因此，深入研究砂岩成岩作用是分析孔隙水演化过程中离子迁移的重要环节。
Thus, studying sandstone diagenesis is an important link for analysis of ion migration in the evolution of pore-water.
利用铌酸锂晶体的结晶学结构特征，从微观角度上分析和研究了铌酸锂晶体的结构与离子迁移之间的关系规律。
The relationship between the crystallographic structure and ionic migration of lithium niobate single crystals are microscopically analyzed and investigated by their crystallographic characteristics.
定量考察了毛细管离子分析中温度及离子浓度对迁移时间的影响。
Influences of temperature and ion concentration on ion migration time in capillary ion analysis are studied.
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