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     and the rate of hyper triglyceride of the male is 21.53%,while it is 13.98% with the female.
     结果表明,男性和女性血糖异常率分别为5.09%和3.95%,男性和女性甘油三酯症的检出率分别为21.53%和13.98%,均为男性于女性;
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     Results: The frequency of hypertension, hyperglycemia, hyper triglyceridemia and low high density cholesterol were 49.1%, 47.3%, 28.1% and 12.1%, respectively.
     结果:血压、血糖、甘油三酯及低密度脂蛋白胆固醇血症发生率分别为49.1%,47.3%,28.1%及12.1%。
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     Study on the New High-performance Link Technology:Hyper Transport
     新型性能互连技术Hyper Transport研究
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     Results (1) Hyper LDL C,low HDL C are the key types in this pasturing area, the former prevalence was 51.0% and 32.1% among the male and female;
     结果(1)LDL-C、低HDL-C血症为该牧区人群血脂异常的主要类型,前者患病率男女性组分别为51.0%,32.1%(χ2=39.50,P<0.01);
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     Apparent diffusion coefficient (ADC), relative ADC (rADC) and the area of hyper intensity on DWI and T 2WI were measured.
     计算各时间点的DWI和T2 WI上的异常信号面积及兴趣区的表观弥散系数 (ADC)值及相对ADC值 (rADC)。
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  “hyper”译为未确定词的双语例句
     Method:The Hyper sil ODS2 C18 column (150 mm×4.6 mm,5μm)was used.
     方法:用HPLC法测定,色谱条件:Hypersil ODS2 C18分析柱(150 mm×4.6 mm,5μm);
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     Research on the Process of (Zn-Ni)/Al_2O_3 Composite Deposition with the Aid of Hyper Dispersant
     超分散剂对(Zn-Ni)/Al_2O_3复合镀工艺的影响
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     Improvement on Properties of Z type Planar Hexaferrite Ba 3Co 2Fe 24 O 41 Materials in Hyper frequency Range
     Z型Ba_3Co_2Fe_(24)O_(41)软磁铁氧体性能的改善
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     An immune evolution algorithm CHIEA(Clonal selection and hyper mutations based immune evolution algorithm) is proposed for solving deterministic job shop scheduling problems. The algorithm is based on clonal selection and hyper mutations.
     基于克隆选择原理与细胞超变异思想构造了一种免疫进化算法CHIEA(Clonal selection and hyper mutations based immune evolution algorithm)求解静态JSP问题(Job shop scheduling problem)。
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     When preparations were superfused with NA (10~(-4)--10~(-3)mol/L), the changesof Rp were as follows: (1) hyper polarization, with amplitude of 8.38±1.42mV(X±SE) (20/48);
     当灌流液中滴加10~(-4)-10~(-3)mol/L去甲肾上腺素(NA)引起如下的膜电位改变:(1)超极化:幅值8.38±1.12mV(x±SE)(20/48);
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     Hyper Design
     超设计
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     On Hyper Semiring
     超半环
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  hyper
On the hyper-order of meromorphic solutions of linear differential equations
      
In this paper the order and the hyper-order of the solutions of higher-order homogeneous linear differential equations is investigated.
      
In this paper, the precise estimation of the order and hyper-order of solutions of a class of three order homogeneous and non-homogeneous linear differential equations are obtained.
      
Physiological response of riparian plants to watering in hyper-arid areas of Tarim River, China
      
(herb species) to variations in water and salinity stress were studied in the hyper-arid environment of the Tarim River in China.
      
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Ⅰ. General SKETCH The Cenozoic basalt lavas are widely distributed along the coastal regionand its adjacent districts in eastern China. They form either widespread plateausor scattered mesa-like hills; and, in some places, the volcanic craters are stilladmirably preserved to-day. These basalt sheets were erupted extensively in lateTertiary and early Quaternary times. They belong to the multiple-vent basalts,but not the plateau basalt in the type of eruption. In this paper are given the results of a petrochemical...

Ⅰ. General SKETCH The Cenozoic basalt lavas are widely distributed along the coastal regionand its adjacent districts in eastern China. They form either widespread plateausor scattered mesa-like hills; and, in some places, the volcanic craters are stilladmirably preserved to-day. These basalt sheets were erupted extensively in lateTertiary and early Quaternary times. They belong to the multiple-vent basalts,but not the plateau basalt in the type of eruption. In this paper are given the results of a petrochemical study of the Ceno-zoic basalt in eastern China. Geological and petrographical studies of the basaltsare not described in detail. Judging from the chemical compositions, the mostoutstanding characteristic feature of the most basaltic rocks is the richness inalkalis, especially in K_2O, also the undersaturation in silica, and, therfore,the most of the basalts distinctly belong to the alkaline rock suite. Such chemicalcharacters are closely related to modal compositions. The general petrogra-phical characters of the basalt may be now as well described. In North Chinaand South Manchuria most basalts are trachy basalt and its allied types, andoccasional nepheline basalt. The constituent minerals of these basalt are cha-racterized by the presence of anorthoclase, potash-adesine, plagioclase, titanaugite,as well as by the abundance of olivine. In South China the main basalt is olivinebasalt, consisting of olivine, augite, and plagioclase as usual. At some placesthe basalt may be slightly silica saturated that the occasional presence of hyper-thene and quartz (xenocryst) is noteworthy. In North Manchuria the dominant basalt is leucite basalt, containing leucite and olivine as phenocryst and groundmass constituent. Xenocryst of quartz and feldspar grains are sometimes present.In Taiwan Province, basalt of Kuanyinshan volcano is of the tholeiite type,but, in some other districts, the alkaline basalt with feldspathoidal constituentalso occurs. In view of the above-mentioned facts, the petrographical difference seemsto be matched by the differences of the major tectonic forms of China. Thesefacts may be tabulated below: Geographical region Tectonic forms Basalt type 1. North Manchuria Granitized region in Varisclde Leucite basalt 2. North China & South Precambrian Sino-Korean Trachybasalt Manchuria massive 3. South China Huanan platform in Yenshanide Olivine basalt 4. Taiwan Himalayide Tholeiite basalt Ⅱ. Regional INVESTIGATION In Table 1 the chemical analyses of the Cenozoic volcanic rocks in easternChina published up to 1951 were collected, of which 74 analyses are basalticrocks. The available analyses of every basalt sheet are taken an average to re-present the regional composition of the basaltic rocks. The localities of the basaltsheets where the analyzed chemical data are referable are shown in Figure 1.In all, 21 localities of basalt are investigated. The average chemical compositionsof each basalt locality, together with the normative minerals, Niggli's valuesand Zavarickij's numbers are given in Tables 2 A and 2 B respectively (localnos. in Table 2 correspond to the numerous in circle in Figure 1). For theconvenience of comparison, the average chemical composition of some standardbasalts (after S. R. Nockolds, 1954), some alkaline basalt in New Zealand (afterW. N. Benson, 1944) and Uganda (after A. Holmes, 1937), and the world's ba-salts, together with the normative minerals, Niggli's values and Zavarickij'snumbers of our calculation, are selected and given in Tables 3A, 3B, 7A, 7Brespectively. As mentioned above, the chemical composition of eastern China basalt ischaracterized by the high content of alkalies, and especially the K_2O. This cha-racter is definitely revealed by the normative feldspar, which is given in Table2 A and graphically shown in Figure 2. From this graphical representation,it is recognized that the normative feldspar becomes increasingly enriched ormolecular from South China to North Manchuria. Although the projected points appear to be scattered, a trend of clustering of the normative feldspars in accor-dance with its geographical distribution is apparent upon close inspection. Inthe normative pyroxene diagram, Figure 3, it is shown that most basalts of easternChina are rich in Wo molecular, falling near the Di-Hd line; On the otherhand, those of Kuanyinshan basalts of Taiwan Province are poor in Wo andcluster in the central part of the Di-Hd-Fs-En field. Therefore, that the easternChina basalt, excluding that of Kuanyinshan, belong to the alkaline rock suiteis justified. The comparison diagrams of qz, al-alk, C-(al-alk) and K-mg ofNiggli's values, based on the data given in Tables 2 B, 3 B, and 7 B, are gra-phically shown in Figs. 4, 5, 6 and 7 respectively. As will be seen from thesefigures, in general, the qz and al-alk of Niggli's value are lower, but C-(al-alk) and K-mg are higher than those of some common basalts. Fig. 8 isZavorickij's petrochemical vector diagram, from which the petrochemical cha-racters of high alkaline property in eastern China basalts are clearly justified. Ⅲ. Serial COMPARISON For ascertaining and understanding the general chemical characters, theCenozoic eastern China basalt and its differentiated associations are divided,based on the SiO_2 content, into 5 chemical types, the average composition ofwhich is given in Table 5A. As the chemical composition of Kuanyinshanvolcanic rocks in Taiwan Province shows a distinct calc-alkaline affinity, it is,therefore, dealt with the same procedure as well. The average chemical compo-sition of the volcanic rocks is given in Table 5 B. Since the Cenozoic basalt ineastern China covers the region adjacent to the Circum-Japan Sea and the Ja-panese Archipelagoes which are well known by the occurrence of alkaline andcalc-alkaline rock suite respectively. The serial variation in the chemical com-position of eastern China volcanic rocks is examinated in comparing them withthose of the Circum-Japan Sea and the Japanese volcanic rocks. The data usedfor the Circum-Japan Sea and Japanese rocks, which are given in Tables 6 A and6 B, are based on Tomita's and Yamada's calculated results respectively. Zavaric-kij's number of the same rocks, based on Zavarickij's data, is given in Table6 C. Following various petrochemical methods, some graphic diagrams are cons-tructed in order to express the chemical characters of the rock series of easternChina more definitely. The difference in chemical composition as comparedwith the Circum-Japan Sea alkaline rock suite is shown in the normal varia-tion diagram Figure 9. Other petrochemical indices (proposed by Peacock, Hol- mes and Tomita respectively) obtained are summarized below: Ⅰ Ⅱ Ⅲ Ⅳ alkali-lime index (Fig. 10) 65.5 59.0 63.0 52.0 alkali-alumina index (Fig. 11) -- -- 67.8 63.3 Ol-Q index (Fig. 12) 20.0 43.0 72.5 76.5 Ne-Hy index (Fig. 13) -- -- 55.0 59.9 Di-C index (Fig. 14) 46.5 46.5 -- -- Ⅰ. Japanese volcanic rocks; Ⅱ. Taiwan volcanic rocks; Ⅲ. Circum-Japan Sea alkaline suite; Ⅳ. eastern China volcanic rocks.From these graphical solutions in Figs. 10-14, it may be justified that thevolcanic rocks in eastern Asia have increasingly enriched the alkali contentfrom the Japanese Archipelagoes to the mainland of China. Figure 15 is avariation diagram of the normative feldspar of the eastern China series, incomparison with that of the Circum-Japan Sea region, the Japanese Archipela-goes and New Zealand. As will be seen from the diagram, the variation of thenormative feldspar of eastern China rock series is quite discriminative. Notonly is it richer in or molecular, but the positions of point N and O (corres-pond to the respective Ol-Q and Ne-Hy indices as shown in Figs. 12 and 13)of the eastern China series are also in a later course than the others. Figure 16is a paragenetic diagram of the normative plagioclase and pyroxlene of theeastern China series. In the variation diagram of the normative pyroxene, Fig.17, the distinct difference in the course of variation between the alkaline andcalc-alkaline series is clearly revealed. In this connection, the directon of varia-tion in the normative pyroxene of the alkaline series differs from that of thecalc-alkaline series. It is also notable that the range of variation in the easternChina series is smaller, due to the presence of higher Wo molecular in bothbasic and acidic types, as compared with that of the Circum-Japan Sea series.Figure 18 is Zavarickij's petrochemical vector diagram of the eastern Chinaseries compared with that of Circum-Japan Sea and Japanese series. It may be acomplemental diagram of the serial comparison diagram of eastern Asia volcanicrock series, prepared by Zavarickij (cf. A. N. Zavarickij's Introduction to Petro-chemistry of Igneous Rocks, 1950, Fig. 61, p. 205, in Russian). The distinctdifference of these rock series may be clearly observed in the graphical solution.In Table 7 A is given the average chemical composition of eastern China basalt,together with the composition of basaltic rocks of the world (including olvinebasalt and Toleiite, Ocean basalt and Continent basalt) for comparison. Theeastern China average is very similar to the average composition of the olivine- basalt of the Circum-Japan Sea region (based on Tomita, 1935, and recalculatedby the writer), while it differed more or less from that of any of the world'sbasalts by the high content of alkali and especially K_20. This character isdefinitely revealed by the normative feldspar and pyroxene, which are graphi-cally shown in Figs. 19 and 21 respectively. Figure 20 is Zavarickij's petroche-mical diagram of the world's basalt. As shown in these diagrams, it suggests atransitional relation rather than a sharp cleft in the petrochemical charactersof the world's basalts. There are no distinct types of basalt magma but rathera continuous series from silica saturated (tholeiitic) to silica-undersaturated(olivine-basalt) rock, although the chemical distinction may be too subtle to beread directly from chemical analyses. Ⅳ. ORIGINAL Basalt Magma The original magma of eastern China basalt belongs to the olivine basaltmagma type. In this discussion it is assumed that the primary olivine basaltmagma is melted from a crust of peridotitic crystalline rock in the upper partof the sima layer. Olivine basalt magma may be modified by the gain of alimited amount of silica and some alkalies to produce a derived melt, whichappears to coincide with the tholeiitic

~~

This paper gives a derivation of the slope deflection equations for the determination of the secondary internal forces due to prestressing, shrinkage and creep for hyperstatic prestressed concrete structures of variable cross section. Tables of seconx dary fixed end moments for prismatic and haunched beams with straight and parabolic tendons have been prepared for use in practical applications, A method of using concordant pressure line for the elimination of secondary forces due to prestressing is introduced....

This paper gives a derivation of the slope deflection equations for the determination of the secondary internal forces due to prestressing, shrinkage and creep for hyperstatic prestressed concrete structures of variable cross section. Tables of seconx dary fixed end moments for prismatic and haunched beams with straight and parabolic tendons have been prepared for use in practical applications, A method of using concordant pressure line for the elimination of secondary forces due to prestressing is introduced. Other constr- uctional methods of avoiding secondary forces due to shrinkage and creep are reviewed. The problem of using the ultimate lood method to the theoretical analysis of hyper- static prestressed concrete structures is also discussed.

本文推导了确定变截面超静定予应力钢筋混凝土结构因予加应力、收缩、蠕变引起附加内力的变位方程式.为了便于实用,对直线及抛物线形予应力压力线的值梁与加腋梁的固端弯矩制成计算表格. 本文并介绍了采用协调压力曲线以消除因予加应力所引起的附加内力的方法,同时介绍了通过施工方法消除因收缩与蠕变所引起的附加内力的方法. 文中并对按极限状态理论计算超静定予应力钢筋混凝土结构的问题作了一般性的探讨.

In order to compare the changes of blood pressure reasonably, concretely, simply, and quantitatively, the "net % of hyper and hypotensive areas", which integrates the considerations of the original level of blood pressure (AD in Fig. 1), the magnitude and the duration of the changes, is proposed. It is especially practical in the screening of drugs. Suppose the area between AD and the base line 0 mm Hg is S, the area between AD and the blood pressure curve below is S', and the area between AD and the...

In order to compare the changes of blood pressure reasonably, concretely, simply, and quantitatively, the "net % of hyper and hypotensive areas", which integrates the considerations of the original level of blood pressure (AD in Fig. 1), the magnitude and the duration of the changes, is proposed. It is especially practical in the screening of drugs. Suppose the area between AD and the base line 0 mm Hg is S, the area between AD and the blood pressure curve below is S', and the area between AD and the blood pressure curve above is S", then % of hypotensive area=-S′/S×100, % of hypertensive area=S"/S+S"×100. The net percentages of different groups (e.g., control and drugs) may be compared by t or F tests. The assay results are considered in terms of both the net % and the statistical significance. For the purpose of illustrating its calculations and applications, 4 different drugs were tested on 4 species of animals. Hexamethonium and hydralazine were confirmed to possess a high hypotensive potency. Reserpine induced a slight elevation of blood pressure in rats and little effects in dogs; these were in conformity to the results of other investigators. The chief advantages of the present project are: 1) no need of special unit; 2) exemption from complicated mathematical computations; 3) adequate revelation of the influences; and 4) applicability to clinical or animal experiments, drug or other therapeutic measurements, acute or chronic trials, and hypertensive or hypotensive effects.

本文综合升、降压强度,升、降压时间及原血压水平等因素,建议用“浄升、降压面积百分比”,以求合理、明确、简便、定量地比较血压变化的结果.尤其是在篩药时,便于迅速比较多种药物的作用。设原血压水平与基线0毫米汞柱间的面积为S,原血压水平与降压曲线间的面积为S’,原血压水平与升压曲线间的面积为S”,则: 降压面积%=—S’/S×100 升压面积%=S”/S+S”×100 降压面积百分比扣减升压面积百分比,得浄升、降压面积百分此。各组间(例如给药组与对照组间,或不同药之间,或不同动物之间)的面积百分比,可按t或F测验求出相差的显著性(P值)。比较药物的效果时,主要根据其净升、降压面积百分比的数值,同时还应参考统计学的显著性。为了说明“浄升、降压面积百分比”之计算及应用,本文利用狗、猫、兔及大白鼠4种动物,注射利血平、藜芦碱、六烃季铵及肼苯噠嗪,按照以上公式计算,求得净升、降压面积百分比。结果证明六烃季铵及肼苯噠嗪的降压效果较强,利血平不使狗血压下降,使大白鼠升压。这些结果与文献报告是一致的。本方案的主要优点是:(1)不用任何特别单位;(2)无需复杂的数学演算;(3)结果能反映药物的作用且与文献相符;(4)无论对于临床或...

本文综合升、降压强度,升、降压时间及原血压水平等因素,建议用“浄升、降压面积百分比”,以求合理、明确、简便、定量地比较血压变化的结果.尤其是在篩药时,便于迅速比较多种药物的作用。设原血压水平与基线0毫米汞柱间的面积为S,原血压水平与降压曲线间的面积为S’,原血压水平与升压曲线间的面积为S”,则: 降压面积%=—S’/S×100 升压面积%=S”/S+S”×100 降压面积百分比扣减升压面积百分比,得浄升、降压面积百分此。各组间(例如给药组与对照组间,或不同药之间,或不同动物之间)的面积百分比,可按t或F测验求出相差的显著性(P值)。比较药物的效果时,主要根据其净升、降压面积百分比的数值,同时还应参考统计学的显著性。为了说明“浄升、降压面积百分比”之计算及应用,本文利用狗、猫、兔及大白鼠4种动物,注射利血平、藜芦碱、六烃季铵及肼苯噠嗪,按照以上公式计算,求得净升、降压面积百分比。结果证明六烃季铵及肼苯噠嗪的降压效果较强,利血平不使狗血压下降,使大白鼠升压。这些结果与文献报告是一致的。本方案的主要优点是:(1)不用任何特别单位;(2)无需复杂的数学演算;(3)结果能反映药物的作用且与文献相符;(4)无论对于临床或动物实验、药物或其他疗法、急性或慢性试验、升压或降压的效果,均可普遍应用。

 
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