| 1. | Lewis - randall rule of fugacity 兰德尔逸度规则 |
| 2. | Coefficient of fugacity 逸度系数 |
| 3. | ( 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 。 |
| 4. | 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. | 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。 |
| 6. | 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 |
| 7. | 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 |
| 8. | 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。 |
| 9. | 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。 |
| 10. | 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。 |