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     This method can be popularized to other data sampling systems.
     该方法可以推广到其他数据采集系统。
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     Analyzes the theoretical defect of grey prediction formula, and points out that ^X (1) (1) shouldn't be limited as the only known condition when forming the prediction formula. Instead, other data could be used.
     分析 GM(1 ,1 )预测模型存在的理论缺陷 ,指出在形成预测公式时规定 ^ X( 1 ) (1 )为已知条件是不合理的 ,应当根据实际情况选用其他数据 .
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     The possible risk factors were analysed by simple and multiple factors Logistic regression, then the interaction between the risk factors of VSD was analysed by Logistic regression, other data were analysed by χ2 test.
     对 CHD、VSD 类型可能的危险因素进行单因素、多因素 Logistic 回归分析,对筛选出 VSD 的危险因素之间作交互作用分析,其他数据分析作χ2检验。
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     If someone wants to transfer other data,its easy to be done.
     虽然这里只讲述了如何传输文件,但若想利用它来传输其他数据都非常容易实现。
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     By simulation and analysis,it is suggested that this new mechanism can fairly treat VoIP with small packets and other data flows with large packets,and guarantee QoS of VoIP.
     经过仿真和分析,该控制机制将公平地处理携带小分组的语音流和其他数据流,进一步保障了VoIP的服务质量(QoS)。
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     Based on 3-D seismic,drilling data and other data,and by using the theories and methods of high-accuracy sequence stratigraphy,sequence stratigraphic framework has been established in Zhanhua depression,which consists of 1 first-order sequence,4 second-order sequences,17 third-order sequences,51 system tracts,70 parasequence sets and 109 parasequences.
     以钻井、三维地震等资料为基础 ,运用高精度层序地层学理论及方法 ,建立了沾化凹陷层序地层格架 ,划分出 1个一级层序、4个二级层序、17个三级层序、5 1个体系域、70个准层序组和 10 9个准层序。
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     According to the analyses of precipitation, temperature, upper circulation field, ocean temperature and other data( 1959-1999) , the main conclusions can be drawn that the more precipitation in summer of 1999 may relate to the following circulation situations, namely, the strong Ural high ridge, the far north position of west Pacific subtropical high ridge line, the far eastward extending west ridge point of it and the strong intensity of polar vortex.
     利用1959-1999年降水、 气温、 高度场等资料分析得出: 1999年夏季青海省多雨与乌拉尔山高压脊偏强、 西太平洋副热带高压位置偏北及西伸脊点位置偏东、  极涡强度偏强等因素有关。
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     Comparison the result from the conventional well logs and other data on the FMI data, showed a criterion of the gra dation of the fractured carbonate formation, and classified the formation into three grades,and it lays a solid foundation for the prediction of the reservoir productioa
     通过与常规测井等资料的对比,建立了储层分级标准,并利用FMI测井资料对储层进行了分级。 多口井的应用结果表明,利用FMI成像测井资料对缝洞型储层的评价结果与录井油气显示和测试结果较吻合。
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     According to the component and carbon isotope characteristics of natural gas and combining with organic matter types,thermal evolutionary stages and other data of hydrocarbon source rocks, natural gas was classified into bacteriogenetic gas, bacterialmature oiltyped gas,low mature coaloiltyped gas,mature oilcoaltyped gas,coaltyped gas and other six genetic types.
     根据天然气组分与碳同位素特征并结合烃源岩有机质类型及热演化阶段等资料,将天然气分为细菌气、细菌-成熟油型气、低熟煤型-油型气、成熟油型-煤型气、煤型气等6种成因类型。
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     There are different growth rates among individuals in a population,therefore we may separate the samples into population depending on the age,capture time and other data in the course of the study,then determine their growth of various groups.
     头足类的年龄与生长研究是一个极为复杂的生物学问题,同一种类不同种群个体之间生长差异明显,因此,在以后的研究过程中,可以根据年龄、捕获日期等资料先分种群,然后按各种群分别研究其生长特性。
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     Comparing with other data conversion models,a data conversion model was proposed using xml file as transportation media,named DCMHD(Data Conversion Model of Heterogeneous Database).
     在参考了其他数据转换模型的基础上,提出了基于XML文件的数据转换模型DCMHD(Data Conversion Model of Heterogeneous Database)。
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     Results(REE/Wt and) TNF-α were closely correlated(r=0.34693,P=0.0328). A correlation trend could be found between REE/BA and TNF-α(r=0.31902,P=0.0509),and there were no significant correlations between REE,REE/Wt,REE/BA and some other data such as pulmonary functions.
     结果REE/W t与TNF-α高度相关(r=0.34693,P=0.0328),REE/BA与TNF-α有相关性趋势(r=0.31902,P=0.0509),而REE、REE/W t、REE/BA与肺功能等各项指标无显著相关性(P>0.05)。
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     The advancement in ensemble-based data assimilation methods are reviewed,including Ensemble Kalman Filter(EnKF),Ensemble Kalman Smoother(EnKS),Ensemble Square-Root Filter(EnSRF),Singular Evolutive Extended Kalman Filter(SEEK). The main characteristics are outlined though comparing them with other data assimilation methods.
     综述了包括集合卡尔曼滤波(EnKF,Ensemble Kalman Filter)、集合卡尔曼平滑(EnKS,Ensemble Kalman Smoother)、集合方均根滤波(EnSRF,Ensemble Square-Root Filter)和减秩卡尔曼滤波(SEEK,Singular Evolutive Extended Kalman Filter)等集合数据同化方法的研究进展状况。
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     then derives formula for computing target motion elements and projectile fir-ing data using Ω_s、Ω_L and other data(i.e.q_I、ε、D、V_W、K_W)while hi-gh-speed solution Can not be implemented.
     并利用Ω_s、Ω_L 和有关数据(qw,ε、D、■、V_w、K_w)推导出在不满足“快解”条件时计算目标运动要素和弹丸发射诸元的计算公式。
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     Adopt the method of“shuang pai bu jin”to adjust the valve clearance data which are 0.15 mm,0.25 mm,0.35 mm and 0.45 mm. Among those data, normal clearance is 0.15mm, using the other data to simulate abnormal state of valve clearance.
     采用双排不进的气门间隙调整法将气门间隙调整为0.15mm、0.25mm、0.35mm和0.45mm,其中0.15mm为正常间隙,用其它的数值模拟气门间隙异常。
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The same type of polymorphism has been detected in samples of different tissues of the same person, so these variants are considered (also based on other data) to be allelic.
      
In light of the data on the topology of the 16S rRNA-based phylogenetic tree and some other data, this review discusses the probable hyperthermophilic nature of the universal common ancestor.
      
Other data show that penta-(A-T) oligonucleotide adsorbed via a covalently bound thiol linker also displays reductive desorption and in situ STM to molecular resolution.
      
This trough could explain the gap in the Galactic HI distribution observed near the solar circle and can be used to locate the corotation region if combined with other data.
      
The detection of radio emission from these two AXPs, together with other data, suggests the need to revise the radio-emission mechanisms in the magnetar model or the magnetar model itself.
      
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The purpose of this series is to make a thermodynamic analysis of the Fe-C system with a minimum of assumptions and to revise the equilibrium diagram of the same system in the light of the results of this investigation. In this paper, the first of the series, activities in liquid Fe-C alloys have been evaluated up to saturation, using Richardson and Dennis' data123 on dilute solutions of carbon in liquid iron and Darken and Smith's model~([1]) for carbon dissolved in austenite with certain modifications.A parameter...

The purpose of this series is to make a thermodynamic analysis of the Fe-C system with a minimum of assumptions and to revise the equilibrium diagram of the same system in the light of the results of this investigation. In this paper, the first of the series, activities in liquid Fe-C alloys have been evaluated up to saturation, using Richardson and Dennis' data123 on dilute solutions of carbon in liquid iron and Darken and Smith's model~([1]) for carbon dissolved in austenite with certain modifications.A parameter α_c defined as logγc/N_Fe~2 with reference to graphite as the standard state is plotted against N_c for both austenite and Fe-C melt in order to facilitate the evaluation of α_(Fe) by graphical integration. Smith's data~([1]) on equilibrium between austenite and gaseous mixtures (CO_2/CO, CH_4/H_2) are re-treated to yield α_c~γ-N_c~γ curves for 800° and 1000℃ as shown in Fig. 1. On the assumption that L_c~γ the relative partial molal enthalpy of carbon in austenite, does not chan preciably with temperature, the α_c~γ-V_c~γ curve for 1153℃, the iron-graphite eutectic temperature, is obtained by extrapolation and found to lie above the graphite saturation point. This fact seems to indicate that the limit of application of Darken and Smith's model is reached somewhere around N_c~γ=0.0661 (1.50%) and a point of inflection should occur at this concentration. The above-mentioned assumption has been semi-quantitatively proved in this paper and will be discussed further in another paper of this series.In a similar manner, α_c~l-N_c~l curves for liquid Fe-C alloys are drawn through the experimental points of Richardson and Dennis on equilibrium between CO_2/CO mixed gases and dilute solutions of carbon in liquid iron at 1560° and 1660℃ as shown in Fig. 1. The curves are extended up to N_c~1=0.15 on the basis of Darken and Smith's model using 3600 cals. as the energy of interaction at 1560℃ between carbon atoms in the neighbouring interstitial sites as recommended by Richardson and Dens. Then, a suitable curve is drawn between N_c~l=0.15 and the graphite saturation point for 1560℃ to meet certain requirements, and a corresponding curve for 1660℃ is obtained by extrapolation, assuming that L_c~l, the relative partial molal enthalpy of carbon in liquid iron, does not change appreciably with temperature. Thus, α_c~l-N_c~l curves for 1560° and 1660℃ are completed from low carbon concentrations up to saturation. The activities of carbon in Fe-C melts at 1600℃ with reference to graphite as the standard state are readily obtained at different carbon concentrations by interpolation, from which the reversible electromotive forces of a concentration cell of the type Fe,C|slag, C_2~2|Fe,C(sat.) have been calculated and found to agree fairly well with the experimental values obtained by and as shown in Fig. 2. This agreement may be taken as partial confirmation of the choice of N_c~l=0.15 as the limit of application of Darken and Smith's model to liquid Fe-C alloys.From α_c~l-N_c~l curves for 160°and 1660℃, L_c~l is easily calculated to be 3930 cals., and by combining this value with certain other data, the following equation is obtained:C(gr.)=C[%]; AF°=3930-9.21 T,which differs considerably from Chipman's equation AF°=8900-12.10T given in the 1951 edition of the "Basic Open Hearth Steelmaking". It is believed that the present author's equation is more reliable than Chipman's in view of the uncertainties involved in the derivation of the latter especially regarding the evaluation of the enthalpy of solution of graphite in liquid iron.By graphical integration of the Gibbs-Duhem equation, the activities of iron in Fe-C melts with pure liquid iron as the standard state are obtained at different carbon concentrations and plotted against N_c~l in Fig. 3. The α_(Fe)~l-N_c~l curve thus obtained is independent of temperature. With the aid of Fig. 3 and certain other data, the activities of iron in an Fe-C melt and austenite both saturated with graphite at the eutectic temperature are evaluated with pure γ iron as the common standard state and found to be practically equal as required by the eutectic equilibrium. This fact renders additional support to the choice of N_c~l=0.15 as the inflection point of the α_c~l-N_c~l curves.The shape of the α_c~l-N_c~l curves is briefly discussed from a structural viewpoint.

作者在本文中综合分析了关於液态铁碳合金中碳活度测定的諸家研究结果並比较其优劣. 然后根据Richardson与Dennis用CO_2/CO平衡法的实验数据,用Darken与Smith的统计模型与最少假定,导出了液态鉄碳合金中α′_c与N′_c的关系(α′_c=logγ′_c,/(N_Fe′)~2,标准状态为石墨),并温度对此关系的影响.计算结果符合於(i)鉄液内石墨溶解度的实验数据;(ii)与用电动势法测定液态铁碳合金中碳活度的实验数据;及(iii)奥氏体、铁液、石墨共晶平衡的要求. 根据本文所导出的α′_c-N′_c曲綫,作者算得石墨在鉄液内的溶解热为3930卡;然后依此及其他必需数据,导出下列关系:C(石墨)=C[%],△F°=3930-9.21T. 最后作者从液态铁碳合金结构的观点讨论了图1中α′_c-N′_c曲綫的形状.

Concluding this series on thermodynamic study of the Fe-C system,the presentpaper deals with an analysis of the metastable iron-cementite equilibrium on thebasis of the activity data derived previously by the author and the free energy ofcementite recalculated by the author in this paper.It has not been possible before to calculate the cementite eutectic temperaturedue to lack of data on activities in the liquid iron-carbon system.With the aid of the results of calculation in a previous paper,this temperature...

Concluding this series on thermodynamic study of the Fe-C system,the presentpaper deals with an analysis of the metastable iron-cementite equilibrium on thebasis of the activity data derived previously by the author and the free energy ofcementite recalculated by the author in this paper.It has not been possible before to calculate the cementite eutectic temperaturedue to lack of data on activities in the liquid iron-carbon system.With the aid of the results of calculation in a previous paper,this temperature has been found tobe 1148°,or 5° below the graphite eutectic temperature.The cementite eutectoidtemperature 723°,determined by Mehl and Wells,is found to be consistent withthermodynamic requirements.Darken and Gurry chose 1146° as the cementite eutectic temperature andwith this value and certain other data calculated the free energy of cementite as afunction of temperature.On the basis of the more rigorously calculated cementiteeutectic temperature 1148° and the carefully determined cementite eutectoid tempe-rature 723° and certain other data,the free energy of cementite has been recal-culated by the author and found to be considerably different from Darken andGurry's results.The solubilities of cementite in austenite and in liquid iron respectively arethen calculated as functions of temperature.It should be pointed out,however,thatthe solubility of cementite in liquid iron thus calculated is only a first approximationand will certainly be revised in the future when more data on the free energy ofcementite at higher temperatures become available.A complete Fe-C equilibrium diagram including both stable and metastableequilibria has been constructed in the light of the results of this and a previouspaper.It is easily seen that certain important differences exist between the conven-tional and the revised diagrams.

在本文中,作者首先计算了铁、碳化铁的共晶平衡,得出共晶温度为1148°;这在以前因为缺乏液态铁碳合金内的活度数据是不可能计算的。其次作者综合分析了前人数据,主要根据1148°的介稳共晶温度及723°的介稳共析温度,算出碳化铁的热力学函数。根据这样算出的碳化铁热力学函数及有关热力学数据,作者(i)复核了碳化铁的共析温度及共析点成分;(ii)计算了碳化铁在奥氏体内的溶解度;(iii)计算了碳化铁在铁液内的溶解度及碳化铁液相线与石墨液相线的相交温度。最后,根据本文及稳定平衡部分的计算结果,作者将现行铁碳相图加以修正,俾合于热力学的要求。但关于碳化铁在铁液内溶解度的计算仅属于初步近似性质,有待将来研究。

The annual cycle of the golden cuttlefish,Sepia esculenta,one of the mast important economic cephalopods distributed in yellow sea,has attracted much attention of the observers in the past.With an attempt to throw light on this subject,the authers had a series of studies on the breeding,development and migration of this animal carried out in the years 1955-1959.The present paper is an account of the main results of them.The BreedingIn from late spring to early summer golden cuttlefishes,after making a long journey...

The annual cycle of the golden cuttlefish,Sepia esculenta,one of the mast important economic cephalopods distributed in yellow sea,has attracted much attention of the observers in the past.With an attempt to throw light on this subject,the authers had a series of studies on the breeding,development and migration of this animal carried out in the years 1955-1959.The present paper is an account of the main results of them.The BreedingIn from late spring to early summer golden cuttlefishes,after making a long journey from the place where elapses thier juvenile time,arrive at many localities in the coastal regions of yellow Sea,of which the northern-most.one on China coast is near the mouth of Yalu Revier,the southern-most a little way off the shore of Lanshantow,a town lying on the southern boundary of Shantung Pennisula.At these localities they group together at the sea bottom,either sandy or mud- sandy,usually of 5-15m.below the surface and spawn.Evidence has been present to show the fact that,along the coast between Tsingtao and Lanshantow,the more northward the spawning place is,the later the spawning season begins,and the factors exert-ing influence over this are water temperature,salinity,strength and direction of the wind.Surveying the record of observations made on the specimens kept in aquaria and within special cages placed in the sea,it is evident that the behavior of the golden cuttlefish during reproduction and egg-laying is similar to that of sepia officinalis,but different in some respects with that of Sepiella maindroni.The species here studied,like Sepia officinalis,has only one method of copulation,for which the famale and the male come head to head with thier arm interdigit-ating for 22-8 minutes.In the course of twenty four hours,the same individuals may copulate over ten times.Four series of experiment were made to determine the rate of ripeness of the ova located in different parts of the oviduct of golden cuttlefish.Result of these experiments clearly proved that the ripening of the ova is quick at the onset of spawning,but becomes slow with advence of season.The females lay thier eggs mostly at the sun set and after the midnight,tying them with thier outer sheaths on the net of the trap set in fishing place,the eggs develope there into young animals in 25-48days at 150°-26.0℃.About the fate of spawned individuals of both sek which has long been a question of interest,a discussion is given in this paper,based upon fishing records and other data concerned.The MigrationThis comprises the inshore migration ot adult and the offshore migration of young.According to data obtained from periodical collections,the time,when the young animals born and bred in Chiao-chow Bay leave the breeding place,may last three months,from July to October.Evidently this duration is in no small measure longer than those existing in other localities along the southern coast of Shantung Pennisula.The authers,therefore,suggest that the geographical fea- ture of the coast has also relation to the annual life of the golden cuttlefish.What by investigations,and what by analysis of the voluminous fishing records obtained from fisheries bureaus,the authors found out that the autumn months and the early winter of the same year belong to the migrating period of the yonng,while the April and May of the next year that of the adult.Between these two periods,that is to say,from Eebruary to March is the winter-passing period of the young,during which it lives in the deep layer and grows up to adult.In this period most individuals of dffterent size stay at a region off Chengshan-Kiao.As shown on the relevant chart,the exact position of it is between 122°30'-123°50'E and 38°.00-33°.30'N.To summarile up,the annual life of the golden cuttlefish may be referred to four arbitrary,but readily distinguished,periods,namely,breeding,inshore migration,offshore migration and winter-passing.

一、金乌贼是一种严格的洄游性动物。其洄游的目的是为了寻找适合于生殖和卵子发育的场所。据此,金乌贼的洄游乃是生殖洄游。 二、由于受着洄游方式的规定,金乌贼全年内的生活共分为四个时期,即:成体由越冬场向产卵场的洄游期,成体在黄渤海沿岸的结群期,新一代幼体自产卵场向越冬场的洄游期和幼体在越冬场内的生长发育期。 三、金乌贼在我国黄渤海沿岸结群的地区很广,北起鸭绿江口,南至山东岚山头。其结群开始时间在不同地区容有差别,但就—地来说,却相当恒定。 四、通过标志放流和野外观察证实了:金乌贼在结群期不但有留恋产卵场而不离岸的情况,同时还有喜欢入笼产卵的习性。 五、就初步分析,沿岸风向、盐度和水温等自然条件的变化,都对金乌贼的结群起有一定影响。沿岸地貌条件特别对结群历时有显著的影响。 六、从结群开始到结束,金乌贼的平均体重、体长和体围有逐渐减小的现象。以胶州湾为例,结群结束时期的平均体重尚不及其开始时期平均体重的一半。 七、在历年结群时期,金乌贼雌雄比例并不是恒定的,有时两者非常接近,有时雄多雌少。雌体过多于雄体的现象,在胶州湾内尚未发现。 八、金乌贼雌雄个体的交配,不但持续于整个结群期,并且在一日内也是很频繁的。在几个个体同...

一、金乌贼是一种严格的洄游性动物。其洄游的目的是为了寻找适合于生殖和卵子发育的场所。据此,金乌贼的洄游乃是生殖洄游。 二、由于受着洄游方式的规定,金乌贼全年内的生活共分为四个时期,即:成体由越冬场向产卵场的洄游期,成体在黄渤海沿岸的结群期,新一代幼体自产卵场向越冬场的洄游期和幼体在越冬场内的生长发育期。 三、金乌贼在我国黄渤海沿岸结群的地区很广,北起鸭绿江口,南至山东岚山头。其结群开始时间在不同地区容有差别,但就—地来说,却相当恒定。 四、通过标志放流和野外观察证实了:金乌贼在结群期不但有留恋产卵场而不离岸的情况,同时还有喜欢入笼产卵的习性。 五、就初步分析,沿岸风向、盐度和水温等自然条件的变化,都对金乌贼的结群起有一定影响。沿岸地貌条件特别对结群历时有显著的影响。 六、从结群开始到结束,金乌贼的平均体重、体长和体围有逐渐减小的现象。以胶州湾为例,结群结束时期的平均体重尚不及其开始时期平均体重的一半。 七、在历年结群时期,金乌贼雌雄比例并不是恒定的,有时两者非常接近,有时雄多雌少。雌体过多于雄体的现象,在胶州湾内尚未发现。 八、金乌贼雌雄个体的交配,不但持续于整个结群期,并且在一日内也是很频繁的。在几个个体同在一起的情形下,它们,特别是雄

 
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