1) limit partitioning coefficient
极限分配系数
2) limit distribution patterns
极限配分值
1.
From this formula limit distribution pattterns of RE ions in electrolyte are calculated,and the effect of different factrors on limit distribution patterns in discussed.
在大量的实验数据基础上引入了析出金属和电解质中两种配分比值的概念,建立了电解质中配分的计算公式,由此导出了电解质中各种稀土离子的极限配分值,讨论了影响极限配分值的有关因素。
3) limit ironing coefficient
极限延系数
4) distribution coefficient
分配系数
1.
Laboratory determination of diffusion and distribution coefficients of contaminants in clay soil;
污染物离子在粘土介质中扩散系数和分配系数的测定(英文)
2.
Swelling behavior and distribution coefficient in the silicone rubber membranes;
硅橡胶膜中的溶胀行为及分配系数
3.
The results showed that the distribution coefficient decreased with increasing temperature and depended on the concentration of L-Phe and the initial pH value of aqueous phase.
以磷酸二(2-乙基己基)脂(D2EHPA)为萃取剂,环己烷为稀释剂萃取L-苯丙氨酸(L-Phe),研究了L-Phe浓度、D2EHPA浓度、温度对萃取分配系数D的影响,以及负载L-Phe有机相的反萃取特性。
5) partition coefficient
分配系数
1.
QSPR study and three-dimensional descriptor characterization of membrane-water partition coefficient of compounds.;
化合物膜水分配系数的QSPR研究和分子三维参数表征
2.
Determination of partition coefficient of trace anionic surfactants in oil/water systems with visible spectrophotometry;
分光光度法测定微量表面活性剂在油/水体系中的分配系数
3.
Adsorption volume and partition coefficient of adsorbate between solid and liquid phase in dilute solution;
稀溶液中溶质的固/液吸附体积及分配系数
6) partitioning coefficient
分配系数
1.
The size of pyrene partitioning coefficient (Koc) in different property NOM was related with aromatic structure and the hydrophobic basic group content in NOM.
结果表明,芘在不同性质NOM中分配系数(Koc)的大小与NOM中芳香结构和疏水基团含量有关,芘在液相、吸附相NOM中的分配行为受NOM自身特性、吸附性能及吸附剂表面有机碳覆盖率(foc)大小的影响。
2.
A series of experiments have been carried out for determining partitioning coefficients of tungsten and tin between various types of hydrothermal fluids and granitic melt (Dwv/L and Dsv/Ln) at 850℃ and 150 MPa.
本文用实验确定了钨、锡在成分不同的花岗质熔体相与共存水热流体相的流-熔分配系数(D_(Me)~(V/L))及其与介质溶液(NaF,KF,HF,NaCl等水溶液)摩尔浓度间的函数关系。
3.
Partitioning coefficient of trace elements between mantle minerals and aqueous fluids is important to understand the evolution and tectonics of the Earth.
微量元素在幔源矿物与热液之间分配系数的差异是造成地幔不均一的一个重要因素 ,对于认识地球演化、元素的分异和板块构造具有重要的意义。
补充资料：稳定极限和静态稳定储备系数
稳定极限和静态稳定储备系数
stability limit and steady state stability margin
wend一ngJ一xlorl heJ一r飞gt。}咖erld一rlgc}〕LJ匕fJ稳定极限和静态稳定储备系数x}S)〕走』limit and steady一state stability margin)力系统德定。(stability 见电
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条