Science. 1970 Nov 27;170(3961):980-2. doi: 10.1126/science.170.3961.980.
Carbon dioxide and organic compounds made by a Fischer-Tropsch reaction at 400 degrees K show a kinetic isotope fractionation of 50 to 100 per mil, similar to that observed in carbonaceous chondrites. This result supports the view that organic compounds in meteorites were produced by catalytic reactions between carbon monoxide and hydrogen in the solar nebula.
在 400 开尔文下进行的费托反应产生的二氧化碳和有机化合物表现出 50 到 100 个千分位的动力学同位素分馏，类似于在碳质球粒陨石中观察到的分馏。这一结果支持了这样一种观点，即在陨石中，有机化合物是由一氧化碳和太阳星云中的氢之间的催化反应产生的。
