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dancing
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  舞蹈
     Design of Dancing Robot’s Control System Based on 80C196KC Single Chip Computer
     基于80C196KC单片机的舞蹈机器人控制系统设计
短句来源
     The super scale is 35%、 25%、 10% at dancing colledge chaoyang and shunyi in summer in 2002,respectively.
     2002年夏季观测试验期间舞蹈学院、朝阳和顺义三个测点O_3超标率分别为35%、25%、10%。
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     Principles and Methods of Training and Teaching of Gymnastic Dancing
     体操舞蹈训练的原则和方法
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     An Analysis and Study of Breathing in Dancing
     舞蹈呼吸分析研究
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     Dancing Therapy:from body to soul
     舞蹈治疗:从身体到心灵
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     (6) The items instructed are in a decreasing sequence Taiji (55.7%), exercising and dancing (46.3%), Qigong (34.6%) and Ping Pang (12.9%), tennis (10.8%) and ball catch (8.1%);
     (6)指导项目依次为太极拳、剑(55.7%),操类(46.3%),气功(34.6%),乒乓球(12.9%),网球(10.8%),门球(8.1%);
短句来源
     antiphonal singing and dancing continued 27-180 second, female was usually 27-50 second, male was usually 1 minute to 1 minute and 36 second.
     对鸣对持续时间为27~180秒,雌鹤一般为27~50秒,雄鹤一般为1分至1分36秒。
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     Dancing of Capital & Industry
     张江:资本与产业共
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     According to records on historical materials, it is conventional to call the popular Tujia Baishou Dancing se~(53)pa~(53),zi~(55).
     土家地区普及的“摆手”,土家语叫se53pa53zi55(舍把日),早已约定俗成,历史文献多有记载。
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     The Plan and Practice of the Street Dancing Course in Universities
     普通高校街课程的设计与实践
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  跳舞
     Style in that period was not independent, it was behind the content, the theme and the figures, "Dancing with shackles".
     就文体意识而言,这一时期的文体并非独立的存在,而是隐藏于思想内容、题材主题和人物形象的背后,“戴着镣铐跳舞”。
短句来源
     Factor A is training mode, comprising two levels: A1, serial folk play training activities, i.e. experiment group; A2, non-folk play training activities, i.e. control group (in which training methods, such as dancing, singing and story-telling areused).
     因素A:训练方式,包括二个水平,A1:系列化的民间游戏训练,即实验组,A2:非民间游戏训练活动(如跳舞、唱歌、讲故事等),即对照组。
短句来源
     The fabrication of a dance robot,controlled by C8051F310 microprocessor was descvibed,which has some advantages such as simple,active movements,harmony in dancing and etc.
     以C8051F310单片机为控制器的核心,制作出了动作灵活、价格低廉、以及模块化结构的跳舞机器人。
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     Look forward the developing tendency of action skill learning from the fashion of dancing blanket
     从跳舞毯的风靡看动作技能学习的发展趋势
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     Dancing and Courtesy: Prohibition against Dancing in Tianjin in 1927
     跳舞与礼教:1927年天津禁舞风波
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  “dancing”译为未确定词的双语例句
     The total colonies qualified rate were 89% for hotels,88% for cafes,86% for libraries,82% for beauty parlours,81% for inns and restaurants,80% for department stores,70% for waiting rooms of hospitals,50% for barber's shops,9% for singing and dancing rooms,and 5% for table tennis rooms. The differences of different years and places were significant(χ~2=428.60,P<0.01).
     各类公共场所空气细菌总数合格率不同,饭店宾馆89%、咖啡厅88%、图书馆86%、美容院82%、普通旅店和饭馆81%、商场80%、医院候诊室70%、理发店50%、歌舞厅9%、乒乓球馆5%,差别有统计学意义(χ2=428.60,P<0.01)。
短句来源
     the forms of exercising body slimming are running (47.1%) and aerobics dancing (45.6%);
     运动瘦身方式是跑步(47.1%)、健身操(45.6%)。
短句来源
     The article analyses the merits and demerits of the electrically controlled system of 11/360 and 8/600 dancing drwing machine by contrast,and approaches some questions in the remake on 8/600 by using 11/360 electrically controlled principles.
     分析比较了11/360和8/600活套式拉丝机电控系统的优缺点,探讨了用11/360电控原理对8/600进行改造中的几个问题。
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     Feature Expression of Digital Dancing Art and Technique of Video Retrieval
     数字化舞蹈艺术的特征表达与视频检索技术
短句来源
     \ \ Research and Design on the Electric Controlling System of the Multi function dancing
     多功能舞台电气控制系统的研究与设计
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  dancing
Dancing for hours at a Technoparty without adequate volume replacement preceded his first urgent admission to hospital.
      
Christina Schoch: Dancing Queen und Ghetto Rapper.
      
Of Dancing Cardinals and Mestizo Madonnas: Reconfiguring the History of Roman Catholicism in the Early Modern Period
      
Dancing for god or the devil: Pentecostal discourse on popular dance in Kinshasa
      
DANCING IN SACRED SPACE: SOME REFLECTIONS ON LITURGY AND PERFORMANCE
      
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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

~~

As the UJ-25 Type D.C. Poten-tiometer being used, the accuracyof analysis by FISE has been comeup to 0.1 millivolt (mv).The table,on which the millivolt could becollverted into the content of fluoridein biological samples and the sameaccuracy could be revealed clearly,has been compiled, according to thecalculative method reported by theDepartment of Health Statistics ofthe School of Public Health, SichuanMedical College. It is, therefore,quite accurate and convenient forapplying. The standard set up bycalculative...

As the UJ-25 Type D.C. Poten-tiometer being used, the accuracyof analysis by FISE has been comeup to 0.1 millivolt (mv).The table,on which the millivolt could becollverted into the content of fluoridein biological samples and the sameaccuracy could be revealed clearly,has been compiled, according to thecalculative method reported by theDepartment of Health Statistics ofthe School of Public Health, SichuanMedical College. It is, therefore,quite accurate and convenient forapplying. The standard set up bycalculative method is better than thatset up by the general method in respectof representation. Using the permissiblerange of fluctuation of mv,the examinerscan directly and easily find out whetherthe results of analysis are right or not. There are two points should benoticed, 1. The straight part of thestandard should be set up by generalmethod before the calculation. Afterthat this step could be omitted inidentical conditions. 2. The contentof fluoride of the standard series inanalysis must be designed in accor-dance with geometrical progression sothat the relevant content of logarithmcould be arithmetic progression. As aresult, a simple and direct methodpublished in the same report by theDepartment of Health Statitsics couldbe applied in the calculation of thetable and then you could look up theK in that one. The treatments of biologicalmaterials and the control of condi-tions in analysis will be reported inthe future.

本文报导采用UJ—25型直流电位差计,使选择性电极测氟的精密度提高到0.1mv。为准确、简便地反映这种精密度和有效地控制检验质量,本文用计算法编制了“毫伏数—含氟量对照表”,并确定了“毫伏数实测值允许波动范围”。还对简捷编表法作了说明。

An investigation was carried out to study the cause of bailure of high speedfurging dies,which are made from 4CrSW2VSi steel,and employed in hot shapingof steam turbine blades.It was found that the life of the die was dependent on thehardness of the die.When the die was hardened in the range of HRC 50~51 thatpremature bailure occurred.It caused lower life for die.When the die was hardenedin the range of HRC 46~48 the life of the die can be increased on two time.The reason for the effect on the life of the die...

An investigation was carried out to study the cause of bailure of high speedfurging dies,which are made from 4CrSW2VSi steel,and employed in hot shapingof steam turbine blades.It was found that the life of the die was dependent on thehardness of the die.When the die was hardened in the range of HRC 50~51 thatpremature bailure occurred.It caused lower life for die.When the die was hardenedin the range of HRC 46~48 the life of the die can be increased on two time.The reason for the effect on the life of the die arising difference in hardnessis thought to be related to fracture toughness of the die steel.The results of metallographic examination showed that grain boundary carbideprecipitates in the die steel can lead to a intergranular crack prcpagaticn.Therefore,avoi-dance of such grain boundary precipitates can produce more higher life of the die.

本文对寿命不同的三个4Cr5W2VSi 钢制汽轮机叶片高速锤凹模进行了失效分析。其结果指出:模具寿命高低与模具的硬度有密切的关系。当模具硬度高于HRC50—51时,会产生早期脆断,寿命很短。当横具的硬度降低到HRC47—48时,模具早期脆断基本消失,使模具寿命可稳定地提高2倍。金相分析结果又指出,当热处理时沿晶界析出网状碳化物时,裂纹是沿晶扩展的,晶界上未析出网状碳化物裂纹是穿晶的,如能避免在晶界上析出网状碳化物还可进一步提高模具寿命。

 
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