Turbulent heat transfer in a tube fitted with serrated twist tape under rolling and pitching environments with applications to shipping machineries     

Shyy Woei Chang  Tong-Miin Liou  Kun-Tse Chen 《Ocean Engineering》2008,35(16):1569-1577

Turbulent heat transfer in a swinging tube with a serrated twist tape insert was experimentally examined to reveal the effects of swinging oscillations on heat transfer for such a swirl tube under sea-going conditions. This swirl tube swings about two orthogonal axes under single and compound rolling and pitching oscillations. A selection of Nusselt number (Nu) measurements illustrates the influences of swinging oscillations with and without buoyancy interaction on heat transfer performances. Single rolling or pitching oscillation with the swinging frequencies ranging from 0.333 to 1 Hz reduces heat transfer levels from the static references. Synergistic effects of compound rolling and pitching oscillations with either harmonic or non-harmonic rhythms improve heat transfer performances. Buoyancy effects in the swinging swirl tube elevate local Nu, but are weakened as the relative strength of swinging force increases. A set of heat transfer correlations is derived that permits the individual and interactive effects of single and compound swinging force effects with buoyancy interactions on the developed flow heat transfer value () to be quantified.  相似文献   

Reply to discussion on “Application of probabilistic neural network to design breakwater armor blocks” by Zekai Şen,Tarkan Erdik,Yavuz Karsavran     

Dookie Kim  Dong Hyawn Kim  Seongkyu Chang 《Ocean Engineering》2008,35(11-12):1284

  相似文献   

Propagation of a solitary wave over rigid porous beds   总被引：1，自引：0，他引：1  

Ching-Jer Huang  Mao-Lin Shen  Hsing-Han Chang 《Ocean Engineering》2008,35(11-12):1194-1202

The unsteady two-dimensional Navier–Stokes equations and Navier–Stokes type model equations for porous flows were solved numerically to simulate the propagation of a solitary wave over porous beds. The free surface boundary conditions and the interfacial boundary conditions between the water region and the porous bed are in complete form. The incoming waves were generated using a piston type wavemaker set up in the computational domain. Accuracy of the numerical model was verified by comparing the numerical results with the theoretical solutions. The main characteristics of the flow fields in both the water region and the porous bed were discussed by specifying the velocity fields. Behaviors of boundary layer flows in both fluid and porous bed regions were also revealed. Effects of different parameters on the wave height attenuation were studied and discussed. The results of this numerical model indicate that for the investigated incident wave as the ratio of the porous bed depth to the fluid depth exceeds 10, any further increase of the porous bed depth has no effect on wave height attenuation.  相似文献   

Latitudinal distribution of mesozooplankton in the off-equatorial northeastern Pacific before and after the 1998/99 La Niña event     

Kang JH  Kim WS  Chang KI 《Marine environmental research》2008,65(3):218-234

Factors affecting mesozooplankton distributions in the northeastern tropical Pacific Ocean were investigated using data obtained along a meridian line (5 degrees -12 degrees N, 131.5 degrees W) in the summers of 1998, 1999, and 2003. The survey periods corresponded to a sharp transition between the 1997-1998 El Ni?o and 1998-1999 La Ni?a events, the 1999 La Ni?a event, and near-normal conditions after the moderate 2002-2003 El Ni?o in the equatorial Pacific. A strong upwelling in the divergence zone from 10.5 degrees to 11 degrees N caused a shoaling of the thermocline depth (approximately 30 m), resulting in increases in nitrate and phytoplankton chlorophyll a (chl-a) concentrations, and, in turn, mesozooplankton abundance during the La Ni?a in 1999. In contrast, in 1998, remnants of El Ni?o characteristics, deeper thermocline depth (60-150 m) and warm surface water (>28 degrees C), led to low concentrations of nitrate, chl-a and low mesozooplankton abundance, except in the convergence zone around 7 degrees N. The thermocline depth and nitrate concentration obtained during the near-normal period in 2003 corresponded to intermediate values as compared to those obtained during El Ni?o and La Ni?a conditions. Interannual changes in the position and strength of ecotones, such as divergence and convergence zones, affected mesozooplankton community structure and cyclopoid-to-calanoid ratios along the 131.5 degrees W meridian line. The clustering pattern of the mesozooplankton community was mostly characterized by calanoid (mainly Clausocalanus sp.) and cyclopoid (mainly Oncaea sp.) copepods, accounting for most of the observed differences among groups during the study period. Cyclopoids and calanoids were more abundant in 1999 than in 1998 or 2003, with a sharp increase to the north, while they were less abundant to the north in 1998 and 2003. The cyclopoid-to-calanoid ratio peaked in the convergence zone in 1998 and the divergence zones in 1999 and 2003, apparently due to the strength and location of the ecotones. Principal component analysis (PCA) with environmental factors and dominant mesozooplankton groups showed that dominant groups were affected by nitrate and chl-a concentrations in 1998, by sigma-t (water density), nitrate and chl-a concentrations in 1999, and by sigma-t, salinity and chl-a concentration (except siphonophores) in 2003. Latitudinal distribution of thermocline depth before and after the 1998/99 La Ni?a event showed a distinct interannual difference. The abundance of mesozooplankton in the divergence zone in 1999 was distinctively higher than abundances found in the convergence and divergence zones in 1998 and 2003, which resulted from the shallow thermocline depth due to an intensified upwelling during the strong 1998-1999 La Ni?a event.  相似文献   

Application of integrated geophysical interpretation on accumulation body     

Caikun GAO Huakun DU Jingtian TANG Kangxiu WU Chang＇an XIAO Shiping WANG 《东北亚地学研究》2008,11(3):191-196

Integrated geophysical interpretation is a method of combinating different geophysics prospecting methods based on different physical properties of accumulation. As different geophysical methods own different interpretations and varying detection accuracies, the key issue becomes how to integrate the results of several geophysical methods to corrently carry out a comprehensive explanation. Based on different geophysical results, the authors proposed an integrated geophysical explanation method and successfully applied it in practical engineering problems.  相似文献   

对气氡脱气装置改造的几点认识   总被引：2，自引：1，他引：1  

邱鹏成  白占孝  常振广  赵昌军 《地震地磁观测与研究》2007,28(3):85-88

拆除了格尔木井原气氡脱气装置,针对该井冷水、大流量的实际情况,自行设计、制造了一套新的脱气装置,在其后的气氡观测中取得了良好效果,通过对改造前后氡值的分析,充分认识到了合理的脱气装置的重要性,形成了几点新的看法.  相似文献   

深海底热液活动研究热点   总被引：3，自引：0，他引：3  

夏建新  李畅  马彦芳 《地质力学学报》2007,13(2):179-191,118

深海底热液活动是现代海洋地质科学研究的前沿热点, 我国这方面的研究工作刚刚开展, 亟需对现有研究成果进行总结。本文对海底热液活动的调查研究过程和现状进行了回顾, 重点分析了热液喷溢动力过程的理论研究成果, 从实测事件数据的研究成果中找出了影响热液柱的形态和分布的各种因素, 并对热液烟囱和极端温度微生物等海洋学研究热点进行了分析, 为深海热液活动调查和理论研究提供基础。   相似文献   

Vertical structure of the M<Subscript>2</Subscript> tidal current in the Yellow Sea   总被引：2，自引：0，他引：2  

Seok Lee  Heung-Jae Lie  Cheol-Ho Cho  Sok Kuh Kang  William J. Teague  Kyung-Il Chang  Kyu-Min Song  Kyung-Hee Oh 《Ocean Science Journal》2011,46(2):73-84

The vertical structure of the M₂ tidal current in the Yellow Sea is analyzed from data acquired using an acoustic Doppler current profiler. The observed vertical profiles of the M₂ tidal current are decomposed into two rotating components of counter-clockwise and clockwise, and restructured using a simple one-point model with a constant vertical eddy viscosity. The analyzed results show that the internal fictional effect dominates the vertical structure of the tidal current in the bottom boundary layer. In the Yellow Sea, the effect of the bottom friction reduces the current speed by about 20–40% and induces the bottom phase advance by about 15–50 minutes. In the shallower coastal regions, the effects of bottom topography are more prominent on the vertical structure of tidal currents. The vertical profile of the tidal current in summer, when the water column is strongly stratified, is disturbed near the pycnocline layer. The stratification significantly influences the vertical shear and distinct seasonal variation of the tidal current.  相似文献   

梅花参中多糖提取工艺及含量测定的研究   总被引：13，自引：0，他引：13  

王远红  吕志华  姜廷福  刘畅  郭少媛 《中国海洋大学学报(自然科学版)》2005,35(6):987-990

采用正交设计L9（34）,研究梅花参（Thelenota ananas）中多糖的提取工艺,探讨并建立了测定海参多糖含量的方法.结果表明：最佳提取条件为1g样品加40mL 3%KOH溶液,40～45℃超声2h;且提取温度为首要的影响因素;产物经二次乙醇纯化的结果较好,粗多糖得率20.25%.多糖经单糖组成分析,岩藻糖含量达到70%以上.测得梅花参中总糖含量8.79%;糖醛酸含量0.95%.该实验操作简单,稳定可靠,重现性好,准确度高,为测定其它海参中多糖的含量提供了可靠的依据.  相似文献   

两个凡纳滨对虾家系体重与体长的关系   总被引：4，自引：0，他引：4  

张灵侠  沈琪  胡超群  张吕平  任春华  陈偿  梁泽廉  陈文林 《热带海洋学报》2006,25(1):23-26

凡纳滨对虾Litopeneaus vannamei家系的培育是遗传选育种的基础,其生长特性包括生长速度、体重与体长的关系等,是家系的表型特征。报道了凡纳滨对虾2个家系的体长与体重的关系。通过回归分析,凡纳滨对虾家系1体重(W)与体长(L)的关系为:W=0.0059L3.2809(R2=0.9931);家系2体重与体长的关系为:W=0.0059L3.2974(R2=0.9940),2个家系体重与体长的关系没有明显的变化,得出凡纳滨对虾体重与体长的关系为:W=0.0059L3.2895(R2=0.9934)。  相似文献