湖相盆地层序发育的主要控制因素为构造升降、湖平面变化和沉积物供应速率的变化。
Main controlling factors of sequence development in lacustrine basins are tectonic uplift and subsidence, lake-level changes, and changes of sediment supply rates.
电流强度是渗滤液toc降解的控制因素，TOC的降解速率随电流强度升高而逐渐提高。
Current density was the control factor and the degradation rate of TOC increased gradually with current density.
原子的扩散传质速率是控制总反应速率的关键因素。
The rate of N atom diffusion is the key factor of controlling whole nitridation rate.
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