论徐连经济带建设   总被引：1，自引：0，他引：1  

沈正平 《地域研究与开发》1997,16(4):15-20

通过对徐连经济带在全省，淮海经济区中经济地位的分析，与省内宁镇扬，苏锡常两区的比较，找出本带经济中存在的问题及原因，提出加快其经济发展所拥有的优势区位，优越的自然条件和重要意义，并就点轴开理论本带建设布局中的应用进行了探讨。  相似文献   

华北板块北缘东段上三叠统的若干特征   总被引：1，自引：0，他引：1  

刘大瞻  刘跃文 《吉林地质》1992,11(4):1-7

位于华北板块与古蒙古洋板块的交接处、金银别河至白水滩一带的一套变质的陆相碎屑岩,前人命名为白水滩组,时代归属早侏罗世。80年代末笔者在此进行1∶5万区域地质调查,在该地层中采到了Neoclamites sp.,Cycadocarpiclium sp.,Uniohuang bogouensis(?)等重要分子,同时发现其被二长花岗岩(U—Pb 192.7Ma)侵入,暂与小营子组对比,将其时代归属为晚三叠世。该套地层分为上下两段,即下部砾岩段和上部砂岩段;地层褶皱形态复杂,断裂构造发育,新老地质体相互推覆掩盖,构成独特的地质景观。  相似文献   

Numerical and Experimental Study of the 3D Effect on Connecting Arm of Vertical Axis Tidal Current Turbine     

郭伟  康海贵  陈兵  谢宇  王胤 《海洋工程》2016,(1):83-96

Vertical axis tidal current turbine is a promising device to extract energy from ocean current. One of the important components of the turbine is the connecting arm, which can bring about a significant effect on the pressure distribution along the span of the turbine blade, herein we call it 3D effect. However, so far the effect is rarely reported in the research, moreover, in numerical simulation. In the present study, a 3D numerical model of the turbine with the connecting arm was developed by using FLUENT software compiling the UDF (User Defined Function) command. The simulation results show that the pressure distribution along the span of blade with the connecting arm model is significantly different from those without the connecting arm. To facilitate the validation of numerical model, the laboratory experiment has been carried out by using three different types of NACA aerofoil connecting arm and circle section connecting arm. And results show that the turbine with NACA0012 connecting arm has the best start-up performance which is 0.346 m/s and the peak point of power conversion coefficient is around 0.33. A further study has been performed and a conclusion is drawn that the aerofoil and thickness of connecting arm are the most important factors on the power conversion coefficient of the vertical axis tidal current turbine.  相似文献   

基于降水微物理特征测量仪的雨滴形状观测与分析   总被引：1，自引：1，他引：0  

舒小健  高太长  刘西川  胡帅  江诗阳 《气象》2017,43(1):91-100

利用自主研制的降水微物理特征测量仪开展降水观测试验,得到了大量的雨滴图像。研究了异常雨滴图像的形成原因和处理方法,以此为基础重点研究了在极坐标下基于Akima插值的数字雨滴图像矢量化方法,得到了雨滴平均形状特征和轴比分布特征。结果表明,直径小于1 mm的雨滴以圆形为主,在1.0~3.0 mm的雨滴以椭圆形为主,大于3.0 mm的雨滴逐渐呈现顶部凸起,底部偏平的形状;雨滴的平均轴比分布与经验分布一致,相互之间差异在±0.04 mm范围以内;雨滴的平均轴比与经验模型的差值在粒径3.4~3.8 mm出现峰值,该范围内的雨滴较经验关系具有更圆的形状特性。  相似文献   

Retrieving the surface axis of the Kuroshio off southern coast of Japan from SST data     

SHAO Quanqin  CHEN Zhuoqi  MA Weiwei 《海洋学报(英文版)》2007,26(1):1-11

1IntroductionThe remarkable shape of the axis of the Kuro-shio revealed by a simple zig-zag bathythermographwas surveyed in1965(Stommel,1972).This sur-vey revealed that the15℃isotherm at the200mdepth is indicative of the axis of the Kuroshio,and ithas be…  相似文献   

Second-order ridge axis discontinuities in the south Atlantic: Morphology,structure, and evolution   总被引：1，自引：0，他引：1  

N. R. Grindlay  P. J. Fox  K. C. MacDonald 《Marine Geophysical Researches》1991,13(1):21-49

Continuous along-axis Sea Beam coverage of the slow-intermediate spreading (34–38 mm yr⁻¹ full rate) southern Mid-Atlantic Ridge (25°–27°30′S and 31°–38° S) shows that the ridge axis is segmented by both rigid and non-rigid discontinuities. Following the model of Macdonald et al. (1988b), a hierarchy of four orders is proposed for ridge axis discontinuities based on a continuum of relative age and distance offset across the discontinuites. This paper discusses the characteristics associated with five second-order discontinuities found in the areas surveyed. First-order discontinuities represent rigid offsets, transform faults, whereas non-rigid discontinuities fall into the second, third and fourth orders. Like transform fault boundaries, second-order discontinuities have distinctive morphologic signatures both on and off-axis-discordant zones — and therefore are better defined than third- or fourth-order discontinuities. Second-order discontinuities are offsets that range in distance from less than 10 km to approximately 30 km and vary in age offset from 0.5 to approximately 2.0 m.y. The variable morphotectonic geometries associated with these discontinuities indicate that horizontal shear strains are accommodated by both extensional and strike-slip tectonism and that the geometries are unstable in time. Three characteristic geometries are recognized: (1)en echelon jog in the plate boundary where ridge axis tips overlap slightly, (2)en echelon jog in the plate boundary where ridge axes are separated by an extensional basin whose long axis is oriented parallel to the strike of the adjoining ridge axes, and (3) oblique offset characterized by a large extensional basin that is oriented approximately 45° to the strike of the ridge axes. In the case of the third type, evidence for short strands of strike-slip tectonism that link an obliquely oriented extensional basin flanking ridge tips is often apparent. Analysis of the detailed bathymetric and magnetic data collected over the second-order discontinuities and their off axis terrain out to 5–7 m.y. documents that second-order discontinuities can follow several evolutionary paths: they can evolve from transform fault boundaries through prolonged asymmetric spreading, they may migrate along strike leaving a V-shaped wake, and they may remain in approximately the same position but oscillate slightly back and forth. In addition, a small change in the pole of relative motion occurring 4–5 Ma is thought to have resulted in the initiation of at least one second-order discontinuity in the survey area. A geologic model is proposed which involves the interplay of lithospheric thickness, asymmetric spreading, temporal and spatial variability of along-axis magmatic input and changes in the poles of relative motion to explain the origin, morphology and evolution of second-order ridge axis discontinuities.  相似文献   

Estimating the Kuroshio Axis South of Japan Using Combination of Satellite Altimetry and Drifting Buoys   总被引：3，自引：4，他引：3  

Daisuke Ambe  Shiro Imawaki  Hiroshi Uchida  Kaoru Ichikawa 《Journal of Oceanography》2004,60(2):375-382

By tracking the locally strongest part of the sea-surface velocity field, which was obtained by integrating data of satellite altimeters and surface drifting buoys, we extracted the Kuroshio axis south of Japan every 10 days from October 1992 to December 2000. The obtained axes clearly express the effect of the bottom topography; three modes were observed when the Kuroshio ran over the Izu Ridge. The axis was very stable to the south of ‘Tosa-bae,’ off the Kii Channel. Mean current speed at the Kuroshio axis gradually increased from 0.65 m/s south of Kyushu to 1.45 m/s off Enshu-nada. This revised version was published online in July 2006 with corrections to the Cover Date.  相似文献   

节理统计锥体单元法的探讨     

李巍然 《中国海洋大学学报(自然科学版)》1993,(Z1)

本文提出在投影球内建立锥体单元统计系统,直接计算以产状表示的单元轴线与节理法线的夹角,统计该夹角小于单元锥角半角的数目。统计结果更合理、可靠。  相似文献   

冲绳海槽中段地球物理场及对其新生洋壳的认识   总被引：13，自引：1，他引：13  

梁瑞才  王述功  吴金龙 《海洋地质与第四纪地质》2001,21(1):57-64

通过对冲绳海槽中的磁场进行分析，在海槽轴部追踪到了线性磁条带异常。另外，在扩张轴附近也拖到了新鲜拉斑玄武岩。重力自由空气异常值较低。根据这是由于深部地幔大幅上升所致。地震剖面及磁力资料显示在海槽轴部有强磁性浅层侵入体及海底山，这些侵入体很可能来自于深部地幔。高温地幔物质上涌在海槽轴部形成高热流、强磁异常、多火山以及热液活动。上述现象说明冲绳海槽中段张裂轴部大陆岩石圈已经破裂，并可能已有新生洋壳形成。  相似文献   

水平轴潮流能水轮机水动力数值模拟研究     

侯二虎  杜敏  王兵振 《海洋技术学报》2015,34(4):74-79

针对水平轴潮流能水轮机,对其进行了力学分析并运用CFD方法对其水动力性能进行了仿真计算。比较了定常计算与非定常计算结果的区别,运用定常计算(MRF)方法得到了表现水轮机性能的功率、扭矩和推力特性曲线,分析了水轮机在不同尖速比时的表现。对水轮机模型进行了拖曳水池试验,并与仿真数据进行了比对分析,两者吻合度较好,并分析了试验过程中出现的在尖速比较大时功率系数衰减的现象,表明CFD方法对水轮机的工程实践有着指导意义。得到了尾流场的速度云图、流线分布图与衰减曲线,结果表明相对于水轮机的直径,受到其影响后的流场存在扩张现象。分析了水轮机后不同位置处的流场衰减情况,结果显示,随着水轮机后轴向距离的不同其速度恢复差别很大,对于今后潮流能水轮机的大规模布置方式研究提供了依据。  相似文献