The existence of carbocationic intermediates in a zeolite environment even at room temperature is supported by hydride (and deuteride) transfers between isoalkanes as monitored ex situ by (13)C NMR.
沸石环境中甚至在室温下,
碳阳离子
中间体的存在也受到异链
烷烃之间的
氢化物(和
氘代)转移的支持,这是通过(13)C NMR进行非原位监测的。