010). The light is internally reflected over and over within each of the fibers that are surrounded by a medium of a lower refractive index (Garlick, 1991). This optical effect is also the result of the large spaces formed by the sodium octahedral chains in the mineral structure. Synthetic fibers used for fiber optics transmit images along a bundle of threadlike crystals the same way naturally occurring ulexite reproduces images due to the existence of different indices of refractions between fibers. Additionally, if the object is colored, all of the colors are reproduced by ulexite. Parallel surfaces of ulexite cut perpendicular to the fibers produce the best image, as distortion in the size of the projected image will occur if the surface is not parallel to the mineral. Curiously, in situ samples of ulexite are capable of producing a decent, rough image. Satin spar gypsum also exhibits this optical effect; however, the fibers are too coarse to transmit a decent image. The thickness of the fibers is proportional to the sharpness of the projected image. the orientation of the fibers around the c-axis is completely random based on the variations in extinctions viewed under cross polarization. Ulexite displays polysynthetic twinning parallel to the elongation, along {010} and {100} (Murdoch, 1940). In thin sections cut parallel to the fibers, ulexite grains display both length-fast and length-slow orientations in equal quantities because the intermediate axis (y) of the indicatrix is roughly parallel to the elongation of the fibers along the crystallographic c-axis (Weichel-Moore and Potter, 1963). == Structure ==

Ulexite crystals contain three structural groups, isolated pentaborate polyanions, calcium coordinated polyhedra, and sodium coordinated octahedra that are joined together and cross-linked by hydrogen bonding. The Ca-coordination polyhedra share edges to form chains which are separate from the Na-coordination octahedral chains. There are 16 distinct hydrogen bonds that have an average distance of 2.84 Å. Boron is coordinated to four oxygens in a tetrahedra arrangement and also to three oxygens in a triangular arrangement with average distances of 1.48 and 1.37 Å, respectively. Each Ca2+ cation is surrounded by a polyhedron of eight oxygen atoms. The average distance between calcium and oxygen is 2.48 Å. Each Na+ is coordinated by an octahedron of two hydroxyl oxygens and four water molecules, with an average distance of 2.42 Å (Clark and Appleman 1964). The octahedral and polyhedral chains parallel to c, the elongate direction, cause the fibrous habit of ulexite and the fiber optical properties. == Significance ==

Boron is a trace element within the lithosphere that has an average concentration of 10 ppm, although large areas of the world are boron deficient. Boron is never found in the elemental state in nature, however boron naturally occurs in over 150 minerals. High concentrations of economically significant boron minerals generally occur in arid areas that have a history of volcanism. Ulexite is mined predominantly from the Borax mine in Boron, California. Recently, as more attention is being given to obtaining new sources of energy, the use of hydrogen as a fuel for cars has come to the forefront. The compound sodium borohydride (NaBH4) is currently being considered as an excellent hydrogen storage medium due to its high theoretical hydrogen yield by weight for future use in cars. Piskin (2009) validates that the boron concentration in ulexite can be used as the boron source or the starting material in the synthesis of sodium borohydride (NaBH4). == Related minerals ==

Borate minerals are rare because their main component, boron, makes up less than 10 ppm (10 mg/kg) of Earth's crust. Because boron is a trace element, the majority of borate minerals occur only in one specific geologic environment: geologically active intermontane basins. Borates are formed when boron bearing solutions, caused from the leaching of pyroclastic rocks, flow into isolated basins where evaporation then takes place. Over time, borates deposit and form into stratified layers. Ulexite occurs in salt playas and dry saline lakes in association with large-scale gypsum deposits and Na-Ca borates. There are no known polymorphs of ulexite nor does ulexite form a solid solution series with any other minerals. According to Stamatakis et al. (2009) Na, Ca, and Na-Ca borates are found in relation to ulexite. These minerals are: • Borax Na2B4O7·10H2O • Colemanite Ca2B8O11·5H2O • Howlite Ca2B5SiO9[OH]5 • Kernite Na2[B4O6(OH)2·3H2O] • Meyerhofferite Ca2B6O6(OH)10·2H2O • Probertite NaCaB5O9·5H2O More common minerals that are not borates, but also form in evaporite deposits are: • Calcite CaCO3 • Gypsum CaSO4·2H2O • Halite NaCl == See also ==