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Abiological formation of formic acid on rocks in nature

机译:自然界岩石上甲酸的生物形成

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The formation of formic acid by ants is well known since the discovery by S. Fisher in 1670. In general, it has been believed that formic acid is not formed abiologically in nature. To evaluate the possibility of abiological formation of formic acid on silicate rock, a photochemical reduction of CO2 using silicate rock powders (amphibolite, gneiss, granite, granodiorite, quartzdiorite, shale and zeolite) suspended in water was investigated under sunlight at ambient temperature and pressure. It was found from the study that 4.6 x 10(-6) g formic acid/m(2) is formed daily on wetting-silicate rocks exposed to sunlight in nature. The range of the expected global production rate is between 2.5 and 3000 kt/a or more. Therefore, formic acid formed on wet-rocks might play an important role in the weathering of rocks. (C) 1999 Elsevier Science Ltd. All rights reserved. [References: 18]
机译:自1670年S. Fisher的发现以来,由蚂蚁形成甲酸是众所周知的。总的来说,人们相信甲酸不是自然地从生物学上形成的。为了评估在硅酸盐岩石上生物形成甲酸的可能性,研究了在环境温度和压力下于阳光下悬浮于水中的硅酸盐岩石粉末(闪石,片麻岩,花岗岩,花岗闪长岩,石英闪长岩,页岩和沸石)对二氧化碳的光化学还原作用。 。从研究中发现,在自然界中暴露于阳光的湿润硅酸盐岩石上每天形成4.6 x 10(-6)g甲酸/ m(2)。预期全球生产率的范围在2.5至3000 kt / a或更高之间。因此,在湿岩石上形成的甲酸可能在岩石的风化中起重要作用。 (C)1999 Elsevier ScienceLtd。保留所有权利。 [参考:18]

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