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Calcium isotopic fractionation during travertine deposition under different hydrodynamic conditions: Examples from Baishuitai (Yunnan, SW China)

机译:在不同水动力条件下钙华沉积过程中的钙同位素分馏:来自白水台的实例(中国云南省云南省)

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Revealing the potential of Ca isotopes in the research of travertine formation processes is the principal goal of this sludy. To achieve this, the hydrochemistry, travertine precipitation rales, and variations in Ca isolopic compositions (delta Ca-44/40) of present-day endogenic (Lhermogenic) travertine in two differem hydrodynamic systems (canal and pool) are studied at Baishuilai (Yunnan, SW China). In the canal, where the travertine precipitation is faster, delta(44/40) Ca values of both solution and travertine show a downstream increase, with Ca2+ isotopic fractionation (Delta(44/40) CaCaCo3-aq) equal to similar to-1.6 parts per thousand. Compared to the canal, Ca isotopic fractionation between travertine and aqueous Cat is smaller (Delta Ca-44/40(CaCO3-aq) approximate to -1 2 parts per thousand) in the pools where travertine precipitation rates are lower.The spatial variations in delta Ca-44/40 values of solution and travertine are related to the amount of Ca removed from the solution when delta Ca-44/40 values of spring water remain stable. In addition, the results confirm the control of precipitation rates on Ca isotopic fractionation between calcite and parent aqueous Ca2+ using natural samples. The observed negative correlation between Delta Ca-44/40(CaCO3-aq) and travertine precipitation rates can be explained by the steady-state kinetic surface reaction model proposed by DePaolo (2011), with equilibrium and kinetic fractionation factors of alpha(eq) = 1.0000 +/- 0.0001 and alpha(f) = 0.9983 +/- 0.0002, respectively. An important consequence of this study is that Ca isotopes in travertine systems are good tools to have access to variations of delta Ca-44/40(aq) which are directly linked to the amount of precipitated Ca. This could then be useful for reconstructing past hydrodynamic conditions when applied to travertine core data. (C) 2016 Elsevier B.V. All rights reserved.
机译:揭示钙同位素在钙华形成过程研究中的潜力是该研究的主要目标。为实现这一目标,在云南白水来研究了两种内在水动力系统(运河和水池)中当今内生(生热)钙华的水化学,钙华的降水规律以及Ca同位素组成(δCa-44 / 40)的变化。 ,西南中国)。在钙华沉积较快的运河中,溶液和钙华的δ(44/40)Ca值均显示下游增加,Ca2 +同位素分馏(δ(44/40)CaCaCo3-aq)等于-1.6千分之几。与钙通道相比,在钙华沉积速率较低的池中,钙华和Cat水溶液之间的Ca同位素分馏较小(Delta Ca-44 / 40(CaCO3-aq)约-1 2千分之一)。当温泉水的δCa-44 / 40值保持稳定时,溶液和钙华的δCa-44 / 40值与从溶液中去除的Ca量有关。此外,结果证实使用天然样品可控制方解石与母体Ca2 +水溶液之间Ca同位素分馏的沉淀速率。观测到的Delta Ca-44 / 40(CaCO3-aq)与钙华沉积速率之间的负相关关系可以通过DePaolo(2011)提出的稳态动力学表面反应模型加以解释,其中平衡和动力学分级因子为alpha(eq) = 1.0000 +/- 0.0001和alpha(f)= 0.9983 +/- 0.0002。这项研究的重要结果是,钙华系统中的Ca同位素是获得δCa-44 / 40(aq)变化的良好工具,这些变化与沉淀的Ca的含量直接相关。当应用于石灰华岩心数据时,这对于重建过去的水动力条件可能很有用。 (C)2016 Elsevier B.V.保留所有权利。

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