flow的过去式

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flow的过去式

篇1:flow的过去式

flow例句分享

The river is flowing slowly.

河水缓缓地流动。

The lines in this painting flow.

这幅画的线条很流畅。

The lava flowed down the sides of the volcano.

熔岩沿火山坡面涌流而下。

篇2:flow的过去式和用法例句

flow的过去式和其他时态:

过去式: flowed

过去分词: flowed

现在分词: flowing

flow的用法:

flow的用法1:flow的基本意思是指如液体流动般地运动,可以是大量地,也可以是少量地; 可以是缓慢地,也可以是急速地。强调持续不断。可用于液体、车流、电流、语流等。flow还可表示“垂”或“飘拂”。

flow的用法2:flow是不及物动词,其后可接away表示“流走”; 接from表示“从…流走”; 接in表示“流入”; 接out表示“流出”; 接over表示“泛滥”; 接to表示“流向”; 接with表示“被…淹过”或“富有…”。

flow的用法3:flow表示位置的移动时相当于表存在的动词be,可用于there flow句型,且须主谓倒装。

flow的过去式例句:

1. In that moment a surge of hatred flowed through my blood.

那一刻,一股仇恨在我的血液中翻涌。

2. A lot of this information flowed through other police departments.

大量此类信息在警察机关其他部门中流传。

3. The square was packed, and the cobbled streets flowed with coloured petals.

广场上挤满了人,鹅卵石铺就的街道上满是五颜六色的花朵。

4. The wine flowed and we danced the night away.

我们喝了很多酒,跳了一个晚上的舞。

5. His words flowed more readily.

他说得更加流利了。

6. She watched aghast as his life flowed away.

看着他的生命逐渐消逝,她惊骇万分。

7. Waves of emotion flowed across his huge face.

他那张大脸上一时间表情千变万化。

8. A stream of blood flowed from the wound.

一股鲜血从伤口流出来。

9. He was so mulish that my admonitions just flowed over him.

他很顽固,我的告诫对他只不过是耳边风.

10. The lava flowed down the sides of the volcano.

熔岩沿火山坡面涌流而下.

11. The river flowed to the east.

河水向东流去.

12. The words flowed unbidden from my pen.

这些字句从我的笔端滚滚流出.

13. Her hair flowed down her back.

她的头发飘垂在背后.

14. The crowd flowed out of the station.

人群涌出车站.

15. The river flowed over the bank.

河水漫过堤岸.

篇3:Information flow and controlling in

Information flow and controlling in regularization inversion of quantitative remote sensing

In order to minimize uncertainty of the inversed parameters to the largest extent by making full use of the limited information in remote sensing data, it is necessary to understand what the information flow in quantitative remote sensing model inversion is, thus control the information flow. Aiming at this, the paper takes the linear kernel-driven model inversion as an example. At first, the information flow in different inversion methods is calculated and analyzed, then the effect of information flow controlled by multi-stage inversion strategy is studied, finally, an information matrix based on USM is defined to control information flow in inversion. It shows that using Shannon entropy decrease of the inversed parameters can express information flow more properly. Changing the weight of a priori knowledge in inversion or fixing parameters and partitioning datasets in multi-stage inversion strategy can control information flow. In regularization inversion of remote sensing, information matrix based on USM may be a better tool for quantitatively controlling information flow.

作 者:YANG Hua XU Wangli ZHAO Hongrui CHEN Xue Wang Jindi  作者单位:YANG Hua,ZHAO Hongrui,CHEN Xue,Wang Jindi(Research Center for Remote Sensing and GIS, School of Geography, Beijing Normal University, State Key Laboratory of Remote Sensing Science, Beijing Key Laboratory for Remote Sensing of Environment and Digital Cities, Beijing 100875, China)

XU Wangli(Department of Mathematics, Beijing Normal University, Beijing 100875, China)

刊 名:中国科学D辑(英文版)  SCI英文刊名:SCIENCE IN CHINA (EARTH SCIENCES) 年,卷(期): 48(1) 分类号:P3 关键词:regularization inversion   information flow   Shannon entropy decrease   information matrix  

篇4:Stability of stratified flow and slu

Stability of stratified flow and slugging in horizontal gas-liquid flow

A transient one-dimensional two-fluid model is proposed to investigate numerically the interfacial instability and the onset of slugging for liquid-gas flow in a horizontal duct. In the present model, the effects of surface tension and transverse variations in dynamic pressure are taken into account. The evolution of interfacial disturbances is displayed and compared with the linear viscous KelvinHelmholtz stability analyses. It shows that interfacial wave is more instable due to the non-linear effect. The model predicts well the stability limit of stratified flow in comparison with the experimental data, and also automatically tracks the onset of slugging. The results show that the initiation of hydrodynamic slugging is related to local interfacial instability. Based on the cycle of slugging, a model for slug frequency is presented, which predicts the trends of slug frequencies with gas/liquid flow rate well in comparison with the available data. The effects of physical properties on slugging have been examined. It is found that with the increase in the gas viscosity and liquid density the slugging would be inhibited, whereas, with the increase in liquid viscosity and gas density, the slugging can be promoted.

作 者:GU Hanyang GUO Liejin  作者单位:State Key Laboratory of Multiphase Flow in Power Engineering, Xi'an Jiaotong University, Xi'an 710049, China 刊 名:自然科学进展(英文版)  SCI英文刊名:PROGRESS IN NATURAL SCIENCE 年,卷(期):2005 15(11) 分类号:P3 关键词:two-fluid model   Kelvin-Helmholtz stability   interfacial instability   onset of slugging   gas-liquid stratified flow  

篇5:Numerical model of flow and pollutan

Numerical model of flow and pollutant transportation in non-orthogonal curvilinear coordinates

Abstract:The planar 2D k-ε double equations' turbulence model was adopted and transformed into non-orthogonalcurvilinear coordinates. The concentration convection-diffusion was introduced to planar 2D SIMPLEC algorithm offlow in non-orthogonal curvilinear coordinates. The numerical model of pollutant transportation in non-orthogonalcurvilinear coordinates was constructed. The model was applied to simulate the flow and pollutant concentrationfields. In the testing concentration field, two optimal operations of contamination discharging both along bank and inthe centerline at the first bend of the meandering channel were adopted. Comparison with available data showed themodel developed was successful, was valuable to engineering application.作 者:WU Xiu-guang    SHEN Yong-ming    ZHENG Yong-hong    YANG Zhi-feng  作者单位:WU Xiu-guang,SHEN Yong-ming(State Key Laboratory of Coastal and Offshore Engineering, Dalian University of Technology, Dalian 116024, China)

ZHENG Yong-hong(Guangzhou Institute of Energy Conversion, Chinese Academy of Sciences, Guangzhou 510070, China)

YANG Zhi-feng(Institute of Environmental Science, Beijing Normal University, Beijing 100875, China)

期 刊:环境科学学报(英文版)  ISTICSCI  Journal:JOURNAL OF ENVIRONMENTAL SCIENCES 年,卷(期):, 16(2) 分类号:X131.2 Keywords:curvilinear coordinates    diffusion-transportation    SIMPLEC algorithm    concentration fields    meandering channel   

篇6:Prevention of debris flow disasters

Prevention of debris flow disasters on Chengdu-Kunming Railway

Chengdu-Kunming Railway is an important transport line on southwestern China. However, this railway's safety is often threatened by debris flows. How to effectively forecast and alarm the debris flow disasters and reduce the losses is the aim to study the prevention system in this paper. The factors to cause or influence debris flow are divided into four parts――the basin environmental factors, the basin meteoric factors, the prevention work's elements and the flood-relief work's elements, and the prevention system is made up of three models――a judgment model to assess the debris flow gully's seriousness, a forecast model to predict the debris flow's occurrence and an alarm model to evaluate the debris flow's disaster. Afterwards, a concise structure chart is worked out and verified by the field data from Chengdu-Kunming Railway. This prevention system will provide beneficial reference for the debris flow's monitoring network to be executed on Chengdu-Kunming Railway.

作 者:WANG Wei XU Wei-lin Liu Shan-jun  作者单位:State Key Hydraulics Lab. of High Speed Flow, Sichuan University, 刊 名:环境科学学报(英文版)  ISTIC SCI英文刊名:JOURNAL OF ENVIRONMENTAL SCIENCES 年,卷(期): 13(3) 分类号:X4 关键词: 

篇7:STUDY ON INTERMITTENT SHEAR FLOW AND

STUDY ON INTERMITTENT SHEAR FLOW AND RELAXATION BEHAVIOR OF THERMOTROPIC LIQUID CRYSTALLINE POLYMER

Intermittent shear flow including start-up flow and small oscillatory amplitude time sweep or stress relaxation after cessation of shear flow was used to study the rheological behavior and internal structure of thermotropic liquid crystalline polymer (TLCP). There are two kinds of intermittent shear flow: all start-up flows are in the same direction (intermittent flow forward: IFF) and start-up flows change their directions alternately (intermittent flow reversal: IFR). The results show that the stress of start-up flow of IFF and IFR in the test process is not superposed, indicating different changes of internal structure of thermotropic LCP (TLCP). Two main factors affect structure changes in the experimental time scale. One relates to long-term texture relaxation process, the other is an interchain reaction that becomes important after 30 min. The two factors raise the stress of IFF, but express complex effects for the stress of IFR. The latter factor becomes very important at long time annealing process. The relaxation behavior was also studied by the application of wide range relaxation spectrum calculated from the combined dynamic modulus, which gave three characteristic relaxation times (0.3, 10 and 600 s)ascribable to the relaxations of less-phase orientation, domain orientation, and domain deformation, respectively. The result also shows that the domain coalescence (texture relaxation), a long relaxation time, is a much slow process and lasts beyond 2400 s of the test time.

作 者:Ruo-Bing Yu Chi-xing Zhou Wei Yu  作者单位:Department of Polymer Science and Engineering, Shanghai Jiao Tong University, Shanghai 40, China 刊 名:高分子科学(英文版)  ISTIC SCI英文刊名:CHINESE JOURNAL OF POLYMER SCIENCE 年,卷(期): 23(3) 分类号:O6 关键词:Intermittent shear flow   Relaxation behavior   Thermtropic liquid crystalline polymer (TLCP)  

篇8:A NOTE ON THE MEAN CURVATURE FLOW IN

A NOTE ON THE MEAN CURVATURE FLOW IN RIEMANNIAN MANIFOLDS

作 者:Chen Xuzhong Shen Yibing  作者单位:Department of Mathematics, Zhejiang University, Hangzhou 310027, China 刊 名:数学物理学报(英文版)  ISTIC SCI英文刊名:ACTA MATHEMATICA SCIENTIA 年,卷(期):2010 30(4) 分类号: 关键词:Mean curvature flow   singularity   hypersurface   weakly convexity  

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