2023 Annual Meeting of Japan Association of Mineralogical Sciences (JAMS)

Presentation information

Oral presentation

R2: Crystal structure, crystal chemistry, physical properties of minerals, crystal growth and applied mineralogy

Fri. Sep 15, 2023 9:00 AM - 12:00 PM 820 (Sugimoto Campus)

Chairperson:Kazuki 小松 Komatsu, Ryo Yamane(Tohoku Univ.), Mariko Nagashima

9:45 AM - 10:00 AM

[R2-04] Structural variability and stability of FBUs in borate minerals

Nishiyasu Wataru1, *Atsushi KYONO1 (1. University of Tsukuba)

Keywords:Borate minerals, Borax, Structural variability, Fundamental Building Units, Quantum chemical calculation

As increasing temperature, tincalconite Na2B4O5(OH)4·3H2O appeared at 30oC as a dehydrated phase and decomposed at 160oC. Subsequently, gamma-Na2B4O7 crystallized as an anhydrous phase at 600oC and changed to alpha-Na2B4O7 at 650oC. The FBU of borax consists of two three-membered rings, each of which is composed of a BO3 triangle and two BO4 tetrahedra. Tincalconite has the same FBU as borax. On the other hand, the FBU of gamma-Na2B4O7 consists of a three-membered ring consisting of one BO3 triangle and two BO4 tetrahedra and two BO3 triangles and one BO4 tetrahedra sharing a BO4 tetrahedron. Alpha-Na2B4O7 is composed of two types of FBUs: one is the same as gamma-Na2B4O7 and another is a three-membered ring consisting of two BO3 triangles and one BO4 tetrahedron. Therefore, the dehydrated and anhydrous phases appearing during the thermal decomposition are characterized by the fact that a three-membered ring consisting of one BO3 triangle and two BO4 tetrahedra is common to the borax FBUs. The total energies of the FBUs of representative borate minerals are compared. The most widely occurring borate minerals are borax, colemanite, ulexite, and kernite. The FBU of colemanite is a three-membered ring consisting of one BO3 triangle and two BO4 tetrahedra. The FBUs of ulexite and kernite also contain a three-membered ring consisting of one BO3 triangle and two BO4 tetrahedra. The FBUs of borax, colemanite, ulexite, and kernite have a common ring, and the total energy of each is relatively lower among borate minerals. Therefore, the structural stability of the FBUs is almost consistent with the frequency of occurrence of borate minerals. The frequency of occurrence of three-membered rings is determined by Burns et al. (1995), which is in good agreement with the results of quantum chemical calculations. The total energies of the FBUs of alpha-Na2B4O7 and gamma-Na2B4O7 were clearly higher than those of borax. This may support the fact that the anhydrous Na2B4O7 phase has five polymorphs and easily changes the FBU geometry without requiring large amounts of energy.