Jonesite | |
Category: | Inosilicates |
Formula: | Ba4(K,Na)2[Ti<sub>4</sub>Al<sub>2</sub>Si<sub>10</sub>O<sub>36</sub>]•6H2O |
Imasymbol: | Jon[1] |
Molweight: | 914.93 g/mol |
System: | Monoclinic |
Class: | Prismatic (2/m) (same H-M symbol) |
Symmetry: | P21/m |
Unit Cell: | a = 10.618, b = 25.918 c = 8.6945 [Å]; β = 127.633°; Z = 4 |
Color: | Colorless |
Habit: | Bladed– Aggregation is thin blade-like crystals and Tabular– Dimensions thin in one direction |
Cleavage: | Distinct |
Fracture: | Irregular |
Mohs: | 3–4 |
Luster: | Vitreous |
Refractive: | Index: 1.64 to 1.68 |
Opticalprop: | Biaxial (+), a=1.641, b=1.66, g=1.682, bire=0.0410 |
Birefringence: | δ = 0.041 |
Pleochroism: | Colorless |
Streak: | White |
Gravity: | 3.21 g/cm3 |
Density: | 3.25 g/cm3 |
Diaphaneity: | Transparent |
Other: | Has medium relief and weak dispersion. Has fluorescent luminescence & white streakYear of Discovery:1977 |
References: | [2] [3] [4] |
Jonesite is a mineral with the chemical formula Ba4(K,Na)2[Ti<sub>4</sub>Al<sub>2</sub>Si<sub>10</sub>O<sub>36</sub>]*6H2O.[5] This mineral is named after Francis Tucker Jones (1905–1993), who discovered the mineral while working as a Research Chemical Microscopist at Berkeley in CA.[6] Jonesite has diffraction symmetry of mmm, which implies an orthorhombic system with all three axes perpendicular to each other and the angles between each axis equal to 90 degrees.[7] In addition to symmetrical properties, Jonesite is a biaxial mineral with birefringence, which is a term to describe the difference between index of refraction.[8] Jonesite is anisotropic, meaning the speed of light changes through the mineral, so the mineral shows color when viewed in crossed polarized light under a microscope. The mineral also has medium relief, which is a measure of how well the mineral stands out when viewed under a microscope in plane polarized light.[9] In addition to being one of the rarest minerals in the Benitoite Gem mine located in California, Jonesite also is the first titanosilicate mineral with a porous double-layered crystal structure.[10] This discovery is important because titanosilicate frameworks have industrial uses in energy companies and are used in containing radioactive waste.[11]