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Solubility and speciation of iron in hydrothermal fluids

机译:热液流体中铁的溶解度和形态

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摘要

Iron is among the most abundant elements in Earth's crust and is also a major aqueous solute in a variety of hydrothermal settings, yet major questions remain regarding the solubility and speciation of iron at hydrothermal conditions. Here, we conducted hydrothermal diamond-anvil cell experiments using synchrotron-radiation micro-XRF and XANES analyses as well as Raman spectroscopy, in situ at hydrothermal temperatures and pressures, to characterize the solubility and speciation of iron in fluids buffered by a variety of mineral assemblages. Our experiments included the assemblages hematite-magnetite (HM), fayalite-magnetite-quartz (FMQ), and magnetite-pyrite-pyrrhotite (MPP). Our results indicate highest solubilities of HM in HCl solutions. In sodium chloride solutions of similar molalities, FMQ shows higher Fe solubility than MPP. XANES data are interpreted as preponderance of ferrous iron in all experiments. Comparison of XANES spectra of these solutions with calculated XANES spectra from the literature indicates octahedral FeClx(H2O)(6-x)(2-x) (x = 0-3) as predominant Fe(II) species at lower Cl-Fe ratios, and suggests additional tetrahedral FeCl42- or FeCl3(H2O)(-) at high Cl-Fe ratios. Raman spectra to 600 degrees C show that the predominant species in ferric iron solutions is FeCl2(H2O)(4)(+) at temperatures less than 100 degrees C, which transitions to FeCl4- between 100 and 200 degrees C. An additional Raman band that occurred in some spectra of a H2O + HCl fluid equilibrated with hematite +/- magnetite at temperatures greater than 300 degrees C may originate from an FeCl3(H2O)(x) (x = 0-3) species. All Raman spectra of ferrous iron solutions show a fairly broad band at about 280 cm(-1), which can be interpreted to stem from Fe(II)-Cl vibrations of FeCl3(H2O)(x)(-) (x = 0-3) (point group D-3h) species or, at low Cl-Fe ratios of about two or less, from octahedral FeClx(H2O)(6-x)(2-x) (x = 0-3) species. These results provide important constraints on the hydrot
机译:铁是地壳中最丰富的元素之一,也是各种水热环境中的主要水溶液,但仍然是铁在水热条件下铁的溶解度和形态的主要问题。在这里,我们使用同步辐射微XRF和XANES分析以及在水热温度和压力下原位的拉曼光谱进行水热金刚石 - 砧座实验,以表征由各种矿物缓冲的液体中的铁的溶解度和形态装配。我们的实验包括组合赤铁矿 - 磁铁矿(HM),Fayalite - 磁铁矿 - 石英(FMQ)和磁铁矿 - 吡啶矾 - PyrrHotite(MPP)。我们的结果表明了HM在HCl溶液中HM的最佳溶解度。在相似麦芽酸钠的氯化钠溶液中,FMQ显示比MPP更高的Fe溶解度。 Xanes数据被解释为所有实验中的铁铁优势。从文献中计算出这些溶液的XANES光谱比较来自文献的XANES光谱表明八面体FECLX(H2O)(6-x)(2-x)(x = 0-3),作为较低CL-FE比的主要FE(II)物种,并在高Cl-Fe比率下提出额外的四面体FECL42-或FECL3(H2O)( - )。拉曼光谱至600摄氏度表明,在少于100摄氏度的温度下,铁溶液中的主要物种是FECL2(H2O)(4)(+),其转变为100到200摄氏度之间的FECL4-额外的拉曼带在大于300摄氏度的温度下与赤铁矿+/-磁铁平平衡的H 2 O + HCl液的一些光谱中发生的可以源自FECL3(H2O)(X)(X = 0-3)种。亚铁溶液的所有拉曼光谱显示出约280cm(-1)的相当宽带,可解释为源于FECL3(H2O)(x)( - )的振动(x = 0 -3)(点组D-3H)物种,或者在低Cl-Fe率,约两于两个或多个,从八面体FeClx(H 2 O)(6-x)(2-x)(x = 0-3)种。这些结果为水滴提供了重要的限制

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