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wuhu
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  芜湖
     Investigation on E. coli O_(157_∶H_7 Infection in Animal Host in Wuhu Area
     芜湖地区肠出血性大肠杆菌O_(157)∶H_7流行病学调查
短句来源
     Investigation on E.coli O157:H7 in animal host in Wuhu area
     芜湖地区动物宿主携带O157:H7大肠杆菌的调查
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     The karyotype of L.radiata from Wuhu population was formulated as 2n=20+1B=1m+9T+4t+6st+1B and 2n=20+1B=1M+9T+10st+1B,belonging to Stebbin's (1971) 3B and 3C type. These new karyotypes and chromosome numbers of L.radiata were reported for the first time.
     生于芜湖的居群核型为 :2n =2 0 +1B =1m +9T +4t +6st +1B和 2n =2 0 +1B =1M +9T +10st+1B ,属于“3B”和“3C”核型。
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     Nitrite content of common vegetables in Wuhu City.
     芜湖市几种常见蔬菜中亚硝酸盐含量分析
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     Analysis of the characteristics of the atmospheric pollution of SO_2 in Wuhu urban area
     安徽省芜湖市市区大气SO_2污染特征分析
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  芜湖市
     Nitrite content of common vegetables in Wuhu City.
     芜湖市几种常见蔬菜中亚硝酸盐含量分析
短句来源
     Analysis of the characteristics of the atmospheric pollution of SO_2 in Wuhu urban area
     安徽省芜湖市市区大气SO_2污染特征分析
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     The application of modified BP algorithm used in NO_X air pollution of WuHu cityl
     改进的BP算法在芜湖市NO_X大气污染中的应用
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     Study of Blood Lead of Children at Age of 3-6 in Wuhu City
     芜湖市3~6岁儿童血铅含量的研究
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     Analysis of STD surveillant data in Wuhu, 1993~1998
     芜湖市1993~1998年性病监测资料分析
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  “wuhu”译为未确定词的双语例句
     The study showed that around Wuhu Plant,soil Cd,Zn and Pb mainly existed in Fe-Mn oxide form,and Cu in residual form,with the percentage of 31.81%,39.83%,53.79%,and 46.24%,respectively.
     研究了污染土壤、油菜籽中Cd、Cu、Zn、Pb含量、形态分布特征和重金属富集状况及可能存在的生物毒性. 结果表明,土壤中Cd、Zn、Pb以铁锰氧化物结合态、Cu以残留态占5种形态最高比例,分别为31.81%、39.83%、53.79%、46.24%;
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     Results:The incidence of birth defects from delivery during hospital stay in the People's Hospital of Wuhu County reached 12.20‰(37/3 033),which was close to the national incidence in China in 2004(12.84‰).
     结果:在该院分娩的围生儿出生缺陷发生率12.20‰(37/3033),与2004年全国围生儿出生缺陷发生率12.84‰接近;
短句来源
     Results Mean blood lead level was 78.5μg/L among 3~5 years old children in Wuhu. The blood lead level of 8.8% children was lower than 50 μg/L and that of 18.6% children was equal or more than 100 μg/L. The blood lead level of 41.1% children in Shi Cheng kindergarten was equal or more than 100 μg/L.
     结果 儿童血铅总体均值为 78.5μg/ L ,<5 0μg/ L的占 8.8%,≥ 10 0μg/ L占 18.6 %,在 5 0~ 10 0μg/ L之间的占 72 .6 %,其中石城幼儿园有 41.1%的儿童血铅≥ 10 0μg/ L。
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     Optimizing transport Structure and Perfecting Ecology Network——De-scription of the Conceptual Planning of Wuhu Area in Daqing City
     优化交通结构 完善生态网络——大庆市五湖地区概念规划解析
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     Type II : The karyotype formula is 2n = 22+lB=6st + 14t + 2T+lB (plate 1: 7, 8). The chromosomes range in length from 6.50 to 11. 02 um, with the ratio of the longest to the shortest 1. 70. The karyotype belongs to 4A. (3) Wuhu cultural type has a karyotype 2n = 33 -30st + 3t.
     另一是黄山产野生材料,观察到两个细胞型,绝大多数细胞为2n=22=12st+10t,极个别细胞出现2n=22+1B=6st+14t+2T+1B的情况,均属“4A”核型。
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  wuhu
The experimental value of [Ca2+]/s for the Wuhu Changjiang River water was 0.2597.
      
Geological and geochemical characters are discussed for the breccias in the Nanjing-Wuhu area, with special reference to their cryptoexplosive origin.
      
Cryptoexplosive breccias in Nanjing-Wuhu volcanic area: Geological characteristics and control on mineralization
      
The geology and geochemistry of porphyrite iron deposits in the Nanjing-Wuhu area, Southeast China
      
Since the "Conference on Foreign Philosophy" held in Wuhu in October 1978, the study of foreign philosophy in China has undergone a prosperous stage.
      
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The data of annual precipitation at Shanghai, Wenchow, Hangchow, Foochow, Nanchang, Wuhu, Kiukiang, Ningpo and Chun'an up to 1972 are treated as time series. The methods of trend analysis (by means of equidistanced point orthogonal polynomials), spectral analysis and linear filtering are applied to these series. It is concluded that the deficiency of water supply for Sin-an river reservoir during last decade was mainly caused by the macro-climatic change. Furthermore, the tendency of precipitation on Sin-an...

The data of annual precipitation at Shanghai, Wenchow, Hangchow, Foochow, Nanchang, Wuhu, Kiukiang, Ningpo and Chun'an up to 1972 are treated as time series. The methods of trend analysis (by means of equidistanced point orthogonal polynomials), spectral analysis and linear filtering are applied to these series. It is concluded that the deficiency of water supply for Sin-an river reservoir during last decade was mainly caused by the macro-climatic change. Furthermore, the tendency of precipitation on Sin-an river basin during ten years about from now on is infered from the results of linear filtering. The results of variance analysis and periodogram analysis fundamently coincide with this inference.

将上海、温州、杭州、福州、南昌、芜湖、九江、宁波、淳安的年降水量资料作为时间序列,进行趋势分析(利用等距点正交多项式)、谱分析和线性滤波。结果表明,六十年代新安江水库水量不足主要由大范围的气候振动引起。应用线性滤波的结果对今后十年左右的降水变化趋势作了推断。方差分析和周期图分析的结果与上述推断基本一致。

The data of annual precipitation at Shanghai,Wenchow,Hangchow,Fo- ochow,Nanchang,Wuhu,Kiukiang,Ningpo and Chun'an up to 1972 are treated as time series.The methods of trend analysis(by means of equi- distanced point orthogonal polynomials),spectral analysis and linear filtering are applied to these series.It is concluded that the deficiency of water supply for Sin-an river reservoir during last decade was mainly caused by the macro-climatic change.Furthermore,the tendency of precipitation on Sin-an river...

The data of annual precipitation at Shanghai,Wenchow,Hangchow,Fo- ochow,Nanchang,Wuhu,Kiukiang,Ningpo and Chun'an up to 1972 are treated as time series.The methods of trend analysis(by means of equi- distanced point orthogonal polynomials),spectral analysis and linear filtering are applied to these series.It is concluded that the deficiency of water supply for Sin-an river reservoir during last decade was mainly caused by the macro-climatic change.Furthermore,the tendency of precipitation on Sin-an river basin during ten years about from now on is infered from the results of linear filtering.The results of variance analysis and periodogram analysis fundamently coincide with this inference.

将上海、温州、杭州、福州、南昌、芜湖、九江、宁波、淳安的年降水量资料作为时间序列,进行趋势分析(利用等距点正交多项式)、谱分析和线性滤波。结果表明,六十年代新安江水库水量不足主要由大范围的气候振动引起。应用线性滤波的结果对今后十年左右的降水变化趋势作了推断。方差分析和周期图分析的结果与上述推断基本一致。

Based on the regional paleogeography, tectonic history and magmaticactivity, this paper deals with the Mesozoic tectonism and magmatism of thelower Yangtze Valley, and also discusses the relation between the mechanismand evolution of continental volcanism. After the beginning of Mesozoic time, the platform block of the lowerYangtze Valley was disintegrated. Under the influence of the northwardmovement of the Pacific Plate, a series of left-lateral deep faults were for-med in the eastern part of Chinese continent....

Based on the regional paleogeography, tectonic history and magmaticactivity, this paper deals with the Mesozoic tectonism and magmatism of thelower Yangtze Valley, and also discusses the relation between the mechanismand evolution of continental volcanism. After the beginning of Mesozoic time, the platform block of the lowerYangtze Valley was disintegrated. Under the influence of the northwardmovement of the Pacific Plate, a series of left-lateral deep faults were for-med in the eastern part of Chinese continent. Among them, the Tancheng-Lu-jiang deep fault is the largest one. From Isopach maps of different ages(Fig.2)we can see that the Tancheng-Lujiang deep fault hadn't any influence over all rock formations,except in Triassic time. Near the fault zone, atZhangbaling, Anhui, the upper Proterozoic schist has a radioactive age of 230-190 m. y., which denotes the age of dynamic metamorphism. In the studiedarea, the Tangcheng-Lujiang deep fault separates the Sino-Korea Plate onthe north-west from the South China Plate on the south-east. The Pre-Me-sozoic formations on both sides are from two quite different sedimentary ba-sins, and have a dislocation of several hundred kilometers. Late Jurassic vol-canics occur along the fault, while the Cretaceous sediments overlap thefault zone. The gravitational and magnetic fields (Fig. 3) suggest that theintrusion of basic and ultrabasic rocks occupy the fault zone. The fault planeis very steep and cuts deeply downwards. According to telluric measurement,it reaches to the upper mantle. Since Mesozoic time, Honshu-Taiwan island arc faced towards east, andobducted above the Pacific oceanic plate. A stretching sea, created behindthis area, i. e., the depression of epicontinental sea type, is attributive to theovercompensation of the upper mantle under southeast China. For the timebeing, this depression is enlarged. It is controlled by the NNE left-lateralfault and NEE spreading axis, we called it North Jiangsu-South Yellow SeaDepression. It is one of the epicontinental seas on the western Pacific. The Mesozoic tectonism of the lower Yangtze Valley is the combinationand interaction of these two kinds of movements. At first, the left-lateralmovement was dominant, and then the stretching (spreading in continent)gradually took place. So the shape and the cross-section of the depressionchanged with time (Fig. 5). Now, we divide the studied area into two parts: continental uplift andepicontinental depression, but as a whole, they are only a part of the conti-nental margin of western Pacific. Mesozoic magmatic activities spread widely over the area. Their locations,ages and rock compositions are closely related to their tectonic positions.They form a continuous evolutional series in space and time. Within thecontinental uplift, the main activities are batholitic intrusions, such as Huang-shan etc. They are intruded into the axial part of anticlinorium, composedmainly of granite or granodiorite. Small continental volcanics might occur inlocal downwarps. On the peripheral part of the continental uplift, there aresome stocks composed of granodiorite with clear differentiation.They are locat-ed at the axial part of folds. In the axial part of synclinorium, there is anotherkind of stocks with quite complex composition from granite to diorite andmonzonite. Upper Jurassic-Lower Cretaceous volcanics occur within local downwarps, such as Fanchang, etc. The main rock types are dacite, partlyrhyolite and rhyodacite, but andesite is very scarce. The volcanic series itselfconstitutes a synclinal downwarp, laid over by different pre-Mesozoic folds,mostly anticlines. On the peripheral part of epicontinental depression, intrusive activity isvery weak. There are some small stocks, mainly diorite. On the western partof the studied area, near Tancheng-Lujiang deep fault, there occur somesyenite batholiths. Continental volcanism spread widely over this area, form-ing large synclinal downwarps of more than thousand square kilometers. Themost famous ones are Nanjing-Wuhu and Lujiang-Zhongyang. Their mainrock types a

一、地质发育概况 长江下游地区在地质发育进程中历经了多次构造旋回,经受多期构造作用的迭加和改造。

 
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