Laboratory experiments in which calcium borate minerals were precipitated by water evaporation from aqueous boron and calcium ion-bearing solutions were carried out at 25 ℃ and boron isotope fractionation accompanying the mineral formation was studied. Nobleite and gowerite were obtained as calcium borate minerals, and isotopic analysis was carried out on nobleite. The
11B/
10B isotopic ratio of the mineral was smaller than that of the solution, which meant that the heavier isotope
11B was preferentially fractionated into the solution phase. The boron isotopic data of nobleite were sufficiently harmonized with those of borax (sodium borate mineral) and K
2[B
4O
5(OH)
4]·2H
2O (potassium borate mineral). The three minerals have the same BO
3/BO
4 ratio, the ratio of the number of the BO
3 triangle units to the number of the BO
4 tetrahedron units in the polyborate anion of the structural formula of the mineral. The present study thus reconfirmed and extended the claim that the boron isotope fractionation strongly depends on the BO
3/BO
4 ratio and is nearly independent of the counter cation.
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