34S enrichment is shown to occur during sulfurization reactions and for the first time conclusively attributed to an isotope equilibrium effect rather than selective addition of 34S enriched nucleophiles.
34S 富集被证明是在
硫化反应过程中发生的,并且首次最终归因于同位素平衡效应,而不是选择性添加 34S 富集的亲核试剂。