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Stable solid and aqueous H2CO3 from CO2 and H2O at high pressure and high temperature

机译:在高压和高温下由CO2和H2O稳定形成的固体和含水H2CO3

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摘要

Carbonic acid (H2CO3) forms in small amounts when CO2 dissolves in H2O, yet decomposes rapidly under ambient conditions of temperature and pressure. Despite its fleeting existence, H2CO3 plays an important role in the global carbon cycle and in biological carbonate-containing systems. The short lifetime in water and presumed low concentration under all terrestrial conditions has stifled study of this fundamental species. Here, we have examined CO2/H2O mixtures under conditions of high pressure and high temperature to explore the potential for reaction to H2CO3 inside celestial bodies. We present a novel method to prepare solid H2CO3 by heating CO2/H2O mixtures at high pressure with a CO2 laser. Furthermore, we found that, contrary to present understanding, neutral H2CO3 is a significant component in aqueous CO2 solutions above 2.4 GPa and 110 °C as identified by IR-absorption and Raman spectroscopy. This is highly significant for speciation of deep C–O–H fluids with potential consequences for fluid-carbonate-bearing rock interactions. As conditions inside subduction zones on Earth appear to be most favorable for production of aqueous H2CO3, a role in subduction related phenomena is inferred.
机译:当CO2溶解在H2O中时,会形成少量的碳酸(H2CO3),但在环境温度和压力下会迅速分解。尽管存在短暂,但H2CO3在全球碳循环和含生物碳酸盐的系统中仍发挥着重要作用。在水中的短寿命和在所有陆地条件下的低浓度假定都扼杀了该基本物种的研究。在这里,我们研究了在高压和高温条件下的CO2 / H2O混合物,以探索天体内部与H2CO3反应的潜力。我们提出了一种通过使用CO2激光器在高压下加热CO2 / H2O混合物来制备固体H2CO3的新方法。此外,我们发现,与目前的理解相反,中性H2CO 3 是在2.4 GPa和110 C以上的CO 2 水溶液中的重要成分,通过IR吸收鉴定和拉曼光谱。这对于深层C–O–H流体的形态形成非常重要,对含碳酸盐的岩石相互作用具有潜在的影响。由于地球上的俯冲带内部的条件似乎最适于产生H 2 CO 3 水溶液,因此推测了与俯冲有关的现象中的作用。

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