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首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Boron speciation in aqueous fluids at 22 to 600 degrees C and 0.1 MPa to 2 GPa
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Boron speciation in aqueous fluids at 22 to 600 degrees C and 0.1 MPa to 2 GPa

机译:在22至600摄氏度和0.1 MPa至2 GPa的水性流体中的硼形态

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The speciation of boron in H2O + H3BO3 +/- NaCl and H2O + Na2B4O7 fluids was studied in situ at temperatures between 22 and 600degreesC and pressures from 0.1 MPa to similar to2 GPa using Raman spectroscopy and a hydrothermal diamond anvil cell. Additionally, we determined the frequency shifts of the 877 cm(-1) Raman line of [B(OH)(3)](0) in aqueous fluids with temperature (partial derivativev(877)/partial derivativeT)(p) = (0.1 MPa) = -0.02532 cm(-1) K-1 and pressure (partial derivativev(877)/partial derivativeP)(T) = (22degreesC) = 4.06 cm(-1) GPa(-1). The observed species in acidic fluids were [B(OH)(3)](0) and smaller amounts of a four-coordinated boron species which may be attributed to dissolved metaboric acid HBO2(aq). The ratio of this B-[4]-O species to [B(OH)(3)](0) increases with temperature and decreases slightly with addition of NaCl. In alkaline solutions, polyboric ions depolymerize rapidly with temperature. Thus, [B(OH)(3)](0) and [B(OH)(4)](-) were the only remaining detectable species at 500 and 600degreesC. The Raman spectra showed an increase of [B(OH)(3)](0) relative to [B(OH)(4)](-) with temperature and an increase of [B(OH)(4)](-) relative to [B(OH)(3)](0) with pressure.The general trend in the boron speciation is a higher stability of simpler complexes with temperature. The experimental observations strongly indicate that planar three-coordinated [B(OH)(3)](0) is the predominant boron species in the aqueous phase over a wide range of P-T-pH conditions. This supports the validity of previous assumptions on boron coordination in crustal and mantle wedge fluids. Copyright (C) 2005 Elsevier Ltd.
机译:使用拉曼光谱法和水热金刚石砧盒,在22至600摄氏度之间的温度,压力从0.1 MPa到接近2 GPa的压力下,对H2O + H3BO3 +/- NaCl和H2O + Na2B4O7流体中硼的形态进行了研究。此外,我们确定了[B(OH)(3)](0)在温度为(偏导数v(877)/偏导数T)(p)=( 0.1 MPa)= -0.02532 cm(-1)K-1和压力(偏导数v(877)/偏导数P)(T)=(22摄氏度)= 4.06 cm(-1)GPa(-1)。在酸性流体中观察到的物种为[B(OH)(3)](0)和少量的四配位硼物种,这可能归因于溶解的偏硼酸HBO2(aq)。该B- [4] -O物种与[B(OH)(3)](0)的比率随温度增加而随NaCl的添加而略有减少。在碱性溶液中,多硼离子会随着温度迅速解聚。因此,[B(OH)(3)](0)和[B(OH)(4)](-)是在500和600摄氏度下仅有的剩余可检测物质。拉曼光谱显示[B(OH)(3)](0)相对于[B(OH)(4)](-)随着温度的升高而增加[B(OH)(4)](- )相对于[B(OH)(3)](0)在压力下的作用。实验观察结果强烈表明,在很宽的P-T-pH条件下,平面三配位[B(OH)(3)](0)是水相中的主要硼物种。这支持了先前关于地壳和地幔楔流体中硼配位的假设的有效性。版权所有(C)2005 Elsevier Ltd.

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