fugacity造句

• Lewis - randall rule of fugacity
  兰德尔逸度规则
• Coefficient of fugacity
  逸度系数
• ( 7 ) by studying of ore - forming fluid and the micas ( using the f , cl contents in micas to calculate the halogen fugacity of the hydrothermal fluid , eg
  ( 7 )通过对成矿流体和花岗质岩石黑云母、白云母中卤素相对逸度的研究( 109担20 / fh 。
• Based on a brief analysis of the genesis of hematite , the authors hold that hematite in red granite was mostly produced under the condition of high oxygen fugacity
  本文对赤铁矿的成因作了简要分析，认为红色花岗岩中的赤铁矿大多为高氧逸度条件下的产物。
• 5 the fugacity coefficients , residual enthalpies and residual entropies of the pure fluids at low temperatures and high pressures were predicted with the general quintic virial equation
  10 。 5用上述通用五次维里方程预测了纯流体在低温高压下的逸度系数、剩余恰和剩余嫡。
• Jin - hsiang lo and whei - may grace lee , 1994 / 9 , experimental study of fugacity capacity of hydrophobic organic compounds in atmospheric fog , proceedings of the 7th iuappa regional conference on air pollution and waste issues
  罗金翔,李慧梅, 1994 / 10 ,雾粒中界面活性物质对有机污染物扩散挥发之影响,第十一届空气污染控制技术研讨会论文专辑
• Abstract : the more precise equation of r - k was used to calculate the real gases . based on the generolized measurement of fugacity , the equation of substance ' s fugacity coefficient of mixed gqses was derived , and the results of the application was discussed
  文摘:对实际气体选择较精确的r - k方程，根据逸度计算的普遍化公式，导出了混合气中物质逸度系数表达式，并对其应用结果进行了讨论
• Then the structure unit of hexangular lattice is found according to the principle of invariable symmetry . renormalization transformation is processed when we regard the structure unit and the growth model as graphs before and after transformation respectively . after choosing the 11 thermodynamic function fugacity as parameter , we can write out the partition functions before and after transformation and the formula of renormalization transformation
  然后根据对称性不变的原则，从整体晶格中选取结构单元，把结构单元和生长模型分别作为重整化变换前、后的图形来进行重整化变换，选取热力学函数易逸度为参量，写出了重整化变换前后的配分函数和重整化变换关系式，求出了这一变换的不动点。
• And apatite . by these analyses and comparison with general granite both in china and the world and with the granite in other au or cu belt in china , the characteristics of the granite in this area are concluded as follows . it belongs to magnetite - i or syntectic granite and has crust - mantle mixed characteristics ; it was formed mainly by crystallization differentiation of melting magma and multiphase varied intrusion ; the degree of differentiation evolvement is not high ; the granite and its enclaves p . re congenetic ; the range of temperature is about 500 - 700 , the range of pressure is about 2 . 50 gpa - 4 . 35 gpa , and the range of oxygen fugacity ( lg fo2 ) is - 15 . 53 - - 14 . 00 ; most granite bodies formed before the collision of plates , and few formed after the collision of plates
  通过对测试数据的分析与综合研究，并同中国和世界一般花岗岩类以及中国主要金、铜成矿岩体的花岗岩类进行对比，得出本区花岗岩类岩石具有以下特征：属磁铁矿-型或同熔型花岗岩，其岩浆物质具壳幔混源特征：主要由熔融态岩浆经结晶分异作用，通过多期变速上侵而形成；其分异演化程度较低；寄主岩基和包体具有同源性；岩石的形成温度范围约为500 - 700 ，压力大约为2 . 50gpa - 4 . 35gpa ，氧逸度值1gfo _ 2为- 15 . 53 ? 14 . 00 ；该岩带主要形成于板块碰撞前消减的活动板块边缘期，为燕山至喜马拉雅早期的大陆边缘火山弧环境的产物。
• A new measurement system for electrical conductivity in an yj - 3000t press fitted with a wedge - type cubic anvil was set up on the basis of the old one . a solartron 1260 impedance / gain phase analyzer was used in the new system ; mo electrodes and a mo shield were also used to keep oxygen fugacity close to the mo - moo2 , which is similar to that of iron - wustite ( iw )
  在yj ?紧装式六面顶压机上，对原有的矿物、岩石电性测量系统进行了进一步的改进：建立了一套以solartron1260阻抗增益?相位分析仪为测试仪器，使用mo电极和mo盾来控制样品氧逸度的测量系统，该系统的氧逸度环境为mo ? moo _ 2 ，接近iw缓冲对。