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fluid composition
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  流体组成
     An Appraisal of Different Experimental Methods in the Determination of Fluid Composition in Mantle-derived Rocks
     对幔源岩中流体组成的不同测定方法评价
短句来源
     Chemical equilibrium calculations of fluid composition and thermodynamical analysis of metamorphic reactions show that the lower metamorphic temperature of kyanite zone is resulted not from the effect of metamorphic pressure and retrogressive metamorphism but from the buffering of temperature of dehydration metamorphic reaction forming kyanite by fluids with lower XH2o. The buffered temperature range is up to 100℃ ̄200℃.
     流体组成化学平衡计算和变质反应热力学分析研究表明,蓝晶石带较低的变质温度并非是压力或退化变质作用所致,而是低XH2O流体对形成蓝晶石的脱水变质反应温度缓冲的结果,缓冲温度值高达100℃~200℃。
短句来源
     The Distribution Law of the Fluid Composition along the Wet-gas Pipelines
     湿天然气输送管道流体组成分布规律研究
短句来源
     The main tasks of reservoir geochemical description are to analyze the heterogeneity, distribution and origin of fluids, and to approach the charge mechanism of fluid through geochemical study of the fluid composition in the reservoir.
     油藏地球化学描述的主要工作是通过对油藏内流体组成的地球化学剖析,分析流体非均质性特征、分布规律及其成因,探讨流体充注机制。
短句来源
     The physical and numerical simulation methods were adopted to study the fluid composition, the viscosity temperature and seepage characteristics of reservoirs. The influencing parameters of steam soaking technology on the reservoir development are analyzed.
     应用物理模拟与数值模拟方法研究了超稠油的流体组成、粘温关系和油藏渗流特征 ,分析了超稠油蒸汽吞吐注汽工艺参数对开采效果的影响。
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  流体成分
     There is marked difference in Equilibrium fluids' composition between Al rich gneiss and marbles. Metamorphic fluid equilibrating with diopside marble and fosterite marble presents x (H 2O)=0 02~0 07, however, these equilibrating with Al rich gneiss has higher water, x (H 2O)=0 27~0 747. There is a great disparity among different rocks in fluid composition in a small area.
     富铝片麻岩和大理岩类岩石中平衡流体成分相差甚大:与透辉大理岩和橄榄大理岩平衡的变质流体成分x(H2O)=0.02~0.07,近于纯二氧化碳; 与富铝片麻岩平衡的流体成分则含有相对较高的水,x(H2O)=0.27~0.747。
短句来源
     The method takes account of the influence of skeleton composition, shale content, porosity, fluid composition, saturation, temperature, and pressure on P and S-waves velocities of oil and gas reservoirs.
     该方法综合考虑了骨架成分、泥质含量、孔隙度、流体成分、饱和度以及温度和压力对油气层速度的影响。
短句来源
     In recently years, the study of ore-forming fluid has achieved some important advances in many ways, such as store and movement of large scale ore-forming fluid, the relationship between giant ore deposit and fluid, the transported dynamics of ore-forming fluid, hydrothermal ore-forming reaction systems, diterminative mothed of fluid composition and so on.
     近年成矿流体研究在大规模流体的存在与运移、巨型矿床与流体的关系、成矿流体输运动力学、建立热液成矿反应体系及成矿流体成分测试技术等方面取得了重要进展 ;
短句来源
     An inclusion within kyanite eclogite is characterized by fluid composition of the nletamorphic peak stage: higher in hemogeneuus tem-perature, relative lower in ice-puint, Complicated-varied in composition and with anatectic characteristics;
     蓝晶石榴辉岩中的石英包裹体表现为变质峰期的流体成分特征:均—温度较高、冰点相对较低、成分复杂多样,具深源特征;
短句来源
     If the fluid was trapped under the condition which is higher than the homogenization temperature, by extrapolation along the isochore corresponding to the fluid composition and density, either the pressure or temperature of trapping may be acquired, provided that the other parameter is known. Each fluid inclusion is both a recording geothermometer and a geobarometer.
     如果流体是在高于均一温度的条件下被捕获,那么沿着相应流体成分和密度的等容线外推,只要压力和温度中一个参数已知,就可以求出捕获温度或捕获压力。
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  流体组分
     The influence of fluid composition and its content on pressure drop and liquid holdup in landing natural gas and condensate pipeline
     流体组分及其含量变化对天然气-凝析液混输上岸管道滞液量和压降的影响
短句来源
     The components of the fluids released from alkali basalts and mantle-derived Iherzolite xeno-liths in eastern China have been determined by the vaccum pyrolysis-mass spectrometric (MS) method in the present study. The results show that mantle-derived Iherzolites formed in fluids composed mainly of reducing gases such as H2 and CO, and their fluid composition is characterized by a higher H2 content and a lower total content of volatiles.
     中国东部新生代碱性玄武岩及其幔源三辉橄榄岩捕虏体中的流体组分存在差异,幔源二辉橄榄岩形成于以H_2、CO等还原性气体为主的流体环境中,其流体组分以含H_2高、挥发性气体总量低为特征;
短句来源
  “fluid composition”译为未确定词的双语例句
     The Nitrogen aerated polycol drilling fluid composition was determined in lab, that is: (1%~2%)MMH+(2%~3%)PPG-1+(2%~3%)SMP+(0.4%~0.6%)PAM+auxiliary additives.
     室内确定了充 (氮 )气多元醇防塌钻井液体系配方为 :(1%~ 2 % )MMH +(2 %~ 3% )PPG 1+(2 %~ 3.5 % )SMP +(0 .4 %~ 0 .6 % )PAM +辅助处理剂。
短句来源
     Effects of bore fluid composition and heat post-treatment on membrane performance and separation properties of O2/N2、H2/N2 and He/H2 were investigated.
     研究了不同芯液组成和中空纤维热处理对O2/N2、H2/N2和He/N2膜性能的影响.
短句来源
     The optic nerve: A new window into cerebrospinal fluid composition?
     视神经:了解脑脊液成分的新视窗?
短句来源
     Fluid composition features high Cl -/SO 4 2- . The Ar-Ar dating (320 Ma±6 Ma) reflects the latest hydrothermal mineralizing age. It is genetically a volcanic exhalation-sedimentary superimposition deposit.
     成矿温度为中温 (2 40℃~310℃ ) ,流体成份以Cl-/SO4 2 -高为特征 ,矿石矿物中石英Ar-Ar年龄 (32 0Ma± 6Ma)反映最终成矿构造热液叠加年龄 ,矿床属火山喷流沉积改造型金矿床
短句来源
     The Xco_2 of fluid in epidote vein in the Kouquan valley is 0.08; while in its surrounding dolostone, larger than 0.4. The difference in Xco_2 in the vein and its surrounding rock also provides evidence that the fluid composition is controlled by buffering.
     口泉主沟内绿帘石脉体中流体的X_(CO_2)为0.08,而围岩白云岩中X_(CO_2)大于0.4,同一地点脉体和围岩中变质溶液具有不同的X_(CO_2)说明溶液成分受缓冲作用控制。
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  fluid composition
Apart from the types of the organic matter, the physical environment (temperature and pressure) and chemical environment (fluid composition and inorganic elements) will result in the abnormal vitrinite reflectance values in the sedimentary basins.
      
Fluid composition and origin in the hydrothermal system of the Nezhdaninsky gold deposit, Sakha (Yakutia), Russia
      
On the quantitative evaluation of metamorphic fluid composition: Verification of the results of physicochemical simulations for
      
It is provided with a feedback system with the sympathetic center controlling the lubricating conditions of the movable joint of the articular bone ends, the lubricating fluid composition, and the elimination of debris from the articular capsule.
      
The variety of waveform character reflects stratigraphic differences and frequency spectrum differences reflect the variation of lithology, fluid composition, and formation thickness.
      
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The first order big fault, occurred either in a single one or in a group,is found in many vein-like W(Sn)deposit areas, and characterized by mulitperiodic activity. Minerogenetic fractures may be induced by fault of this type. Mineralizations filled in fractures are under the control of the fault. For this reasonit is named as an induced-controlled fault. It is a premineraliaztion structure composed of a complex fault zone, because it had undergone structural activities many times during and after the mineralization....

The first order big fault, occurred either in a single one or in a group,is found in many vein-like W(Sn)deposit areas, and characterized by mulitperiodic activity. Minerogenetic fractures may be induced by fault of this type. Mineralizations filled in fractures are under the control of the fault. For this reasonit is named as an induced-controlled fault. It is a premineraliaztion structure composed of a complex fault zone, because it had undergone structural activities many times during and after the mineralization. It consists of fracture belts several metres wide,in which wall-rock alterations suck as silicification, chloritization,sericitization, etc., are observed. In addition,along the fracture belts metallogenic elements ro volatile elements halo anomalies are also detected. The induced-controlled fault plays an important role in controlling metallogenesis, vertical zonality, the position of enriched zones, the distribution of useful components, mineralization temperature, ore-bearing fluid (composition and flow direction) and the dip of the ore veins. It is also a structure of the derived rocksand an emplacement place of the concealed granite at the bottom of the ore deposit. A study of induced-controlled fault is significant for the exploration of semi-concealed 'five storeys'type W(Sn)deposits.

在很多脉状钨锡矿床中,都可以见到一条或一组矿区级的大断层。它具有多期次活动的特点,并引生了矿床的成矿裂隙,在裂隙充填成矿的全过程中又起明显的控制作用,故称之为引控断层。它是成矿前构造,成矿期及成矿后又多有活动,故为综合性断层。断层多由宽数米的破碎带组成,常见硅化、绿泥石化、绢云母化等蚀变,沿断层破碎带常出现成矿元素或挥发性元素的晕带。引控断层对矿床的成矿作用、垂向形态分带、规模、富集段的产出位置、有用组分的分布、成矿温度、含矿流体组分及流向、矿脉倾侧方向等均起明显的控制作用,又是矿床底部隐伏花岗岩的导岩构造和侵位场所。研究引控断层对寻找半隐伏的、具“五层楼”式的脉状钨锡矿床有一定的指导意义。

The fluid systems concerning fluid inclusions are divided into two categories: non-brine system and brine system. It is very important to study and to understand the phase equilibria data of these fluid systems for exploiting fully various useful informations reserved in fluid inclusions.In the study of fluid inclusions we assume generally that the fluid inclusion has remained a system of constant volume and constant composition since it formed. In a fluid inclusion with constant volume and composition, both...

The fluid systems concerning fluid inclusions are divided into two categories: non-brine system and brine system. It is very important to study and to understand the phase equilibria data of these fluid systems for exploiting fully various useful informations reserved in fluid inclusions.In the study of fluid inclusions we assume generally that the fluid inclusion has remained a system of constant volume and constant composition since it formed. In a fluid inclusion with constant volume and composition, both the molar volume and the composition of the fluid can be determined from temperatures of phase transitions involving univariant equilibria. The overall composition of an inclusion may be infered from the eutectic temperature(or temperature of first melting).The concentration is given by the final melting temperature of solids which form as the system is cooled.The relative proportions of different salts in the solution can be estimated from the melting of solid phases between the eutectic temperature and the disappearance of the last solid to melt,Estimates of density are based on the homogenization temperature of the fluid inclusions.If the fluid was trapped under the condition which is higher than the homogenization temperature, by extrapolation along the isochore corresponding to the fluid composition and density, either the pressure or temperature of trapping may be acquired, provided that the other parameter is known.Each fluid inclusion is both a recording geothermometer and a geobarometer.Various valid fluid inclusion geobsrometers have been also presented and discussed in this paper.The pressure data provided by the fluid inclusion geobarometers are of more than academic interest. Because they provide some evidence of the depth beneath the surface at which the process occured,they can provide the exploration geologist with valuable information on the amount of cover that has been faulted or eroded away, the possible nature of the deposit, the former occurrence of boiling that can cause ore deposition, etc.and pressure differences may eventually also yield information on the direction of flow of the ore-forming fluids.

与流体包裹体有关的流体系统可分为非盐水体系和盐水体系两大类。研究和熟悉这些流体体系的相平衡数据对于充分开发流体包裹体中所储存的各种有用信息具有重要意义。流体包裹体研究中一般假定流体包裹体形成之后保持为一恒容、恒组成体系,其所含流体的摩尔体积和组成都能从与单交平衡有关的相变温度加以确定。根据低共熔温度(或初熔温度)可以推断包裹体的总组成。由体系冷却时所形成的固相的最终熔化温度可以求得流体的浓度。还可以根据低共熔点和最后一个固相消失温度间的固相熔化情况估测溶液中各种盐类的相互比例。包裹体的均一温度可以用来测定所含流体的密度。如果流体是在高于均一温度的条件下被捕获,那么沿着相应流体成分和密度的等容线外推,只要压力和温度中一个参数已知,就可以求出捕获温度或捕获压力。每一个流体包裹体都是一个纪录在案的地质温压计,本文介绍和讨论了各种有效的流体包裹体地质压力计,它们所提供的压力数据不仅能够提供有关地质作用发生的深度,还能提供有关错断和剥蚀作用的强度等重要信息。流体包裹体压力计对于研究成矿作用也有重要意义,例如压力降引起的沸腾作用可以导致成矿物质沉淀,根据压力差还可以获得有关成矿流体流动方向的信息。

The fluid systems concerning fluid inclusions are divided into two categories:non-brine system and brine system.It is very important to study and to understand the phase equilibria data of these fluid systems for exploiting fully various useful informations reserved in fluid inclusions.In the study of fluid inclusions we assume generally that the fluid inclusion has remained a system of constant volume and constant composition since it formed.In a fluid inclusion with constant volume and composition,both the...

The fluid systems concerning fluid inclusions are divided into two categories:non-brine system and brine system.It is very important to study and to understand the phase equilibria data of these fluid systems for exploiting fully various useful informations reserved in fluid inclusions.In the study of fluid inclusions we assume generally that the fluid inclusion has remained a system of constant volume and constant composition since it formed.In a fluid inclusion with constant volume and composition,both the molar volume and the composition of the fluid can be determined from temperatures of phase transitions involving univariant equilibria.The overall composition of an inclusion may be infered from the eutectic temperature(or temperature of first melting).The concentration is given by the final melting temperature of solids which form as the system is cooled.The relative proportions of different salts in the solution can be estimated from the melting of solid phases between the eutectic temperature and the disappearance of the last solid to melt.Estimates of density are based on the homogenization temperature of the fluid inclusions.If the fluid was trapped under the condition which is higher than the homogenization temperature,by extrapolation alone the isochore corresponding to the fluid composition and density,either the pressure or temperature of trapping may be acquired,provided that the other parameter is known.Each fluid inclusion is both a recording geothermometer and a geobarometer.Various valid fluid inclusion geobsrometers have been also presented and discussed in this paper.The pressure data provided by the fluid inclusion geobarometers are of more than academic interest.Because they provide some evidence of the depth beneath the surface at which the process occured,they can provide the exploration geologist with valuable information on the amount of cover that has been faulted or eroded away,the possible nature of the deposit,the former occurrence of boiling that can cause ore deposition,etc.and pressure differences may eventually also yield information on the direction of flow of the ore-forming fluids.

与流体包裹体有关的流体系统可分为非盐水体系和盐水体系两大类.研究和熟悉这些流体体系的相平衡数据对于充分开发流体包裹体中所储存的各种有用信息具有重要意义.流体包裹体研究中一般假定流体包裹体形成之后保持为一恒容、恒组成体系,其所含流体的摩尔体积和组成都能从与单变平衡有关的相变温度加以确定.根据低共熔温度(或初熔温度)可以推断包裹体的总组成.由体系冷却时所形成的固相的最终熔化温度可以求得流体的浓度.还可以根据低共熔点和最后一个固相消失温度间的固相熔化情况估测溶液中各种盐类的相互比例.包裹体的均一温度可以用来测定所含流体的密度.如果流体是在高于均一温度的条件下被捕获,那么沿着相应流体成分和密度的等容线外推,只要压力和温度中一个参数已知,就可以求出捕获温度或捕获压力.每一个流体包裹体都是一个纪录在案的地质温压计,本文介绍和讨论了各种有效的流体包裹体地质压力计,它们所提供的压力数据不仅能够提供有关地质作用发生的深度,还能提供有关错断和剥蚀作用的强度等重要信息.流体包裹体压力计对于研究成矿作用也有重要意义,例如压力降引起的沸腾作用可以导致成矿物质沉淀,根据压力差还可以获得有关成矿流体流动方向的信息.

 
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