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液态
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  “液态”译为未确定词的双语例句
    A PRIMARY STUDY ON CARBON ISOTOPE OF N-ALKANE,PRISTANE AND PHYTANE IN CRUDE OIL
    液态正构烷烃系列、姥鲛烷、植烷碳同位素初步研究
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    DISCUSS ON THE LIQUID-POTASH DEPOSIT AND ITS EXPLOITING IN SICHUAN BASIN
    四川盆地液态钾矿资源及其开发有关问题探讨
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    Secreet resinite is characterized by early maturation,and its“oil window”is in the region of 0.35% to 0.75% of vitrinite reflectance,howe- ver,the amber resinite is lately matured,and its“oil window”is from 0.50% to 1.0%.
    泌树脂体具有早期生油的特点,其液态窗范围介于镜质组 R_r=0.35%~0.75%之间; 琥珀树脂体成熟较晚,其液态窗范围介于 R_r=0.50%~1.0%之间;
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    The melt structures of the above three immiscible melts mainly differ in the number of bridge oxygen: the highest in the relative acid globe and lower in the relative basic melt, but in the melt structure of the ore-forming melt all oxygen is non-bridge oxygen.
    液态不混溶作用产生的三种不混溶熔体的结构差异明显,主要表现在结构单元中桥氧数目的变化,相对偏酸性的A类小球体的结构单元中桥氧数最高,基底玻璃熔体中桥氧数则相对较少,而成矿熔体中不存在桥氧。
短句来源
    In the third stage, triple phase inclusions with fluid CO 2 and the lowest density were trapped.
    第三阶段捕获了低密度的三相含液态CO2包裹体。
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Thermal evolution simulation tests of kerogen of sapropel type in the immature source rocks from No. 1 Nen Section of Cretaceous of Songliao basin are carried out, together with analyses of the loss of weight due to heating and of the products of simulation tests (in gas and liquid state) to indicate the significance of heat and time of exposure to heat in the evolution of kerogen. The process of transformation of kerogen into hydrocarbons is discussed through a comparative study of the properties of its evolution...

Thermal evolution simulation tests of kerogen of sapropel type in the immature source rocks from No. 1 Nen Section of Cretaceous of Songliao basin are carried out, together with analyses of the loss of weight due to heating and of the products of simulation tests (in gas and liquid state) to indicate the significance of heat and time of exposure to heat in the evolution of kerogen. The process of transformation of kerogen into hydrocarbons is discussed through a comparative study of the properties of its evolution products with those of oil and gas, and it is proposed that hydrocarbons are formed due to increase of temperature that leads to the constant internuclear adjustment of bonds of various functional groups of kerogen.

本文用松辽盆地白垩系嫩一段未成熟生油岩的腐泥型干酪根、进行了热变模拟试验、热失重分析以及热变模拟产物(包括气态、液态)的分析,指出了干酪根演化过程中温度和受热时间的意义。根据热变产物和油、气性质的比较,讨论了干酪根转化及成烃过程,认为烃类的生成是由于温度的增加,不断地调整干酪根核间各种官能团化学键的结果。

Based on the character of source rocks of the oil pools at Banqiao and Qikou in the central part of Huanghua depression, the process of evolution of organic matter into hydrocarbons is divided into four stages, with the thermal window for oil formation at 85.5-163℃(2,000-4,200 meters). According to the properties of alkanes, source rocks of Paleogene of this area are classified into 5 types and crude oils into 2 main groups in 6 subdivisions. Oil sources are compared on the same basis, which leads to the supposition...

Based on the character of source rocks of the oil pools at Banqiao and Qikou in the central part of Huanghua depression, the process of evolution of organic matter into hydrocarbons is divided into four stages, with the thermal window for oil formation at 85.5-163℃(2,000-4,200 meters). According to the properties of alkanes, source rocks of Paleogene of this area are classified into 5 types and crude oils into 2 main groups in 6 subdivisions. Oil sources are compared on the same basis, which leads to the supposition that the condensates in the pool at Banqiao come from the source rock in No. 3 shahejie Section, while the oil in the pool at Dagang-Tangjiahe has its source in No. 2 and No. 3 Sbahejie sections.

本文研究了黄骅拗陷中区板桥和歧口两个凹陷生油岩的演化特征,将有机质的成熟演化划分为四个阶段;提出该区石油液态窗为85.5~163℃(2000~4200米)。根据烷烃特征,将该区下第三系生油层划分为五种类型,将原油划分为二大类、六亚类。并在上述基础上,进行了油源对比研究,认为板桥凝析油气田的油源来自板桥凹陷沙三段生油岩,而大港油田和唐家河油田的油源来自歧口凹陷的沙二、三段生油岩。

In the evolution of nebular disk to dust layer, the Hpuid grains of material of iron and nickel sank to the epuatorial plane of nebular disk firstly and accumulated , formed the central layer, and the grains of material of chondrite which sank slowly were beside the cetral layer to form the outer layers, because the sinking rates of different dust grains were differet. The planetsimals of material of iron and nickel in the central layer formed the lipuid planetary cores, which then attracted the planetsimals...

In the evolution of nebular disk to dust layer, the Hpuid grains of material of iron and nickel sank to the epuatorial plane of nebular disk firstly and accumulated , formed the central layer, and the grains of material of chondrite which sank slowly were beside the cetral layer to form the outer layers, because the sinking rates of different dust grains were differet. The planetsimals of material of iron and nickel in the central layer formed the lipuid planetary cores, which then attracted the planetsimals of material of chondrite in the outer layers to form the solid planetary mentles and the lateral mass-non-uniformity in the mentle.

星云盘在演化成尘层的过程中,因尘粒沉降速率的不同,使液滴状铁镍物质首先到达并集中于星云盘赤道面,成为中心层,球粒陨石物质分布于中心层上下。中心层的铁镍星子首先形成液态行星核,然后吸积上下层的球粒陨石星子形成固态行星幔,并造成行星幔的横向不均匀。

 
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