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An unusual isotopic fractionation of boron in synthetic calcium carbonate precipitated from seawater and saline water

机译:海水和盐水中沉淀的合成碳酸钙中硼的同位素分馏异常

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Inorganic calcium carbonate precipitation from natural seawater and saline water at various pH values was carried out experimentally. The results show the clear positive relationships between boron concentration and δ~(11)B of inorganic calcium carbonate with the pH of natural seawater and saline water. However, the variations of boron isotopic fractionation between inorganic calcite and seawater/saline water with pH are inconsistent with the hypothesis that B(OH)_4~- is the dominant species incorporated into the biogenic calcite structure. The isotopic fractionation factors a between synthetic calcium carbonate precipitate and parent solutions increase systematically as pH increases, from 0.9884 at pH 7.60 to 1.0072 at pH 8.60 for seawater and from 0.9826 at pH 7.60 to 1.0178 at pH 8.75 for saline water. An unusual boron isotopic fractionation factor of larger than 1 in synthetic calcium carbonate precipitated from seawater/saline water at higher pH is observed, which implies that a substantial amount of the isotopically heavier B(OH)_3 species must be incorporated preferentially into synthetic inorganic carbonate. The results propose that the incorporation of B(OH)_3 is attributed to the formation of Mg(OH)_2 at higher pH of calcifying microenvironment during the synthetic calcium carbonate precipitation. The preliminary experiment of Mg(OH)_2 precipitated from artificial seawater shows that heavier ~(11)B is enriched in Mg(OH)_2 precipitation, which suggests that isotopically heavier B(OH)_3 species incorporated preferentially into Mg(OH)_2 precipitation. This result cannot be applied to explain the boron isotopic fractionation of marine bio-carbonate because of the possibility that the unusual environment in this study appears in formation of marine bio-carbonate is infinitesimal. We, however, must pay more attention to this phenomenon observed in this study, which accidentally appears in especially natural environment.
机译:实验从各种pH值的天然海水和盐水中沉淀出无机碳酸钙。结果表明,硼的浓度与无机碳酸钙的δ〜(11)B与天然海水和盐水的pH值具有明显的正相关关系。然而,无机方解石与海水/盐水之间的硼同位素分馏随pH值的变化与B(OH)_4-是生物成方解石结构中占主导地位的物种这一假说不一致。合成碳酸钙沉淀物和母液之间的同位素分馏因子α随着pH的增加而系统地增加,海水从pH 7.60的0.9884增加到pH 8.60的1.0072,从pH 7.60的0.9826增加到pH 8.75的pH178上的1.0178。观察到在较高pH值下从海水/盐水中沉淀的合成碳酸钙中硼的同位素分馏系数大于1的异常,这意味着必须优先将大量同位素较重的B(OH)_3物种优先掺入合成无机碳酸盐中。结果表明,B(OH)_3的掺入归因于在合成碳酸钙沉淀过程中,在较高的钙化微环境pH下,Mg(OH)_2的形成。人造海水中沉淀的Mg(OH)_2的初步实验表明,〜(11)B富含Mg(OH)_2沉淀,这表明同位素较重的B(OH)_3物种优先掺入Mg(OH)_2沉淀。该结果不能用于解释海洋生物碳酸盐的硼同位素分馏,因为该研究中海洋生物碳酸盐形成中异常环境的可能性极小。但是,我们必须更加注意在本研究中观察到的这种现象,这种现象在自然环境中尤其偶然出现。

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