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温度判断
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  temperature estimation
     40Ar/ 39Ar chronological study was undertaken on hornblende and biotite from the mylonite in this work. A plateau age of 143.3±1.3 Ma, Early Cretaceous, was obtained from the hornblende sample N14. Deformation temperature estimation suggests that this hornblende age represents deformation time related to the sinistral movement.
     通过对该段走滑糜棱岩中角闪石与黑云母的40Ar/39Ar年代学研究,本次工作中获得了一个角闪石(N14)的40Ar/39Ar坪年龄为143.3±1.3Ma(早白垩世初),据变形温度判断其代表了该断裂带左行平移中的变形年龄。
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  “温度判断”译为未确定词的双语例句
     The Feasibility Research of Judging the Blast Furnace Thermal State by Tuyere Flame Temperature
     用风口燃烧温度判断高炉热状态的可行性研究
短句来源
     Judgment of Degree of Shaft Damage of Blast Furnace for Phosphatic Fertilizer from External Wall Temperature
     由外壁温度判断磷肥高炉炉体的破损程度
短句来源
     Research on raw coal gas temperature to judge final coking time
     用粗煤气温度判断结焦终了时间的研究
短句来源
     Utilizing the characteristic of temperature sensor that resistance of temperature sensor varier with temperature, supplying constant current driving and measuring the voltage of each RTD to obtain the resistance, then calculating the temperature of this point where this RTD is located.
     本设计利用温度传感器阻值随温度变化的特性,对Pt100阵列提供恒流激励,然后测量每个RTD上的电压,求出其阻值以得出该RTD所处点的温度,判断是否位于液氮液面以下。
短句来源
     In addition,the maximum palaeotemperature of Ordovician carbonate reservoir underwent was approximately140-160℃ by means of the geothermometer of dickite.
     此外.据该地开石形成温度判断,奥陶系碳酸盐储层所经历的最大古地温为140~160℃。
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  相似匹配句对
     T is temperature, ℃.
     T为温度,℃。
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     The Temperature Controller in High-accuray Quartz Crystal Oscillator
     温度控制电路
短句来源
     Research on causality judgments
     因果关系的判断
短句来源
     The Judgement of Danger
     危险的判断
短句来源
     Research on raw coal gas temperature to judge final coking time
     用粗煤气温度判断结焦终了时间的研究
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  temperature estimation
OES analysis in a nonthermal plasma used for toxic gas removal: Rotational and excitation temperature estimation
      
The accuracy of true temperature estimation versus a number of unknown parameters of a body emissivity model and quantity and the width of spectral bands as well are investigated by means of the "quasi-real" experiments.
      
Temperature estimation by oxygen-stable record over the past 200 ka in Zoigê basin
      
Empirical garnet-orthopyroxene barometry at least in the system CMAS can be formulated to obtain a pressure estimate without previous temperature estimation (P(kb)=34.4-19.175 1n XAlM1+17.702 1n XCaM2).
      
Finnerty and Boyd (1984, 1987) found that many independent thermometers yield similar P-T arrays, so that features of xenolith geotherms cannot be artifacts of the method of temperature estimation.
      
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The effect of different molecular weight and adding quantity of PEG on the compatibility of PET/PEG blend was investigated by DSC method.Experiment shows that it is impossible to determine the compatibility of these two components in given system by determining whether two T_g are existed.It can be decided from the temperature of

用差示扫描量热法(DSC)研究了不同分子量和加入量的PEG 对与PET 共混时共混物相容性的影响。实验得知,此体系不能用两个T_g 的方法来判断二者的相容性。由熔融峰的温度判断,PET 和PEG 的晶相是不相容的。在共混物的无定形区,PEG 的加入使PET 的T_g 下降10℃左右,使PET 的冷结晶温度降低10~20℃,热结晶温度升高16℃左右,表明PEG 显著影响PET 无定形区的性质,所以在无定形区有部分相容性。部分相容的程度与PEG 的分子量有关,PEG 分子量小,相容程度就大。PEG(M=20000)在加入量6%时,有DSC 可检测的PEG 熔融峰,而PEG(M=2000)在加入量为20%时仍未出现熔融峰。

There are a number of kaolinite subgroup clay minerals in the Ordovician carbonate sediments of Shaanganning Basin. They were studied by scannins electron microscopy, X-ray powderdiffraction,infrared absorption spectroscopy and differential thermogram analysis and comfirmed thatthiS kind of mineral is dickite and not kaolinite. Since depth-dependent transformation of kaolinite todickite needs acidic diagenetic agent,the present dickite indicates the activity of relatively acidic porefluid during diagenesis....

There are a number of kaolinite subgroup clay minerals in the Ordovician carbonate sediments of Shaanganning Basin. They were studied by scannins electron microscopy, X-ray powderdiffraction,infrared absorption spectroscopy and differential thermogram analysis and comfirmed thatthiS kind of mineral is dickite and not kaolinite. Since depth-dependent transformation of kaolinite todickite needs acidic diagenetic agent,the present dickite indicates the activity of relatively acidic porefluid during diagenesis. Under this condition,calcite and dolomite rich in iron and manganese sealingoff most of the porosity could not precipitate. So,dickite is an indicator of good reservoirs. In addition,the maximum palaeotemperature of Ordovician carbonate reservoir underwent was approximately140-160℃ by means of the geothermometer of dickite.

陕甘宁盆地奥陶系碳酸盐古风化壳天然气储集层中存在丰富的高岭石族矿物,经扫描电镜观察、单矿物样的X射线衍射、红外吸收光谱及差热分析,确认为地开石,而不是高岭石。由于地开石的存在反映酸性的成岩介质,这不利于作为孔隙封堵物的高铁、锰方解石和白云石的沉淀,而有利于碳酸盐矿物的溶解,对埋藏成岩过程中储层孔隙的保存与发育极为有利;同时由于地开石的分子体积小于高岭石,高岭石向地开石的转化会有多余的孔隙空间出现.并形成更多的晶间孔隙,因而地开石通常是好储层的指示矿物。此外.据该地开石形成温度判断,奥陶系碳酸盐储层所经历的最大古地温为140~160℃。

After analyzing some ways of estimation of the end of coking,three ways to decide the ending of coking by the temperature of the raw gas are p ut forward.And the model of the cokin g index is adopted,which is applied through the programme in the coke ove n automatic heating control system.

在研究了各种判断结焦终了时间的方法后,提出了用粗煤气温度判断结焦终了时间的三种方法,并采用结焦指数模型,在焦炉加热自动控制中通过编程得到应用。

 
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