apparent diffusion coefficient meaning in Chinese
表现弥散系数
Examples
- From the concentration dependence of bsa apparent diffusion coefficients , protein interaction parameters have been regressed . it bears a net effective charge of - 9 . 0 and has a hamaker constant of 2 . 8ket
根据扩散系数随蛋白浓度变化的斜率与离子浓度变化的相关性，回归出了蛋白相互作用参数，蛋白所带的有效电荷zp二一9 . oe 、 hamaker常量= 2 - In this paper , the performance of adsorbing and retarding 125i ( substituted for 129i ) for mixed materials as buffer , backfill material was investigated , the distribution coefficient kds by batch sorption experiments were determined for four kinds of minerals and one kind of bentonite under atmosphere , iodine sorption and desorption on several mianerals were studied under low oxygen ambience at first time in the domestic , and apparent diffusion coefficient da of 125i ~ was determined for mixed minerals under atmosphere
在大气条件下用批式实验法研究了放射性125i - 、 125io3 - (用i - 125代替i - 129 )在黄铜矿、方铅矿、黄铁矿、辰砂上的吸附和解吸行为，并且在国内首次研究了低氧条件下碘在几种矿物上的吸附和解吸行为；在大气条件下，用恒定源扩散法研究了125i -在方铅矿与膨润土组成的混合材料中的扩散行为。 - The concentration dependence of bsa apparent diffusion coefficients was interpreted in the context of a two - body potential of mean force that includes repulsive hard - sphere and coulombic interactions and attractive dispersion : with increasing ionic strength , debye screening decreased , and protein interaction changed from repulsion to attraction , and protein aggregations was onset
利用平均势场理论的两体硬球相互作用模型解释了蛋白分子的相互作用变化规律：随着离子强度的增加，离子氛厚度减小，蛋摘要白分子间的相互作用由排斥变为吸引，蛋白开始聚集。 - For same mineral , desorption of 125i " on it was weaker than 125io3 " , and sorption of 125i i25io3 " on galenite is irreversible . apparent diffusion coefficient da of 125i " in the mixed material were determined by the pass - through diffusion way , da values under atmosphere was given : da = 7 . 29x10 - 12m2 ? s - 1
大气条件下，随体系固液比的减小，固相的量相对在下降， 125i -在矿物材料上的kd值减小；随材料粒度的减小，材料的比表面积增加， 125i -在矿物材料上的kd值有所增加。