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高温水介质中有机合成的证据——事实与展望。

Evidence for organic synthesis in high temperature aqueous media--facts and prognosis.

作者信息

Simoneit B R

机构信息

College of Oceanic and Atmospheric Sciences, Oregon State University, Corvallis 97331, USA.

出版信息

Orig Life Evol Biosph. 1995 Jun;25(1-3):119-40. doi: 10.1007/BF01581578.

Abstract

Hydrothermal systems are common along the active tectonic areas of the earth. Potential sites being studied for organic matter alteration and possible organic synthesis are spreading ridges, off-axis systems, back-arc activity, hot spots, volcanism, and subduction. Organic matter alteration, primarily reductive and generally from immature organic detritus, occurs in these high temperature and rapid fluid flow hydrothermal regimes. Hot circulating water (temperature range - warm to >400 degrees C) is responsible for these molecular alterations, expulsion and migration. Compounds that are obviously synthesized are minor components because they are generally masked by the pyrolysis products formed from contemporary natural organic precursors. Heterocyclic sulfur compounds have been identified in high temperature zones and hydrothermal petroleums of the Guaymas Basin vent systems. They can be interpreted as being synthesized from formaldehyde and sulfur or HS kappa- in the hydrothermal fluids. Other products from potential synthesis reactions have not yet been found in the natural systems but are expected based on known industrial processes and inferences from experimental simulation data. Various industrial processes have been reviewed and are of relevance to hydrothermal synthesis of organic compounds. The reactivity of organic compounds in hot water (200-350 degrees C) has been studied in autoclaves, and supercritical water as a medium for chemistry has also been evaluated. This high temperature aqueous organic chemistry and the strong reducing conditions of the natural systems suggest this as an important route to produce organic compounds on the primitive earth. Thus a better understanding of the potential syntheses of organic compounds in hydrothermal systems will require investigations of the chemistry of condensation, autocatalysis, catalysis and hydrolysis reactions in aqueous mineral buffered systems over a range of temperatures from warm to >400 degrees C.

摘要

热液系统在地球活跃构造区域很常见。正在研究的可能发生有机质蚀变和有机合成的潜在地点包括洋中脊、轴外系统、弧后活动区、热点、火山活动和俯冲带。在这些高温且流体快速流动的热液环境中发生有机质蚀变,主要是还原作用,一般源自未成熟的有机碎屑。热循环水(温度范围从温热到>400摄氏度)导致了这些分子变化、排出和迁移。明显合成的化合物是次要成分,因为它们通常被当代天然有机前体形成的热解产物所掩盖。在瓜伊马斯盆地铁口系统的高温区和热液石油中已鉴定出杂环硫化合物。它们可被解释为由热液中的甲醛和硫或HSκ合成。潜在合成反应的其他产物在自然系统中尚未发现,但基于已知工业过程和实验模拟数据的推断是有望存在的。已对各种工业过程进行了综述,这些过程与有机化合物的热液合成相关。已在高压釜中研究了有机化合物在热水(200 - 350摄氏度)中的反应活性,并且也评估了超临界水作为化学介质的情况。这种高温水相有机化学以及自然系统的强还原条件表明这是原始地球上生产有机化合物的一条重要途径。因此,要更好地理解热液系统中有机化合物的潜在合成,将需要研究在从温热到>400摄氏度的温度范围内,在含水矿物缓冲系统中的缩合、自催化、催化和水解反应的化学过程。

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