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阻拦
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  “阻拦”译为未确定词的双语例句
     And in the mouth of the bay, the concentration of NO_3~- increased about 35%(0.1mg/l). In Xuamen Bay, the concentration of NO_3~- reduced 90%(0.1 ~0.3mg/l) corresponding to the blocking;
     在湾口,NO_3~-浓度也有35%(0.1mg/l)左右的升高,而在漩门湾,由于物质受到堵坝工程的阻拦,NO_3~-浓度产生了90%以上(0.1~0.3mg/l)的相应减小;
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     By analyzing the characteristics movement of soil water flow and preferential flow through water discharge, flux and velocity, it shows that the flow in soil water movement in the researched four successive stages mainly exhibits preferential flow, and the matrix part of soil exhibits non-move area;
     根据出流液的流量、通量及流速来分析土壤水流及优先流特征。 研究发现研究区域内4个演替阶段的土壤水分运动的壤中流过程主要表现为优先流,而土壤中的基质部分,则表现为不动区域,并且一旦优先流路径形成,土壤将不再阻拦水入渗,导致随后的降雨入渗穿过前面已经湿润的、已经存在的优先路径。
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     A non-intercepting beam monttor system for a 20 MeV linear electron accelerator
     20MeV电子直线加速器无阻拦束流监测系统
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     The mechanism of this coexistence corroding tubular goods and its influenced factors are emphatically discussed in theory. It is tentatively found that when H_2S coexists with CO_2,the mechanism is likely that in liquid phase,first CO_2 acts on steel to generate FeCO_3; then H_2S acts on FeCO_3 to generate even more stable FeXSY;
     重点从理论上探讨了CO2和H2S共存时对油气管材的腐蚀机理及其影响因素,初步发现:当H2S和CO2共同存在时,其机理可能是CO2在液相中与钢先发生作用生成FeCO3,H2S在液相中与FeCO3反应生成了更为稳定的FexSy,在液相中,FexSy吸附层对离子的迁移起到了部分的阻拦作用。
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     The role of water conservancy facilities was discussed in relation to preventing sediments from entering the main channel of Yangtze River.
     然后 ,进一步探讨了长江上游水利工程在阻挡流失水土进入长江主河道过程中的地位和作用 ,探讨表明 ,这些水利工程有效地阻拦了流失水土进入长江河道 ;
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     It is believed that root proof materials are very important to the system.
     根阻拦材料在种植屋面中显得十分重要.
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     A STUDY ON THE INTERCEPTING MECHANISM OF AN AIR-BUBBLE CURTAIN ON BLACK PORGY (SPARUS MACROCEPHALUS)
     气泡幕对黑鲷阻拦作用机制初探
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Discourage free riding in Peer-to-Peer file sharing systems with file migration and workload balancing approach
      
A file migration and workload balancing based approach (FMWBBA) to discourage free riding is proposed in this paper.
      
Watermark embedding is a method to discourage unauthorized copying and identify the owner or distributor of digital data.
      
Such an evaluation will, in most cases, be favourable and should therefore not discourage consumption of probiotics.
      
reducing the waiting list, sending appointment reminders) may be counterproductive as they can discourage successful active problem coping.
      
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This article presents the physical concept about controlled blasting with half of the excavated rock on one side to a throw and half on the other loosened. Apart from providing the controlling .ranges of both Sides, it also deals with the basic principles concerning this type of blasting', method. .

本文提出了一侧抛掷和另一侧松动的抛松控制爆破的物理概念、抛松两侧控制范围和抛松控制爆破的基本原理。 通过实验观察和分析,得出抛松两侧最小抵抗线的合理抛松比K_(ps)、抛掷侧爆破作用指数n_p和松动侧爆破作用指数n_s的计算方法及控制条件。 为了保护松动侧的各种建筑物、构筑物和工业设施等,专门设计了防止空气冲击波的防冲屏、降低爆破地震波作用的防震沟以及阻拦滚石的拦石壩。经实践检验和测定,证明这些屏、沟、壩是切实可行的对松动侧的有效保护措施。

The wusong Jiang is a Chief waterway from the Taihu Lake to Shanghai. It flows 125 kilometers.The upper and Lower reaches are narrower than the middle.This is due to its physical evolution as well as the effects of human activities. Before the end of the Tang Dynasty,its source was the Taihu kou (太湖 口),situated to the south of Wu-jiang xian.Its Lower reaches were the Qiu- jiang (old River) where it emptied into the sea.The river mouth was about 10 KM wide. The building of the Long Bridge at Wujiang xian in the...

The wusong Jiang is a Chief waterway from the Taihu Lake to Shanghai. It flows 125 kilometers.The upper and Lower reaches are narrower than the middle.This is due to its physical evolution as well as the effects of human activities. Before the end of the Tang Dynasty,its source was the Taihu kou (太湖 口),situated to the south of Wu-jiang xian.Its Lower reaches were the Qiu- jiang (old River) where it emptied into the sea.The river mouth was about 10 KM wide. The building of the Long Bridge at Wujiang xian in the Northern Song Dynasty prevented the water flowing from the Taihu Lake,while the tides flew up into the lower reaches,causing the river being silted rapidly, and so dredging was continually required.At that time,the river mouth reached to south Changpu kou (南跄浦口).This mouth was silted up gradual- ly in the early period of the Southern Song Dynasty.In the middle of the Southern Song Dynasty,due to the building of Lihu Dam (里护塘),Dong- jiang (East River) no longer emptied into the sea and compelled the rivers in North Zhejiang plain to drain into Huangpu (黄浦).Thus the Huangpu River became wider and wider,though it still remained as a tributary of the wusong Jiang. In the Ming and Qing Dynasty,the original upper source,Taihu kou, became shallower and narrower gradually,then Guajin kou (瓜泾口) became the chief source of the Wusong Jiang.In the middle of the Ming Dynasty,the lower reaches ran along the present cource,hence it became a tributary of the Huangpu Jiang.In the early period of the Qing Dynasty,Old Dam and New Dam were built.In the middle of the Qing Dynasty,the Huangdu canal (黄渡 越河) was constructed,and the present river system is thus formed.

吴淞江是太湖流域通至上海的一条重要航道。全长125公里。今日的河道形成两端狭中段宽的特殊形态,乃是长期自然演变及人为治理的结果。在唐末以前,它源出吴江县以南的太湖口,下游在今上海市区的原虬江道入海,当时河口宽达10公里。北宋时期由于吴江修筑了长桥,阻拦了太湖下泄的水量,下游由于潮汐倒灌,日益浅,以后曾不断进行治理。当时河口已到达南跄浦口,此口在南宋初期淤没。南宋中期由于修建了里护塘,阻断了东江下游出口,迫使浙江北部平原的水流均汇入黄浦,使黄浦日益增大,但它仍为吴淞江的支流。明清时期,吴淞江上源太湖口逐渐浅狭,遂以瓜泾口为正源。明代中叶下游引入今道,成为黄浦江的支流。清代初期下游曾修建老闸及新闸,中期又开凿黄渡越河,遂形成今日的全部河道。

The wusong Jiang is a Chief waterway from the Taihu Lake to Shanghai. It flows 125 kilometers. The upper and Lower reaches are narrower than the middle. This is due t0its physical evolution as well as the effects of human activities. Before the end of the Tang Dynasty, its source was the Taihu kou (太湖口), situated to the south of Wu-jiang xian. Its Lower reaches were the Qiujiang (old River) where it emptied into the sea. The river mouth was about 10 KM wide. The building of the Long Bridge at Wujiang xian in...

The wusong Jiang is a Chief waterway from the Taihu Lake to Shanghai. It flows 125 kilometers. The upper and Lower reaches are narrower than the middle. This is due t0its physical evolution as well as the effects of human activities. Before the end of the Tang Dynasty, its source was the Taihu kou (太湖口), situated to the south of Wu-jiang xian. Its Lower reaches were the Qiujiang (old River) where it emptied into the sea. The river mouth was about 10 KM wide. The building of the Long Bridge at Wujiang xian in the Northern Song Dynasty prevented the water flowing from the Taihu Lake, while the tides flew up into the lower reaches, causing the river being silted rapidly, and so dredging was continually required. At that time, the river mouth reached to south Changpu kou (南跄浦口). This mouth was silted up gradually in the early period of the Southern Song Dynasty. In the middle of the Southern Song Dynasty, due to the building of Lihu Dam (里护塘), Dongjiang (East River) no longer emptied into the sea and compelled the rivers in North Zhejiang plain to drain into Huangpu (黄浦). Thus the Huangpu River became wider and wider, though it still remained as a tributary of the wusong Jiang. In the Ming and Qing Dynasty, the original upper source, Taihu kou, became shallower and narrower gradually, then Guajin kou (瓜泾口) became the chief source of the Wusong Jiang. In the middle of the Ming Dynasty, the lower reaches ran along the present cource, hence it became a tributary of the Huangpu Jiang. In the early period of the Qing Dynasty, Old Dam and New Dam were built. In the middle of the Qing Dynasty, the Huangdu canal (黄渡越河) was constructed, and the present river system is thus formed.

吴淞江是太湖流域通至上海的一条重要航道。全长125公里。今日的河道形成两端狭中段宽的特殊形态,乃是长期自然演变及人为治理的结果。在唐末以前,它源出吴江县以南的太湖口,下游在令上海市区的原虬江道入海,当时河口宽达10公里。北宋时期由于吴江修筑了长桥,阻拦了太湖下泄的水量,下游由于潮汐倒灌,日益淤浅,以后曾不断进行治理。当时河口已到达南跄浦口,此口在南宋初期淤没。南末中期由于修建了里护塘,阻断了东江下游出口,迫使浙江北部平原的水流均汇入黄浦,使黄浦日益增大,但它仍为吴淞江的支流。明清时期,吴淞江上源太湖口逐渐浅狭,遂以瓜泾口为正源。明代中叶下游引入今道,成为黄浦江的支流。清代初期下游曾修建老闸及新闸,中期又开凿黄渡越河,遂形成今日的全部河道。

 
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