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  不良
     A Study on Bad Creditor's Rights of Japan's Banking
     日本银行业不良债权问题研究
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     Dissolving Bad Loans and Preventing Credit Risk of China's State-owned Commercial Banks
     中国国有商业银行不良贷款化解及信贷风险防范
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     Some Problems in Real-Time Application of the Estimation-Identification Approach of Bad Data
     不良数据估计识别法在实时应用中的几个问题
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     ON BAD DATA IDENTIFICATION METHOD FOR POWER SYSTEM STATE ESTIMATION
     关于电力系统状态估计中不良数据的估计识别方法
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     The Influence of Bad Tuft Rising on Combing Quality
     须从抬头不良对精梳质量的影响
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     Causal Analysis on Bad Starting Performance and the Big Overload Smoke of X195 Diesel Engine
     X195柴油机起动性烟度大的原因分析
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     The Fracturing Technology of Thin and Bad Reservoir in Daqing Oilfield
     大庆油田薄油层压裂挖潜技术
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     Li2O—ZnO—SiO2 system glass ceramic was used to replace conventional glass as the bond of vitrified bond diamond grinding wheels,in hope of overcoming the disadvantages of conventional glass bond such as bad soakage and high thermal expansion coefficient gap between vitrified bond and diamonds.
     本文研究用Li2O—ZnO—SiO2系微晶玻璃代替普通玻璃用作金刚石砂轮结合剂以克服普通玻璃结合剂对金刚石浸润性、热膨胀系数与金刚石相大的缺点。
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     The highest sensitive drugs were josamycin(99.40%)and deoxycyline(94.80%),minoccyline(93.20%)and clarithromycin(91.30%) being the second. The sensitivenesses of levofloxacin,sparfloxacin,tetracycline,ofloxacin,etc. were bad,and the rates were 79.30%,72.60%,63.70% and 61.70%,respectively.
     对交沙霉素(99.40%)、强力霉素(94.80%)最为敏感,其次为美满霉素(93.20%)和克拉霉素(91.30%),对左旋氧氟、司帕沙星、四环素、氧氟沙星等敏感性,敏感率分别为79.30%、72.60%、63.70%和61.70%。
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     The result of 5 excellent, 4 good, and 1 fair, 9 bad. The percentage of being excellent and good was 47.37%.
     晚期手术组19例中优5例,良4例,可1例,9例,优良率为47.37%。
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     The Method of Repairing Bad Tracks of Hard Disk with HDD Regenerator Shell
     用HDD Regenerator Shell修复硬盘
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     Automatic detection of bad data in SCADA system
     SCADA系统中数据的自动检测
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     CONTROL BAD FEELING
     控制心情
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     When the diameter of the inspected apple is between 7.0 cm to 8.5 cm and the diameter of defective part of a bad quality apple is larger than 2 cm, according to the optimal threshold obtained by studying, the accuracy for classifying is larger than 80% with 1 kHz working frequency of capacitive sensor, and its work efficiency can attain one apple per 2.5 s being close to the efficiency of manual sorting.
     在待检苹果直径为 7.0 cm~ 8.5 cm ,损部分的直径大于 2 cm,电容传感器工作频率为 1k Hz时 ,以学习得到的最佳分类阈值进行分类 ,分级正确率大于 80 % ,分级效率达到 2 .5 s分选一个苹果 ,接近人工分选效率
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     Strengthening the Management of Account Receivable and Avoiding the Risk of Bad Debt
     加强应收账款管理 防范呆资金风险
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  恶劣
     Using various safety coefficients (F_s) the formula is suited not only to broad graded sand gravel(F_s=1.5)and low plastic loess (F_s=3) and silty sand (F_s=4.5),but also is suited to suffusion or loose sand gravel and bad construction conditions in the use of double safety coefficient.
     在采用不同的安全系数F_s时,该计算式除适用于保护广级配的砂砾(F_s=1.5)、低、无塑性的黄土(F_s=3)和粉砂(F_s=4.5)之外,在加倍取用安全系数时,还适用于“砂俘走”型或欠密实砂砾,及施工条件恶劣或过薄的滤层。
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     The mean PI in34(57%)patients with good outcomes was lower than1.5,whereas in30patients(83%)with bad outcomes was higher than1.5(P<0.001).
     34例预后良好患者平均PI小于1.5,30例预后恶劣患者平均PI大于1.5(P<0.001)。
短句来源
     By scale static beaker tests,the experimental results showed that its scale inhibition efficiency against CaCO_3,Ca_3(PO_4)_2 and CaSO_4 were 90.5%,93.2% and 86% when its dosage is 8 mg/L,there are still ideal scale inhibition efficiency(40.4%,)32.4%,37.6% against CaCO_3 in bad condition of high temperature,high pH value,high hardness.
     通过静态阻垢实验表明,阻垢剂投加量达到8 mg/L对CaCO3、Ca3(PO4)2和CaSO4的阻垢效果较佳,分别为90.5%,93.2%和86%; 在高温、高pH、高硬度等恶劣条件下对碳酸钙仍分别有40.4%,32.4%,37.6%的较好阻垢率;
短句来源
     Taking EL320 ×256 as an example, this paper introduces hardware interfacing circuit Of electroluminescent (EL) display and its corresponding software flowchart to implement Chinese character menu display and VT100 instruction of compatiblekeyboard, and make the EL display become a general-purpose intelligent display terminal under the bad environment.
     以EL320×256为例,介绍了场致发光显示器的硬件接口电路及相应的软件流程,以实现可显示中文菜单及兼容键盘VT100指令,使之成为真正通用的适合于恶劣环境下使用的智能显示终端。
短句来源
     there are still ideal scale inhibition efficiency 60.2%,46.4%,53.2 %against CaCO_3 in bad condition of high temperature,high pH,high hardness.
     在高温、高pH、高硬度等恶劣条件下对碳酸钙仍分别有60.2%,46.4%,53.2%的较好阻垢率;
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  bad
In this paper, we clarify exactly how "bad" such Gabor expansions are, we make it clear precisely where the edge is between "enough" and "too little," and we find a remedy for their shortcomings in terms of a certain summability method.
      
How to Publish a Good Article and to Reject a Bad One.
      
The effect of complexing with phosphatases and 14-3-3 proteins was demonstrated by the example of Bad protein.
      
How bad can a Banach space with the approximation property be
      
Specific features of the distribution of rare elements and radionuclides in processing of the bad- deleyite concentrate by various methods to obtain pure zirconium compounds and in its chemical purification were studied.
      
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This is a continuation of a previous paper "The Dynamic Behaviors of a Self-biased Bistable Multivibrator". A criterion is obtained in which the effect of distributed capacitances and component tolerance under worst combinations are considered as the bases for design. Experimental results show that the method of design introduced in this paper is effective.

本文是“触发器动态研究”一文的继续,介绍了一个比较简单的动态设计方法。文中考虑了各种分布电容的影响。当电路参数发生变化且处于最不利搭配时,触发器仍具有“交点在U_T前沿的单调翻转过程”。实验结果表明,本文所介绍的设计方法是有效的。

After soil survey of the whole region,it is found that the soils of the North China Great Plain consist of four great soil groups including drab soil,light meadow soil,glei swamp soil and saline soil.The term“calcareous alluvial soils” formerly used hardly interprets any mean of soil formation and productive cha- racteristics. The drab soils formerly named as“Shangtung brown soils”are generally located on the alluvial fan and the foot of mountains.Owing to the higher relief,excess drainage and deeper ground...

After soil survey of the whole region,it is found that the soils of the North China Great Plain consist of four great soil groups including drab soil,light meadow soil,glei swamp soil and saline soil.The term“calcareous alluvial soils” formerly used hardly interprets any mean of soil formation and productive cha- racteristics. The drab soils formerly named as“Shangtung brown soils”are generally located on the alluvial fan and the foot of mountains.Owing to the higher relief,excess drainage and deeper ground water(below 4—6 meters),saliniza- tion is not found.The drab soil is neutral to slightly alkaline in reaction. The chemical data show no evidence of chemical decomposition of clay,but the disintegration of soil particles-clay formation is quite obvious.Along the foot of Taihang range,the drab soils are covered with new calcareous material and bring out the process of recalcification shown by the presence of pseudo- mycelins in the Soil profiles. Light meadow soils are generally distributed in the alluvial plain with higher ground water table laying at 2—3 meters.Owing to the frequency of the fluc- tuation of the ground water in the soil profile,oxidation and reduction are alternately carried out and lots of rusts and mottlings are found in the soil profile of these soils.Under intensive cultivation,the surface soil of light meadow soil is usually loose and mellow and contains lower content of organic matter. The glei swamp soils are formed by the lakeside and in the depressed lowlands where ground water table is quite shallow and sometimes close up to the sur- face.In the depressed lands contacted with mountain foot,longer duration of water-lodging produces strongly gleyed swamp soil with higher content of humus. In the depressed portion of alluvial plain,the temporary water-lodging gives weakly gleyed swamp soil with low content of humus,whilst the strongly gleyed soils are found in the depressed land along seacoast. Salinization of soils is influenced by the ground water and relief.Saline soils are usually distributed in the lowland with higher ground water table and higher mineral content of the water.Irrigation without drainage system will rise ground water table and causes the process of secondary salinization. Saline soils of North China plain may be divided into two subtypes:(1) Saline soil of alluvial plain and(2)Saline soils along the seacoast.The former belongs to the chloride-sulfate saline soils in which the ground water table is about 1.5—2.0 meters and the mineral content of the ground water is about 1—3 grams/liter.In the coastal region,the chloride saline soils are usually found with high ground water table at 1.0—1.5 meter and also high mineral content more than 10 grams/liter.The transitional belt between these two soils above-mentioned is sulfate-chloride saline soils where the ground water table is around 1.5 meter and the mineral content of ground water is 5—10 grams/liter. These four genetic soil types are closely related each other and also alternate between themselves.It is very interesting to study the transitional types among these four soil groups. Between drab soils and light meadow soils,the transitional soil types as meadow drab soils and drab meadow soils are formed under different transitional circumstances.The meadow drab soil is distributed at the bottom of alluvial fan with higher ground water table(1.5—3 meters),while the drab meadow soil is formed on the old riverbed in the alluvial plain with comparatively uplifting relief where the ground water table becomes deeper(3—3.5 meters). Many transitional soil types are also developed between the light meadow soils and glei swamp soils.The worse water lodging condition enforces the meadow soil transfering to glei swamp soil,whilst promotion of water condi- tion by diking drainage cannel or local silting up of lowlands causes the trans- formation of glei swamp soil in to light meadow soil or even to the drab soil. Salinization of soil is always accompanied with the formation of light meadow soil.Rising the ground water table and increasing the mineral content of ground water will induce or enforce the process of sainization of soils.On the other side,desalinization of soils can be carried out when the ground water table becomes lower.When the seatide is shut by dikes and the drainage condition is improved,the saline soil in the coastal region will be transfered to the light meadow soils.

经过一年多的大规模调查,证实了华北平原的土壤都具有不同的类型和不等程度的发育,其中包括很多土类、亚类和变种,过去简称华北平原土壤为“石灰性冲积土”,是很难反映情况和说明问题的。华北平原的主要成土过程有褐土过程、浅色草甸土过程、沼泽过程和盐土过程。褐土多发育于山麓及冲积扇形地上,地势较高,排水良好,地下水埋藏较深,约在4—6米以下。在降水淋洗之下,可溶盐类皆被淋失,不发生盐演化现象,土壤只及于粘化作用,pH 值多属中性至微碱性。太行山麓的褐土因受石灰性沉积物的覆盖,发生次生碳酸盐化作用,土壤剖面中有假菌丝体存在。浅色草甸土多分布于冲积平原,其形成过程受地下水的影响极显著。地下水埋藏深度约2—3米,也可达4—5米。由于地下水升降频繁,氧化还原作用交替进行,土壤中呈现显明的锈纹斑,但无假菌丝体。土壤疏松多孔而有结构性,因土壤中有机质较少、土色浅淡而多受人为耕作的影响,故称耕种浅色草甸土。洼地及湖淀附近,地下水埋藏较浅或地表积水,土壤发生沼泽化过程。山麓交接洼地,积水时期长久,潜育作用及腐殖质积累均较显著。平原中洼地比较平坦,积水时间亦较短,腐殖质积累和潜育作用都较轻微。海滨洼地中,潜育作用较为剧烈,但有机质的积累则...

经过一年多的大规模调查,证实了华北平原的土壤都具有不同的类型和不等程度的发育,其中包括很多土类、亚类和变种,过去简称华北平原土壤为“石灰性冲积土”,是很难反映情况和说明问题的。华北平原的主要成土过程有褐土过程、浅色草甸土过程、沼泽过程和盐土过程。褐土多发育于山麓及冲积扇形地上,地势较高,排水良好,地下水埋藏较深,约在4—6米以下。在降水淋洗之下,可溶盐类皆被淋失,不发生盐演化现象,土壤只及于粘化作用,pH 值多属中性至微碱性。太行山麓的褐土因受石灰性沉积物的覆盖,发生次生碳酸盐化作用,土壤剖面中有假菌丝体存在。浅色草甸土多分布于冲积平原,其形成过程受地下水的影响极显著。地下水埋藏深度约2—3米,也可达4—5米。由于地下水升降频繁,氧化还原作用交替进行,土壤中呈现显明的锈纹斑,但无假菌丝体。土壤疏松多孔而有结构性,因土壤中有机质较少、土色浅淡而多受人为耕作的影响,故称耕种浅色草甸土。洼地及湖淀附近,地下水埋藏较浅或地表积水,土壤发生沼泽化过程。山麓交接洼地,积水时期长久,潜育作用及腐殖质积累均较显著。平原中洼地比较平坦,积水时间亦较短,腐殖质积累和潜育作用都较轻微。海滨洼地中,潜育作用较为剧烈,但有机质的积累则不一致,水浅处的有机质积累较多。因地形及地下水的情况不同,土壤盐渍程度各地不一。盐渍土多发生于山前交接洼地、碟形洼地边缘,以及槽状洼地和地上河流的两侧。有些灌区由于缺乏合理的灌排系统和灌溉制度,土壤发生了次生盐演化现象。华北平原盐渍土可分为内陆及海滨两种:内陆盐渍土多属氯化物硫酸盐土,地下水埋藏深度约1.5—2.0米,地下水矿化度约1—3克/升;海滨盐土区多属氧化物盐土,地下水埋藏深度约1.0—1.5米,地下水矿化度大于10克/升;过渡地带(即海滨盐土与内陆盐土的过渡地带)的盐渍土多属硫酸盐氯化物盐土,地下水埋藏深度约1.5米左右,地下水矿化度5—10克/升。华北平原中的四个主要成土过程是互相联系,而且有过渡阶段的。褐土和浅色草甸土的形成条件,主要在于排水情况和地下水位的不同。所以这两种土壤分布毗鄰而有互相过渡的发展情况。扇形地中下部,地面排水尚好而地下水埋藏较浅(1.5—3米),褐土区中可发育浅色草甸褐土。在泛盐平原中地势相对高起的黄河故道或靠近冲积扇地区,地下水埋藏较深(3.5—5米),可发育褐土化浅色草甸土。泛溘平原中的洼地积水愈久,沼浑化过程愈强,可由沼泽化浅色草甸土过渡至浅色草甸沼泽土或沼泽土。但经人工挖沟排水或洼地淤平以后,土壤可由沼泽土转向浅色草甸过程或褐土过程发展。浅色草甸土中如地下水埋藏浅而矿化度高,则土壤可向盐土方向发展。海滨盐土如不再受海潮影响和改善排水情况,则土壤也可由盐土向浅色草甸土发展。

The branching ratios of the decay of the hyperons, the ratios of the mean life times of the decay of various hyperons and the ratios of the life times of the hyperons to that of the K+ -meson are calculated by using the universal Ferm weak interaction proposed by Feynman and Gell-Mann and the strong interaction proposed by Salam. The perturbation theory is used with a cut off in the region of large momentum. By using the coupling constants of the strong interaction given by Warner and choosing suitable values...

The branching ratios of the decay of the hyperons, the ratios of the mean life times of the decay of various hyperons and the ratios of the life times of the hyperons to that of the K+ -meson are calculated by using the universal Ferm weak interaction proposed by Feynman and Gell-Mann and the strong interaction proposed by Salam. The perturbation theory is used with a cut off in the region of large momentum. By using the coupling constants of the strong interaction given by Warner and choosing suitable values for the other two coupling constants remaing to be fixed most of the results of our calculation agree fairly well with the experiments. The worst result differs from the experimental Values at most by

本文应用了费曼和盖尔曼所提出的普适费米弱相互作用和同位旋守恒的强相互作用计算了各种超子、K介子衰变的分枝比和平均寿命的比例。在计算时应用了微扰论,并在大动量处将相互作用截断。在应用了查尔斯·瓦纳所给出的相互作用常数和对其余两个常数作了一定的选择之后,得到的分枝比和平均寿命之比大部分和实验结果符合,最坏相差一个因子二。如果选择本文所采用的相互作用常数,可以改进前一篇源文中K~+介子分枝比计算结果和实验的符合程度。 本文计算表明V-A普适弱相互作用确实适用于K分子和超子衰变现象,表明在解释这些现象时,必须考虑到“很强”和“较强”两类强相互作用所分别产生的影响。此外,本文还表明Λ和∑应具有相同的相对宇称,K分子和核子、超子之间的四种强相互作用中必须至少有一对是膺标量耦合。

 
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