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   阶段温度 的翻译结果: 查询用时:0.191秒
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阶段温度
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  sub stage
     the substage of partial retrograde metamorphism, 629-776℃ and 1.2-1.6 GPa;
     部分退变质阶段温度为629~776℃,压力1.2~1.6Gpa;
短句来源
     the substage of retrograde metamorphism, 550-650℃ and 0.5-0.7 GPa;
     退变质阶段温度为550~650℃,压力0.5~0.7Gpa;
短句来源
     the substage of strong retrograde metamorphism, 300-400℃ and 0.30-0.35 GPa.
     强退变质阶段温度为300~400℃,压力0.30~0.35Gpa。
短句来源
  “阶段温度”译为未确定词的双语例句
     Fluid inclusion research and thermodynamic calculations indicate that the depositing temperature was from 150℃ to 370℃ and that the pressure was from 3.7×10~7Pa to 5.0×10~7Pa, with a depositing temperature of 250℃ and a pressure of 5.0×10~7Pa at the major stage of mineralization.
     流体包裹体及热力学计算表明:成矿温度在150~370℃,压力为3.70×10~7~5.00×10~7Pa,主成矿阶段温度在250℃,压力为5.0×10~7Pa;
短句来源
     Temperature and concentration of P_(2)O_(5) in PPA are important factors for this reaction. Temperature shouldn't exceed 120℃ during the process of removing HCl,and the maximum yield is 88% when the concentration of P_(2)O_(5) in PPA is 84%.
     温度以及多聚磷酸中P2O5的浓度是合成反应的重要影响因素,在脱HC l阶段,温度不能超过120℃,P2O5含量为84%时的产率最高(88%)。
短句来源
     The ore forming temperature is 200°C±.
     成矿流体研究表明主要成矿阶段温度为200°C±;
短句来源
     Reaction temperature is 15°C around, PH value of solution is 9~10, amount of air is 0.1m~3/h and density of ferrous sulfate are the best factors in the course of production of inoculating crystal.
     (1)晶种制备阶段,温度15℃左右,PH值9~10,空气通入量为0.1m~3/h,硫酸亚铁浓度为 20g/l。
短句来源
     The measured temperature data of fluid inclusions show that gold deposit is featured with low temperature(133℃~276℃),δ~(18)O_(H_2O) values of quartz from-0.2‰ to-7.0‰,δD__(V-SMOW) values of quartz from-63‰ to-85‰.
     δD值为-63‰~-85‰,1δ8O水值为-0.2‰~-7.0‰,主成矿阶段温度为133~276℃。
短句来源
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  相似匹配句对
     T is temperature, ℃.
     T为温度,℃。
短句来源
     The optimum temperature is 20℃C in first-step reaction.
     第一阶段最佳反应温度为20℃;
短句来源
     Temperature and time in different heating phases were also fixed.
     确定了烧成工艺的各个阶段温度和停留时间。
短句来源
     Measure of Temperature
     温度的测量
短句来源
     Finally, it is the phase of historism.
     历史主义阶段
短句来源
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  sub stage
Sub stage I began immediately after the intrusion of the pluton into the enclosing impure carbonates.
      


Regarding the temperature of cocoon drying, heat supplying temperture was generally used in the past owing to the inadequacy of the thermoscope4: And the temperature of the heated body was usually deficient. In this experiment, we measured the cocoon layers, pupa shells and hearts of the heated bodies in the processes of drying with modern transistor thermoscopes Through several measurements of the inside heat supplying in 1964-1965, 1975, we have got a few data. In general, a formula may be formed as: wall...

Regarding the temperature of cocoon drying, heat supplying temperture was generally used in the past owing to the inadequacy of the thermoscope4: And the temperature of the heated body was usually deficient. In this experiment, we measured the cocoon layers, pupa shells and hearts of the heated bodies in the processes of drying with modern transistor thermoscopes Through several measurements of the inside heat supplying in 1964-1965, 1975, we have got a few data. In general, a formula may be formed as: wall temperature >room temperature >pupa temperature > layer temperature. In the past the highest temperature of drying was controlled below 100? but now it may be raised on to 120癟his experiment, in practice indicates the rational ity of the raising of temperature. In add'tion, with the gradual development of the drying degrees, the temperature of the cocoon layer and the pupa body rises. The temperature risiing in the cocoon layer is higner than that in the pupa body. Attention musto be paid to the grasp of the temperature in the later stage, especially to the final temperature.

对于烘茧温度,过去由于测温仪器的局限性,一般用的都是给热温度。至于受热体的温室,基本缺如。本试验应用现代的半导体测温仪器,对受热体蚕茧的茧层和蛹皮、蛹心,行烘茧进程中的温度实测。经1964、1965和1975年的几次测定,于内部予热式烘茧,初步摸索了一些数据,大体为壁温>室温>蛹温>层温的概念。过去烘茧最高温度规定100℃,现在又提可达120℃,这次试测,就从实践上说明了提高温度的合理性。又在烘茧中,随着干燥程度的逐步发展,茧层温度和蛹体温度就比例上升,茧层温度的上升比又大于蛹体,这是掌握后阶段温度特别是最后温度时特别应该注意的。

The Beishicheng and Hefangkou fault zones in Miyun and Huairou area have been studied. A mylonite belt tens to hundreds meters in width was developed on the foot wall of the former fault and a fracture belt 300-500 meters in width on the hanging wall. A mylonitized granite belt occurred on the foot wall of the latter fault and cataclasites or cataclastic granite on the hanging wall.Microscopically quartz and mica ,within mylonites exhibit their features of strong plastic deformation indicated by apparent flow...

The Beishicheng and Hefangkou fault zones in Miyun and Huairou area have been studied. A mylonite belt tens to hundreds meters in width was developed on the foot wall of the former fault and a fracture belt 300-500 meters in width on the hanging wall. A mylonitized granite belt occurred on the foot wall of the latter fault and cataclasites or cataclastic granite on the hanging wall.Microscopically quartz and mica ,within mylonites exhibit their features of strong plastic deformation indicated by apparent flow structure and grain size reduction due to dynamic recrystallization. All minerals in the cataclastic rocks, however, display brittle behaviour. It is clear that the two kinds of rocks were formed under different physical conditions.Based on the distribution pattern of the fault rocks and dynamic analysis of twin lamellae of dolomite, it can be inferred that there were two phases during the develop-ement of the fault zones: a ductile shearing occurred at the deeper level of the crust leading to the formation of mylonite belts, and then the mylonite belts gradually were uplifted along the south-eastern sides of the fault zones onto the higher level.According to the mineralogical assemblage and the characteristic of the mylonites, it is deduced that the ductile shearing occurred at temperature of 450-500°, and confining pressure of about 4 kb, corresponding to the depth of 15 km. A differential stress value of 0.5-1 kb and a strain rate of 1.6 × 10-9-10-10 sec-1 have been estimated from rescrytallized grain size, subgrain size, dislocation density and the spacing of deformation lamellae of quartz revealed in chemically etched mylonite samples.Finally, the possible relationship between ductile shear belt, the elastic-plastic transition zone within the crust and the layer feasible to shake in continent has been discussed.

本文论述了糜棱岩类与碎裂岩类的变形特征,它们各自代表了不同的成因机制,反映了断层带经历过早期韧性剪切和后期脆性破裂的发育历史。根据断层岩石的显微构造特征,估算了断层带发育过程中两个阶段的温度、压力、应变速率、差异应力大小和方位,并讨论了韧性剪切带、地壳中弹塑性过渡带与大陆地震多发层之间的关系。

The relation between the technological conditions of cocoon drying process and the quality of cocoons has been studied in this paper with the cocoon drying machine designed and made by ourselves. It has been pointed out that the one-step drying system is superior to the two-step one, with which their quality will be decreased. The main factors that affect the neatness of cocoons are the half-dry recovery effect and the ralitive humidity in the later drying stage and the proper temperatures in the earlier drying...

The relation between the technological conditions of cocoon drying process and the quality of cocoons has been studied in this paper with the cocoon drying machine designed and made by ourselves. It has been pointed out that the one-step drying system is superior to the two-step one, with which their quality will be decreased. The main factors that affect the neatness of cocoons are the half-dry recovery effect and the ralitive humidity in the later drying stage and the proper temperatures in the earlier drying stage should be further tested within the temperature range from 110 ℃ to 125℃.

本文用自行设计、制造的蚕茧干燥设备对蚕茧干燥工艺条件与茧质关系问题作了初步探讨。指出:与一次干法相比,采用二次干法将使夏秋茧茧质下降;影响净度成绩的主要因素是半干还性效果及后阶段相对湿度;适当的前阶段温度应在110~125℃之间作进一步试验。

 
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