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  zone 2
     Dictyograplus wutingshanensis zone, 2).
     Dictyograptus wutingshanensis带,(2).
短句来源
     According to the geographical distribution and vertical variation of fusulinid fauna in the strata, the fusulinid fauna may be distinguished into 3 zones as following (in ascending order). 1) Pseudoschwagerina miharanaensis zone, 2) Sphaeroschwagerina sphaerica zone and 3) Eoparafusulina pararegularis zone.
     根据类动物群在地层中的分布和垂向变化规律 ,自下而上建立 3个化石带 :(1 )Pseudoschwagerina miharanaensis带 ,(2 )Sphaeroschwagerina sphaerica带和(3)Eoparafasulina pararegularis带 .
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  “带(2”译为未确定词的双语例句
     Paraspathognathodus obesus ass. zone,(3). Interval zone A,(4).
     simplex组合带,(2)Paraspathognathodus obesus组合带,(3)A间隔带,(4)Spathogathodus paranassi-S.
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     According to the N-terminal sequence of the 1By HMW-GS, a degenerated primer was designed to amplify cDNA from immature seed ofⅡ-1-3 by RT-PCR. Three segments 2.3kb, 2 2kb and 2.0kb, were obtained.
     依据Ⅱ 1 3中类似 16亚基N端 15个氨基酸序列设计简并引物 ,通过RT PCR扩增Ⅱ 1 3F4 中未成熟胚种子总RNA ,得到三条特异带 (2 .3、2 .2、2 .1kb) ,对其中分子量最大的一条 2 .3kb带谱进行了克隆、测序。
短句来源
     2.Cool-temperate coniferous and broadleaf forest (2*!650~3*!150*!m):1.612*! 6;
     Ⅱ 温凉性针阔叶混交林带 ( 2 6 5 0~ 31 5 0m) 1 6 1 2 6 ;
短句来源
     In the above growing period of winter wheat, it can be divided intothe rare belt of drought frequency (2.5-5), the intermediate-long belt ofdrought frequency (2.5-5) and the usual belt of drought frequency (7.5)according to the drought frequency (still less than 2.5) from the southto the north.
     在上述小麦生育期中,根据干旱频率(级差2.5)从南至北划分为干旱频率稀少带(频率指标1—2.5)、干旱频率中常带(2.5—5)和干旱频率经常带(>5)。
短句来源
     The Walongshan Formation was established then and it is featured by abundant fusulinid. Six fusulinid zones were established as follows:(1)Eostaffella mosquensis zone,(2)Millerella-Eostaffella zone,(3)Pseudostaffella-Eostaffella zone,(4)Profusuliena zone,(5)Fusulina-Fusulinella zone,(6)Protriticites-Triticites zone.
     经研究,自下而上建立6个■类化石带:(1)Eosta ffella mosquensis带,(2)Millerella-Eostaf fella带,(3)Pseudostaf fella-Eostaf fella带,(4)Pro-fusuliena带,(5)Fusulina-Fusulinella带,(6)Protriticites-Triticites带。
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     (2) Isarcicella isarcica zone;
     (2)Isarcicellaparva
短句来源
     (2)Zone of coniferous and broad─leaf mixed forest(1700─2500m).
     (2)针阔混交林
短句来源
     (2)Neogondolella krystyniZone;
     (2 )Neogondolellakrystyni ;
短句来源
     2. It has a rib.
     (2) 肋;
短句来源
     Dictyograplus wutingshanensis zone, 2).
     Dictyograptus wutingshanensis,(2).
短句来源
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  zone 2
Es wird ein neues Verfahren zur Wiederherstellung der Beugesehnenverletzungen in der Zone 2 nach Verdan beschrieben: die Beugesehnenplastik mit Sehnenscheidenbildung aus einer Vene.
      
Most affected islets were found within zone 1 (intratumoral) and zone 2 (peritumoral), to a lesser extent in zone 3 (acini close to tumor) and none in zone 4 (acini remote from tumor).
      
However, zone 2, between the KXK and the Strymon valley, is structurally homogeneous (~ 10° cw rotation).
      
The paleomagnetic signature of the Vertiskos massif (zone 3) implies a larger (>amp;gt; 30°) cw rotation, whereas sites in the Vardar basin (zone 4) contain a paleomagnetic signature similar to that of zone 2.
      
The growth of crystallites occurred in zone 2, which visualized the interface of zones 1 and 2.
      
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Emission and absorption band spectra of sulphur dioxide were studied in the region between 2600 to 2000 A.U. A new system of emission bands (about 150 bands) was found. When these bands were compared with the absorption bands and Mr. Lotmar's fluorescent bands, coincidences were found which amount to 40% and 50% of the total number of absorption and fluorescent bands respectively. These agreements and the very different structure as compared with the SO bands recorded on the same plate made it very probable...

Emission and absorption band spectra of sulphur dioxide were studied in the region between 2600 to 2000 A.U. A new system of emission bands (about 150 bands) was found. When these bands were compared with the absorption bands and Mr. Lotmar's fluorescent bands, coincidences were found which amount to 40% and 50% of the total number of absorption and fluorescent bands respectively. These agreements and the very different structure as compared with the SO bands recorded on the same plate made it very probable that SO2, is the emitter of these emission bands. Evidences were also found that these emission bands arc not the known bands of O2, Oa+ and S2 in the same region. As a further support a vibra-tional level scheme was worked out, using the three fundamental frequencies of the normal SO2, molecule (1150, 525, and 1360 cm-1) in the lower state and 750 and 350 cm-1 (possible also 1110 cm-1) as the frequencies in the upper state. This scheme accounts for 1Q% of the absorption bands, 70% of the emission bands and a small fraction of the fluorescent bands. While the scheme may not be the final due to the complexity of the vibrational formula, one feels fair, as far as the present evidence goes, to conclude that the emission bands observed are actually emitted by the SO2, molecules and that they can be fitted by a vibrational level scheme based on the three known fundamental frequencies of the normal state.

此文目的在报告二氧化硫气体分子之吸收光谱及发射光谱(emission speetrun)之研究光谱区域约在2000A与2600A间有一新组发射光(band)发现。数约百五十在吸收光中有百分之四十之光与此发射光附合。在Lotmar先生之弗光光谱(fluorescent speetrum)中,有百分之五十之光与此发射光附合并此所得之发射光之结构与SO之光显有区别,令人设信此发射光为SO_2分子所发者。在另一方面,找到证据,所得之发射光亦非0_2,O_2~+及S_2诸分子之光谱为求更进一步之证实,试以SO_2之三基本振动数(fundamental frequency)1150,525及1360cm~(-1)为能力阶梯之差而作一常态(normal state)下之能力阶梯。再用750,350cm~(-1)(或1110亦用)为分子在激态(excited state)时之振动数,而作一激态下之能力阶梯所得之能力图(energydiagram)可说明吸收光之70%,发射光...

此文目的在报告二氧化硫气体分子之吸收光谱及发射光谱(emission speetrun)之研究光谱区域约在2000A与2600A间有一新组发射光(band)发现。数约百五十在吸收光中有百分之四十之光与此发射光附合。在Lotmar先生之弗光光谱(fluorescent speetrum)中,有百分之五十之光与此发射光附合并此所得之发射光之结构与SO之光显有区别,令人设信此发射光为SO_2分子所发者。在另一方面,找到证据,所得之发射光亦非0_2,O_2~+及S_2诸分子之光谱为求更进一步之证实,试以SO_2之三基本振动数(fundamental frequency)1150,525及1360cm~(-1)为能力阶梯之差而作一常态(normal state)下之能力阶梯。再用750,350cm~(-1)(或1110亦用)为分子在激态(excited state)时之振动数,而作一激态下之能力阶梯所得之能力图(energydiagram)可说明吸收光之70%,发射光之70%及弗光光之一小部份,此能力图并不完全,故不能望其为最终者。以三原子分子情形复杂,完全正确之分析,尚有待焉。之 能 力唯协所得之能 力 圆 山。。。,。w山。…。。。。\可。Z5t 叫 吸收 几 卅之70九传 时 光排 上 7,%及 比 儿 儿 卅上 一 个 部 份 此 能 力 闲 伙 不 正 全;故个能 望IC iX侦相 许 nt原一户 外 广似形 应 输,完全 正雕之分 析。尚有

Measurement of the intensity of total scattering of x-rays by a number of polyatomic gases was made for scattering angles between 15° and 130 ° using an ionization method of recording the scattered intensity. Balanced filters of ZrO2, and SrO were used to separate the MoKa rays and Soller slits were placed in front of the ionization chamber to obtain a definite scattering angle. The gases studied are CL2, CO2, N2O, H2S, CC14 and CHCl3. In each case the absolute values of the scattered intensity were determined...

Measurement of the intensity of total scattering of x-rays by a number of polyatomic gases was made for scattering angles between 15° and 130 ° using an ionization method of recording the scattered intensity. Balanced filters of ZrO2, and SrO were used to separate the MoKa rays and Soller slits were placed in front of the ionization chamber to obtain a definite scattering angle. The gases studied are CL2, CO2, N2O, H2S, CC14 and CHCl3. In each case the absolute values of the scattered intensity were determined by comparison with the scattering from oxygen, the results of Wollan for the latter gas being taken as correct. The experimental results are actually compared with Woo's theory of the scattering of x-rays by polyatomic gases and the agreement seems to be satisfactory.

吴有训氏最近对于多原子气体散射线之理论,曾作详尽的探讨。吴氏得到一个公式,表示由多原子气体所散射之强度,其中一部为相干的散射,另一部为不相干的散射。 以前关于多原子气体散射X-线之实验,为数甚少,且为定性的结果。最近美人Wollan,对于由O_2及N_2(双原子气体)所散射钼的K_3α线之强度,曾作绝对的度量。Wollan的结果,与吴有训氏的理论,甚属相符。本篇目的,在测定由 Cl_2,CO_2,N_2O,H_2S,CCl_4及 CHCl六种气体所散射X-线之强度,每一实验,均与由0_2者互相比较,根据Wollan的结果,每种气体所散射之绝对强度,皆一一量得。所用之入射X-线为钼之Kα线,系藉Ross的平衡过滤法分出。强度之测量,系用一游离方法。散射角度的范围,自15度至130度。每种气体的实验结果,均与吴氏的理论,互相比较,证明理论与实验,甚属相符。在计算时,原子的“构造因数”,系由Hartree的方法算得,一分子中两原子的相隔距离,则由光谱的结果推得。

With a view to locating the lowast state of trebly ionized cerium, the absorption spectra of CeCl3, and Ce2(SO4)3 solutions are examined between 2,000 A and 10,000 A. While no absorption was found in the long wave length side up to 9500 A, a new broad absorption region was observed, with center at about 2105 A. It is suggested that this and the four other similar absorptions observed by Freed are not related with the transitions which probably lie in a region not yet covered in this study.

本文从理论及实验方面讨论Ce~(+++)之最低能位问题。从CeCl_3及Ce_2(SO_4)_3溶液,除Freed氏已得之四吸收外,在2105A处更薄现一阔而漫之吸收。在红外方面,则直至9500A尚无吸收光线。因各种理由,似可证明Ce~(+++)之4f~2F—5d~2D线,与各紫外吸收无关而应在1至10μ间。

 
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