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interrupt
相关语句
  中断
     A UNIVERSAL KEY INPUT SYSTEM WITH DIRECT INTERRUPT CODING
     直接中断型编码方式的通用输入键盘系统
短句来源
     The Design of Intel 8085A Hardware Interrupt Test Microcomputer
     INTEL8085A硬件中断测试单板机设计
短句来源
     The Design of Z80 Microcomputer Interrupt Control System on Multi-interrupt Sources
     多中断源Z80微型机中断控制系统的设计
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     CMS CONSOLE INTERRUPT AND IT'S SERRICE PROGRAMS
     CMS控制台中断及相应的服务程序
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     IBM-PC COMMUNICATION INTERRUPT SERVICE
     IBM-PC机通信的中断服务
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  “interrupt”译为未确定词的双语例句
     Principle & application of MSP430 TIMER_A interrupt
     MSP430单片机TIMER_A中断的原理及运用
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     Applied Research on the Interrupt of TMS320LF240x Series DSP
     TMS320LF240x系列DSP中断的应用研究
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     This paper describes the advantages of using the P87LPC76X and P89LPC900 CPU family as the hardware monitor of the 8XC5X (including 8XC5XX2 and P98C6XX2) CPU family, the methods of hardware connection, and the main points of the monitor CPU's interrupt service procedure programming.
     介绍了用P87LPC76X、P89LPC900系列CPU作8XC5X(包括8XC5XX2、P98C6XX2)系列CPU硬件监视器的优点、硬件连接方式、监控CPU中断服务程序编写要领.
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     Interrupt system analysis and C language program on TMS320LF2407
     TMS320LF2407中断系统分析及C语言编程
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     Interrupt Handle Based on MPC8250 and Embedded Linux
     基于MPC8250和嵌入式Linux的中断处理
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  相似匹配句对
     Interrupt Test in RISC
     RISC体系结构计算机的中断检测
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     The Design and Implementation of Interrupt Handling
     CHILL语言中断处理的设计实现
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查询“interrupt”译词为用户自定义的双语例句

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  interrupt
For example, aminoglycosides interrupt translation, producing toxic peptides.
      
Links cuts, node interruptions, software errors or hardware failures, and transmission failures at various points can interrupt service for long periods of time.
      
Furthermore new arrivals with higher priority level can interrupt the lower retransmission in order to reduce its access delay although it increases the lower priority's delay.
      
- It is important to interrupt the passivity, inadequacy and regressive defences against unresolved conflicts which underlie the progress of the psychosis.
      
The treatment comprises avoidance of any precipitating factor and administration of heme arginate or high-dose glucose infusions which interrupt the dysregulated hepatic heme biosynthesis.
      
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The effect of hot working on the graphite formation in 1.1—1.2% carbon toolsteels during subsequent annealing was investigated.Specimens were heated in air to1050℃ for 10 minutes,cooled in a second furnace to the forging temperature,forged rapidly to give reductions in height between 0—40%,air-cooled,and annealed for16 hours at 700℃.Graphite was determined by chemical analysis.It was foundthat:1.Austenitizing in air between 870°and 1050℃ followed by air cooling causedthe formation of graphite during subsequent...

The effect of hot working on the graphite formation in 1.1—1.2% carbon toolsteels during subsequent annealing was investigated.Specimens were heated in air to1050℃ for 10 minutes,cooled in a second furnace to the forging temperature,forged rapidly to give reductions in height between 0—40%,air-cooled,and annealed for16 hours at 700℃.Graphite was determined by chemical analysis.It was foundthat:1.Austenitizing in air between 870°and 1050℃ followed by air cooling causedthe formation of graphite during subsequent annealing.The amount of graphiteincreased with increasing austenitizing temperature.Precipitation of graphite occurredalong the austenite grain boundary.2.Hot working at various temperatures increased the tendency of graphitizationduring subsequent annealing.The amount of graphite formed was smallest whenthe specimens were forged at 870℃ and increased with increasing or decreasingtemperature.3.Slow cooling after the specimens had been heated to or hot worked at hightemperatures reduced the degree of graphitization,provided that free cementite wasabsent during hot working.4.Forging during continuous cooling removed the effect of previous heatingor hot working until the temperature was sufficiently low to produce free cementiteduring forging.Forging during cooling gave minimum amount of graphite whenthe forging was interrupted between 820°and 870℃.A possible explanation to account for the phenomena is suggested.

在热加工过程中,加热及加工温度对1.1—1.2%碳钢在加热或加工后空冷再进行球化退火时,渗碳体分解为石墨的作用有重要的影响。在奥氏体状态870℃以上,停止加工的温度愈高,以后石墨的析出作用也愈严重。高温加工后缓冷或在低温加工可以减轻石墨化的作用。

Ⅰ. The Yinshan district as an example of "activizing region" in the Chinese platform One of the most typical localities that show clearly the phenomenon of"activization of platform" (активи. зация платформы) is the Yinshan region, aneast western mountain range on the border between the North-China plain andthe Mongolian plateau. It has long been recognized as a platform because ofthe presence of a folded foundation Pre-Sinian in age. However, owing to thefacts that Mesozoic crustal movements and magmatic activities...

Ⅰ. The Yinshan district as an example of "activizing region" in the Chinese platform One of the most typical localities that show clearly the phenomenon of"activization of platform" (активи. зация платформы) is the Yinshan region, aneast western mountain range on the border between the North-China plain andthe Mongolian plateau. It has long been recognized as a platform because ofthe presence of a folded foundation Pre-Sinian in age. However, owing to thefacts that Mesozoic crustal movements and magmatic activities are importantwithin this area, some geologists including G Schoenmann, hold that it is ageosynclinal region. It is Ю. М Шейманн who first noticed the phenomenon of activizationappearing in the Chinese platform. В. М. Синицын in his "Строенив и развитиекитайской платформы" indicates that some of the mountain ranges includingYinshan, which have been formerly referred to the folding belts developingfrom geosynclines, are in fact the internal structures of the Chinese platform. In this paper the writer after the opinion of В. М. Синицын, assigns theYinshan area as one of the "activizing regions" in the Chinese platform, andgives more detailed descriptions and discussions mainly on the point of thehistory of its stratigraphic development. Really it is a fact that the Yinshan region has an old folded foundationwhich is composed of metamorphic complex including chiefly gneisses, schists,and old granitic intrusions apparently Pre-Sinian in age. Since the formationof this folded foundation during the Luliang movement (=Goto-Karelian mo-vement), the old land of the Yinshan region has "activized" or "resurrected"several times. As early as in the Sinian period, a depression prolonging in E-Wdirection happened on its southern border, where Sinian limestone 900 metresin thickness and in some places up to 9,620 metres was so deposited. During a long time of the Palaeozoic era, the Yinshan old land was in the poriod ofdenudation except some Cambrian marine limestones only 144 metres in thick-ness deposited in the western part. At the end of the Palaeozoic era, local acti-vization with the formation of continental basin-deposits of Permian age, up to1,380 metres in thickness, as found in the Tachingshan area again happened.In the middle Mesozoic era, the Yinshan region came to a period of strongactivity. Structural depressions duo to "Процесс аркогенеза" occurred universallywithin the whole area and magmatie activities in large magnitude associatedthis crustal movement, so that a great sequence of freshwater basin-depositswith intercalations of volcanic beds, up to 8,000 metres in total thickness wereformed. During the formation of these strata, especially at the end of Mesozoic,interruptions of depositon happened frequently, folds and thrusts were abund-antly formed, and intrusive bodies of "young granite" were produced hereand there. In the Tertiary period, the Yinshan region was violently faulted, andvolcanic activities still happened, producing the basalt lava flow spreading ina wide area. The activity of the Yinshan old land has not ceased even to-dayas shown by the facte that its whole area is in the process of uplift and by thepresence of an earthquake zone known in the historical time. Ⅱ. To what Geotectonic Unit does the Southeastern Coastal Region of China Belong? On the Southeastern coast of China there is a district where geotectoniccharacteristics have never been recognized clearly. It is A. W. Grabau who firstreferred it to an old land named "Cathaysia". J. S. Lee holds the same opinion.In his geotectonic map of China, B. M. Синицын also assigns this region to aplatform and marks it as a part of his "Южно-китайский платформенный массив".However, there is still another opinion opposed to this. A. C. Хоминтовский, forinstance, renders recently this district to a geosynclinal region and proposes thename "Minche Pacific folding zone" for it. H. T. Yang and T. Y. Yu agreewith him. In the year 1954, the writer in his compilation-work connected with thegeology of Fukien and Kwangtung, found that the geotectonic characteristics ofthe southeastern coastal region of China are not only unagreeable with thosefound in a common platform on the one hand, but also contrasting, with thoseof a geosynclinal region on the other. In fact, it cannot be referred suitably toany geotectonic unit except to the intermediate type as shown by the history ofits geological development. Apparently it is an "activizing" or "resurrected" platform. During the Pre-Sinian crustal movement (the Luliang movement), a foldedfoundation composed of old gneisses, schists, and phyllites was completely for-med. Obviously this is a part of the broad old land of Southern China. In the earlier stage of the Palaeozoic era, the whole area of this region wasexposed in the air and under denudation. Hence, no deposit of any kind wasformed. After the Caledonian movement, depressions happened in the western partof this region, where the Devonian-Lower carboniferous continental deposit, theNanching series consisting mainly of quartzite, conglomerate and shale has beenformed, but the other parts were still under denudation. These facts show thatthis region was still a land at that time. Uralian and Lower Permian limestones, known respectively as the Chuan-shan limestone and the Chihsia limestone, separated from each other by adisconformity, spread widely in this region. This indicates that the marine trans-gressions really happened in the southeastern coastal region of China. However,the thicknesses of these limestones (only 30 metres and 150 metres respectively)and their uniformity in the horizontal direction show that the sea at thosetimes was shallow, and the magnitude of subsidence of the earth crust withinthis region was small. The unnoticed lateral changing of lithological charactersof these limestones proves the same fact. Undoubtedly these limestones arenothing but the marine deposits of platform-type. From Upper Permian toTriassic, this region was under a condition of alternation of transgression andregression of the sea. Owing to the fact that the amplitude of oscillation of theearth crust of this region at that time was small, the deposits formed duringthe marine transgression were thin and interrupted again and again by disconfor-mities (or even unconformities). Sometimes continental deposits are intercalated. Since the later period of Triassic, the southeastern coastal region has neverbeen covered by the sea again. And, a new condition began to happen in LowerJurassic. Here, the old land became to "resurrected", so that a series of depres-sing belts were formed as a result of "Процесс аркогенеза". In association withthe subsidence of these depressions, continental beds with a total thicknessup to 3,000 metres were deposited. In the beds interruptions frequently occurred.Folds were abundants, although they or at least some of them were intermediatetype. At the same time, magmatic activities were significant. Itappearedfirstly in the form of volcanic eruptions as recorded by a great sequence of beds consisting of tuff and rhyolite intercalating in the continental bedsmentioned above. And then, at the end of the Mesozoic, numerous graniticbodies were produced. Coming to the Cenozoic era, this region still sufferedfrom rather strong crustal movements accompanied by basalt lava eruptions. Theactivity of the old land has not yet been ceased even to-day as marked by thepresence of a famous earthquake zone between Kwangtung and Fukien, and theabundance of hot springs which widely spread within this region. All theseshow the typical characters of an "activizing" or "resurrected" platform. Final-ly, the complexity of the types of mineral deposits found in Fukien and Kwang-tung also proves the geotectonic nature of this region. Summarizing the whole matter, we may say that the southeastern coastalregion of China was originally an old land. Although it has been agian andagain submerged by the sea, the resulting marine deposits are entirely differentfrom those of geosynclinal region. In the middle of Mesozoic, this region beganto be active violently again, producing a series of depressions or "secondarygeosynclines", in which thick continental beds were deposited, and, at the sametime, folds of intermediate type, serious volcanic eruptions and magmatic intru-sions were produced. Hence, to refer the southeastern coastal region of China toan "activizing" platform is quite strongly proved. The northwestern boundary of this "activizing" platform is generally onthe line starting from central Chekiang through central Kiangsi to the Sou-thwestern part of Kwangtung, because the history and characteristics of geolo-gical development of the Southeastern Kiangsi and Central-southern Kwangtungare quite similar to those of Fukien and Eastern Kwangtung. As to the nomination of this geotectonic unit, the writer proposes to callit "Cathaysian activizing region". This name is derived from the "Cathaysia"of A. W. Grabau but adds, according to necessity, the meaning of activizing or"resurrected" characters of this region. The so-called "Minche Pacific foldingzone" of A. C. Хоминтовский is obviously unacceptable because it entirely doesnot coincide with fact. Compared with the "aetivizing" platforms found in other parts of theworld, the Cathaysian coastal "activizing" platform has its own characteristics,especially shown by the presence of numerous, widely spread, small depressionsor "secondary geosynclines", and the acidic magmatic activities appearing on alarge scale. All these indicate that this is a special type differing from all theknown "activizing" plat

~~

The present paper deals with the third stage larvae of synanthropic flies col-lected from Shanghai District. A general key is given, comprising 31 identifiedspecies and several undetermined species. The latter are keyed to the family orgenus only. The larvae of Fannia prisca Stein, Ophyra chalcogaster (Wd.), and the pupaeof Graphomyia rufitibia Stein, and Musca convexifrons Thoms. are described for thefirst time. 1. Fannia prisca Stein (fig. 2) Third stage larva: The sculptures of the cuticle of the ventral...

The present paper deals with the third stage larvae of synanthropic flies col-lected from Shanghai District. A general key is given, comprising 31 identifiedspecies and several undetermined species. The latter are keyed to the family orgenus only. The larvae of Fannia prisca Stein, Ophyra chalcogaster (Wd.), and the pupaeof Graphomyia rufitibia Stein, and Musca convexifrons Thoms. are described for thefirst time. 1. Fannia prisca Stein (fig. 2) Third stage larva: The sculptures of the cuticle of the ventral side of theabdominal segments are scale like, those on the posterior one fourth being moreregular. On the same side of segments IV-VII are 2 large non-pediculate strawberrylihe sub-lateral processes, in addition to 6 small ones transversely arranged nearthe posterior border of each segment. The basal portion of the marginal fleshyprocesses of the 8th abdominal segment are provided with bifurcated short branches.The anterior spiracle possesses 9 finger-shaped processes radiating in a fan-likemanner. The pediculate posterior spiracle is provided with 3 rather long processes,on the tip of which the spiracular slit opens. These characteristics when used incombination are sufficient to distinguish this species from F.canicularis (L.) andF. scalaris (F.). In nature, the larvae are chiefly found in decaying Vegetable matter, such asheaps of vegetable leaves in garden or in garbages; occasionally they occur on de-caying animal matter as well as animal and human feces. In the laboratory, thelarvae can be reared easily in dregs from bean curd manufacture. 2. Graphomyia rufitibia Stein (figs. 3, 4) Pupa: Puparium brown, spindle shaped, tapering on both ends. Posterior surfaceof 8th abdominal segment very small, with 3 pairs of posterior processes. Posteriorspiracles small, elliptical, with spiracular slits slightly sinuous and subparallel toeach other. In the anal region are 2 anal, 2 subanal, 2 extra-anal tubercles and asingle preanal protuberance. With the exception of the anal tubercles the remainingtubercles and protuberance are provided with minute spines. Anal plate rather small,the lateral portion gently bent backwards. Anterior spiracle with 5 rounded digits.The general appearance of the bucco-pharyngeal apparatus is similar to the Phaonia type. Egg: The egg has broad dorsal flanges, which run nearly parallel, well separa-ted to each other, and with a bluntly serrated margin. This also suggests that thegenus Graphomyia is closely related to phaoniine flies. The pupae were found twice in garbage heaps. 3. Ophyra chalcogaster (Wd.) (fig.6) Third stage larva: Resembles to O. leucostoma (Wd.), but differing in the fol-lowing points: Anterior margin of the anal plate rounded and oblique to theposterior border of the segment before it, but the posterior margin is curved in-wardly, with the effect that the endings of the plate are directed slightly caudad.In O. leucostoma (Wd.), however, both the anterior and the posterior margins of theanal plate run parallel to the segment border. Near the posterior border of theabdominal segments are 1-2 rows of closely set series of minute spinules. In O.leucostoma (Wd.), these spinules are larger and are irregularly arranged. The larvae breed chiefly in feces of domesticated birds or animals and also ingarbages. 4. Musca convexifrons Thoms.(fig.9) Pupa: Puparium brownish grey. The posterior spiracles are heavily chitinizedwith much sinuously convoluted spiracular slits. There are no spinules along thedorsal grooves of the 8th abdominal segment. The lateral portion of the anal plateis square shaped. On the ventral pads of the abdominal segments is a row of largespines, which is interrupted in the middle. On each side of the row are smallerspines arranged in 2 definit rows arteriorly, but are arranged irregularly posteriorly.Anterior to the anterior margin of the anal plate below the square shaped lateral.portion is an isolated single row of minute spines. As a whole the characteristics as given above are very similar to those givenby Zimin (1948) for the larva of M. larvipara Portsch. In fa

本文用检索表的方式报告了采自上海的50多种与人类杂处的常见蝇类和其他双翅类的幼虫鉴别特征;其中34种(内3种非上海产)有种的鉴别特征,其余的有些仅鉴别到属、亚科或科。对过去还未见记载的元厕蝇和斑跖黑蝇的幼虫、以及绯胫纹蝇和突额家蝇的蛹的形态,文内作了必要的描述。从绯胫纹蝇的口咽器和卵的形态看来,纹蝇属是与棘花蝇类很近缘的。

 
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