逸度的英文

• fugacity

• "逸"英文翻译    ease; leisure
• "度"英文翻译    surmise; estimate
• "氧逸度" 英文翻译 :    oxygenfugacity
• "易逸度" 英文翻译 :    fugacity
• "安逸度日" 英文翻译 :    pass days in indolence
• "逸度系数" 英文翻译 :    fugacity coefficient; fugafcity coefficient
• "逸度系数比" 英文翻译 :    fugafcity coefficient ratio
• "淫逸度日" 英文翻译 :    pass days with luxurious ease
• "安逸度日的人" 英文翻译 :    lotus-eater
• "兰德尔逸度规则" 英文翻译 :    lewis-randall rule of fugacity
• "逸定" 英文翻译 :    itsusada
• "逸刀" 英文翻译 :    hayato
• "逸儿" 英文翻译 :    itsuji
• "逸村" 英文翻译 :    itsumura
• "逸尔" 英文翻译 :    itsuji
• "逸次" 英文翻译 :    itsuji
• "逸二" 英文翻译 :    itsuji
• "逸纯" 英文翻译 :    itsusumi

• 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。
• The phase angles display a strong dependence on frequency ; the impedance magnitudes decrease across the entire frequency spectrum . the activation enthalpies lie in the range of 1 . 03 - 2 . 11ev
  在压力为l一3gpa 、温度为1282一z544k 、频率为0 . 1一lo6hz 、氧逸度为mo一mooz的条件下，对纯橄榄岩的电导率进行了测量。
• 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
• Secondly , based on the microbeam analytical technique , on the one hand , through investigating the characteristic of major elements in the mantle minerals the author acquired the static information from mantle ; on the other hand , through multi - point analysis of a part of the minerals from mantle , the auther got dynamic information from mantle . finally , generalizating the fruits of this study and predecessors , the autor holds that the constituents of lithospheric mantle possibly includes spinel lherzolites , clinopyroxenites , websterite , dunite , harzburgites , garnet lherzite , phlogopite lherzite , eclogites , clinopyroxene megacrysts ; compared with east china and north china platform , the research field mantle shows the characteristics of higher degree of partial melting processes and more depleted mantle ; the . upper mantle beneath north hetian area is heterogeneous , with a tendency of deficit in a12o3 and lree from kaliyang in west hetian to the river basin of kalakshi river and yulongkashi river ; the subduction of the crust beneath north hetian has ever occurred in geological history and caused the mixing of mantle - crust ; the depth of the origination of basaltic magmas beneath north hetian exceeds 73km ; the thickness of the lithosphere beneath the research area amounts to 204 . 9km ; the mantle beneath north hetian has geological condtions for forming diamond deposits
  最后，综合本区幔源矿物和地幔岩石的特征以及地球物理资料，得出如下结论：本区上地幔的物质组成有尖晶石二辉橄榄岩、二辉岩、单斜辉石岩、纯橄榄岩、方辉橄榄岩、石榴石二辉橄榄岩、金云母二辉橄榄岩、榴辉岩；与中国东部以及华北地台上地幔相比，研究区上地幔具有富集主元素中相容元素和亏损其中的不相容元素的特征，局部熔融程度较高；上地幔存在横向和纵向的不均一性，从西部的克里阳到喀拉喀什河和玉龙喀什河流域， al和lree富集程度呈下降趋势，不同来源的相同矿物中主元素的含量差异较大；地质历史时期这里可能发生过地壳俯冲并产生壳幔混合作用；玄武岩浆的起源深度73km ；从幔源重砂矿物的温压估算结果，可以推断出岩石圈厚度可达204 . 9km ；综合岩石圈物质组成特征、岩石圈热状态、地幔温压状态、氧逸度以及幔源岩石和幔源矿物的化学成分，认为研究区具备了金刚石成矿地幔地质条件。
• Ore - forming fluid , mineralizing agent , auxiliary aget came mainly from the mixing of deep - source bittern , formation water , palaeometeoric water . ( 5 ) when sinking palaeometeoric water and rising deep - source solution mixed during their moving , their physicochemical condition was changed , which made ore - forming
  下渗的大气降水与上升的深源流体在运移过程中混合，使得溶液的温度、 ph值、 h _ 2s的浓度、硫逸度、氧逸度以及氧化还原电位改变，从而发生成矿作用。
• 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。

• 逸度的法语：Fugacité
• 逸度的韩语：퓨가시티
• 逸度的俄语：pinyin:yìdù 1) превосходные манеры, прекрасная выправка 2) физ. фугитивность, рассеиваемость
• 逸度的阿拉伯语：انفلاتية;
• 逸度的印尼文：fugasitas;
• 逸度什么意思：超逸的风度。    ▶ 《世说新语‧文学》“ 裴冀州 释二家之义， 通彼我之怀” 刘孝标 注引 三国 魏 管辰 《管辂别传》： “ 裴使君 有高才逸度， 善言玄妙也。”    ▶ 元 辛文房 《＜唐才子传＞引》： “及其逸度高标， 馀波遗韵， 临高能赋， 闲暇微吟， 旧格近体、古风乐府之类， 芳沃当代， 响起陈人。”    ▶ ...