Japan Geoscience Union Meeting 2014

Presentation information

Oral

Symbol U (Union) » Union

[U-05_30AM2] Interrelation between Life, Water, Mineral, and Atmosphere

Wed. Apr 30, 2014 11:00 AM - 12:45 PM 419 (4F)

Convener:*Tsubasa Otake(Division of Sustainable Resources Engineering, Faculty of Engineering, Hokkaido University), Yohey Suzuki(Graduate School of Science, The University of Tokyo), Fumito Shiraishi(Department of Earth and Planetary Systems Science, Graduate School of Science, Hiroshima University), Ken Takai(Extremobiosphere Research Center, Japan Agency for Marine-Earth Science & Technology), Yuichiro Ueno(Department of Earth and Planetary Sciences, Tokyo Institute of Technology), Takeshi Naganuma(Graduate School of Biosphere Science), Takeshi Kakegawa(Graduate School of Science, Tohoku University), Tadashi Yokoyama(Department of Earth and Space Science, Graduate School of Science, Osaka University), Kentaro Nakamura(Precambrian Ecosystem Laboratory (PEL), Japan Agency for Marine-Earth Science and Technology (JAMSTEC)), Chair:Tadashi Yokoyama(Department of Earth and Space Science, Graduate School of Science, Osaka University), Kentaro Nakamura(Precambrian Ecosystem Laboratory (PEL), Japan Agency for Marine-Earth Science and Technology (JAMSTEC))

12:15 PM - 12:30 PM

[U05-10] Effects on Phosphate Ion for the Phase Changes of Amorphous Calcium Carbonate

*Yuki SUGIURA1, Kazuo ONUMA2, Astushi YAMAZAKI1 (1.Department of Creative Science and Technology, Waseda University, 2.National Institute of Advanced Industrial Science and Technology, Central 6)

Keywords:Amorphous, Calcium carbonate, Phosphate, Phase transformation, Biomineralization

Under the biometric simulated environment, amorphous calcium carbonate (ACC) appears as initiation phase by reaction of calcium and carbonate ions. There is a strong relationship between the ACC phase and the forming crystalline polymorphs. We have shown a significant inhibit effect on the vaterite formation and calcite crystallized instead, and also stabilize ACC under higher PO4 concentration conditions. We hypothesized that PO4 ions incorporated in the ACC in that suspect that the adjusting the transfer mechanism of the amorphous phase. The structure and stability of ACC under various PO4 concentrations were examined using in situ ultra violet/visible spectroscopy (UV/Vis). Further, in order to observe in detail the coupling state, the ex situ measurement of ACC by Raman spectroscopy and by using a Ca ion electrode were performed to evaluation of the presence time of the ACC phase. The bicarbonate buffer was mixed with supersaturated solution of calcium chloride and sodium bicarbonate solution to precipitate the ACC, under conditions of pH ~ 8.6. By mixing the potassium hydrogen phosphate at a concentration of any carbonate solution side during mixing, PO4 ions was adjusted between 0-50μM concentrations. The ACC contains no PO4 ions shows a spectrum similar to calcite. However the concentration of PO4 ions increase, UV / Vis absorption spectrum was carried out changed to spectrum like vaterite gradually. The similar behavior showed in the spectrum observed by Raman spectroscopy. By results of measurements of the molecular weight and particle size of the ACC by scattered light spectroscopy, the increasing both density and particle size of ACC was obsereved. Ion electrode measurements showed that the residence time of the ACC increased exponentially as increasing PO4 concentration. In the presence of PO4 ion, ACC showed a structure similar to vaterite and its stability was increased. Moreover, the type of forming polymorphs greatly changes in variation of PO4 ions in μM scale, and stability amorphous structure is also highly variable. The results suggest a need to consider the effects of coexisting PO4 ions on ACC, when calcium carbonate tissue is formed in the organism.