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Phosphine and methylphosphine production by simulated lightning - s study for the volatile phosphorus cycle and cloud formation in the earth atmosphere

机译:模拟闪电研究磷化氢和甲基膦的研究 - 挥发性磷循环和地球大气云的形成

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摘要

Phosphine (PH3), was recently found worldwide even in the remote atmosphere (Naturwissenschaften 83 (1996a,131, Atmos. Environ. 37 (2003) 2429). It is of interest to find natural mechanisms which could produce phosphine gas and drive a volatile link of the atmospheric phosphorus cycle and the formation of phosphoric acid as possible condensation nuclei for clouds.Here we report on simulated lightning exposing sodium phosphate in a reducing medium (methane model atmosphere or organic matter) for 5 seconds to a spark induced by microwave. The gas product analyzed by gas chromatography contained phosphine (yield up to 0.6 g per kg phosphate P) and methylphosphine (CH3)PH2 (yield up to 0.02 g per kg phosphate P).We suggest a plasma-chemical formation mechanism where organic compounds or methane or secondary hydrogen thereof reduce phosphate to phosphine of which a small fraction can subsequently react with methyl radicals to form methylphosphine. A small yield of 6 mg phosphine per kg phosphate P was even obtained in methane free medium, by simple plasmatic recombination of inorganic phosphorus. We believe that methane and hydrogen are useful model substances of pyrolytic gases with high reducing power which may form if lightning strikes biomass, soil and aerosol.These results suggest evidence that phosphine and methylphosphine (detectable in the field by intense garlic odor) are produced when atmospheric lightning strikes the ground or aerosol which is containing oxidized forms of phosphorus and chemical reductants.Additional reviewed data show that laboratory lightning was able to reduce a much more significant portion of phosphate to phosphite (up to 25% yield), methylphosphonic acid (up to 8.5% yield) and traces of hyposphosphite in a matter of seconds.
机译:最近在世界范围内甚至在偏远的大气中也发现了磷化氢(PH3)(Naturwissenschaften 83(1996a,131,Atmos。Environ。37(2003)2429)。寻找能够产生磷化氢气体并驱动挥发物的自然机制是令人感兴趣的。大气磷循环与磷酸的形成可能是云的可能凝结核之间的联系。在这里,我们报道了模拟雷电将磷酸钠在还原性介质(甲烷模型大气或有机物)中暴露5秒钟的微波火花。气相色谱法分析的气体产物中含有膦(每公斤磷酸盐P可达0.6克)和甲基膦(CH3)PH2(每公斤磷酸盐P高达0.02克),我们建议采用等离子化学形成机理,其中有机化合物或甲烷或其仲氢将磷酸盐还原为膦,其中一小部分随后可与甲基自由基反应形成甲基膦,每千克磷的产量为6毫克膦通过无机磷的简单等离子重组,甚至可以在无甲烷的介质中获得磷酸盐P。我们相信甲烷和氢气是热解气体有用的模型物质,如果雷电击中生物质,土壤和气溶胶,它们可能会形成高还原力,这些结果表明当磷化氢和甲基膦(强烈的大蒜味可在野外检测到)时产生大气中的闪电击中地面或含有氧化形式的磷和化学还原剂的气溶胶。附加的审查数据显示,实验室的闪电能够将磷酸盐的大部分还原为亚磷酸酯(产率高达25%),甲基膦酸(到8.5%的产率)和痕量的次磷酸盐在几秒钟之内。

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