Based on this, double exchange of tetrads and centromere mapping are analysed and discussed in detail. 在此基础上,对双交换(DE)四分子的分析和着丝粒作图进行了详细地讨论。
Using the competing between manganites crystal field and double exchange interaction explains the metal property at room temperature. 用锰氧化物晶场和双交换(DE)作用的竞争解释了其温度Tp以下的金属特性。
The results are attributed to double exchange interaction, magnetic dilution and lattice effects arising from Zn doping. 这些结果归因于Zn掺杂引起的双交换(DE)作用、磁稀释作用和晶格效应。
The above results support the double exchange model in manganite. 从结构和磁性两个方面,证实了双交换(DE)模型在解释锰氧化物的铁磁金属性是合理的。
This behaviors can be explained by double exchange ( DE ) model and nonmagnetic randomness. 在T>TC区域,电阻率、磁电阻都随温度的升高而迅速下降,样品在高温(TC附近及T>TC区域)的这一行为可用双交换(DE)(DE)模型与非磁无序来说明。