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氰化氢和甲醛合成的能量产率:原始海洋中的氰化氢和氨基酸浓度。

Energy yields for hydrogen cyanide and formaldehyde syntheses: the HCN and amino acid concentrations in the primitive ocean.

作者信息

Stribling R, Miller S L

出版信息

Orig Life Evol Biosph. 1987;17(3-4):261-73. doi: 10.1007/BF02386466.

DOI:10.1007/BF02386466
PMID:2819806
Abstract

Prebiotic electric discharge and ultraviolet light experiments are usually reported in terms of carbon yields and involve a large input of energy to maximize yields. Experiments using lower energy inputs are more realistic prebiotic models and give energy yields which can be used to estimate the relative importance of the different energy sources on the primitive earth. Simulated prebiotic atmospheres containing either CH4, CO or CO2 with N2, H2O and variable amounts of H2 were subjected to the spark from a high frequency Tesla coil. The energy yields for the synthesis of HCN and H2CO were estimated. CH4 mixtures give the highest yields of HCN while H2CO is most efficiently produced with the CO mixtures. These results are a model for atmospheric corona discharges, which are more abundant than lightning and different in character. Preliminary experiments using artificial lightning are also reported. The energy yields from these experiments combined with the corona discharge available on the earth, allows a yearly production rate to be estimated. These are compared with other experiments and model calculations. From these production rates of HCN (e.g. 100 nmoles cm-2 yr-1) and the experimental hydrolysis rates, the steady state concentration in the primitive ocean can be calculated (e.g., 4 X 10(-6) M at pH 8 and 0 degrees). A steady state amino acid concentration of 3 X 10(-4) M is estimated from the HCN production rate and the rate of decomposition of the amino acids by passage through the submarine vents.

摘要

益生元放电和紫外线实验通常根据碳产量来报道,并且需要大量能量输入以实现产量最大化。使用较低能量输入的实验是更现实的益生元模型,其产生的能量产量可用于估计原始地球上不同能源的相对重要性。含有CH4、CO或CO2与N2、H2O以及不同量H2的模拟益生元大气受到高频特斯拉线圈产生的火花作用。估算了合成HCN和H2CO的能量产量。CH4混合物产生的HCN产量最高,而CO混合物最有效地产生H2CO。这些结果是大气电晕放电的模型,大气电晕放电比闪电更常见且性质不同。还报道了使用人工闪电的初步实验。这些实验的能量产量与地球上可用的电晕放电相结合,使得能够估算出年产量。将这些结果与其他实验和模型计算进行比较。根据这些HCN的产量(例如100纳摩尔·厘米-2·年-1)和实验水解速率,可以计算出原始海洋中的稳态浓度(例如,在pH值为8和0摄氏度时为4×10(-6)M)。根据HCN产量和氨基酸通过海底通风口的分解速率,估计氨基酸的稳态浓度为3×10(-4)M。

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