配位吸附波测定粮食中的痕量钼

在0.1 mol/L HAc-NaAc(pH=3.7)介质中,Mo(Ⅵ)-NCP配合物在2.5次微分极谱图上产生良好的吸附还原波。其峰电位为-0.54 V,峰电流与Mo(Ⅵ)浓度在8.0×10-8～6.0×10-6mol/L范围内呈良好的线性关系,检测限为5.0×10～8mol/L。应用该法测定了豆类样品中的微量钼,获得了满意的结果。研究了配合物的组成,极谱波的性质及其机理。     

三维数值波浪水池技术与应用

建立了用于波浪-结构物相互作用数值模拟的三维数值波浪水池．应用VOF方法对粘性流动的基本方程进行数值求解并描述其自由表面，水池计算域的一侧使用数值造波机条件产生斜入射波浪，其下游开边界联合使用辐射条件和局部强迫衰减，侧向边界使用周期性条件使斜向波浪透过．数值试验表明，所建立的三维数值波浪水池产生和传播波浪具有良好的重复性和稳定性，应用于海洋结构物波浪荷载的确定也是可靠的．     

He原子基态能量与波函数的变分计算

在He原子模型研究的基础上,采用了一种包含坐标张弛系数的试探波函数,对He原子的基态能量和解析波函数进行了变分计算,得到了比较理想的结果,其中在波函数取N=11时,氦原子基态能量与实验值相比,误差仅为0.014‰.     

蛇形多向不规则波造波机波浪产生方法及特性

介绍了自行研制的蛇形多向不规则波造波机系统．造波机宽28m，由70块高0.9m、宽0.4m的造波板组成．在此基础上论述了分段式造波机产生波浪的原理及方法，并对其产生的斜向和多向不规则波的波浪统计特性以及波浪的频谱和方向分布进行了试验研究．结果表明，研制的造波机各项性能达到了预期的指标，可产生较理想的单向和多向不规则波．     

波阻抗反演技术在孤东地区馆陶组薄储层描述中的应用

根据一维波动方程的拟合迭代法原理 ,给出了求解波阻抗σ(x)的算法。针对孤东地区馆陶组薄储层油藏存在的地层埋深浅、较疏松以及井径变化大泥岩中含有膨化矿物蒙脱石等引起的声波测井速度失真问题 ,采用分段函数法对其进行了校正。将校正后的声波资料进行反演 ,可得到高质量的资料 ,用该校正资料追踪描述的储层与录井结果吻合较好。应用结果表明 ,测井资料在反演中可以补充地震资料缺少的低频和高频分量 ,地震波阻抗反演技术是薄储层描述的有效方法     

Instability of the shear layer in the near wake of a circular cylinder

The instability of the shear layer separated from a circular cylinder is studied with the Reynolds number (Re) of 3000～104 by numerically solving the two-dimensional Navier-Stokes equations. In the wake of the cylinder, primary vortex shedding with natural frequency fs occurs, and the instability of the shear layer with frequency ft develops, which leads to mixing layer eddies and interacts with the primary shedding vortices. However, there remains some uncertainties regarding to the variation of the shear layer characteristic frequency with the Reynolds number. Based on the previous experimental work, several relationships of ft/fs with Re has been proposed including ft/fs～Re0.5 by Bloor, ft/fs～Re0.87 by Wei and Smith and ft/fs～Re0.67 by Prasad and Williamson. The objective of this study is to predict reasonably the relation of the shear layer instability frequency with the Reynolds number based on the present accurate calculation with the high-order schemes and high-resolution spectrum analysis. According to our calculated results, a variation for the normalized shear-layer frequency of the form ft/fs～Re0.69 is predicted numerically, which is in good agreement with a recent experimental measurement of Re0.67 and physical prediction of Re0.7.     

磁空间群Pб_ 3/m''''m’c''''不可约共表示的计算

群表示理论在群论的发展和应用中占有十分重要的地位,它对求解C-G系数,同位标量因子及母分系数是必不可少的。本文主要以P6_3”m′m′c′的对称点L点为例,应用诱导表示的方法,介绍磁空间群不可约共表示的计算方法。     

浅层水中沉底爆炸冲击波相互作用数值模拟

根据试验模型和试验结果，进行了浅层水中沉底爆炸冲击波相互作用数值模拟；研究了水底水面对沉底爆炸冲击波传播与相互作用的影响。结果表明，水底对冲击波压力峰值有较大的削弱作用，水面使冲击作用冲量明显减少，冲击波相互作用的压力叠加或多次冲击作用大大提高了爆炸威力。     

Investigation on the Cause of Excessive Vibration of an Offshore Platform

0　IntroductionWiththeexploitureanddrillingforoceanre source,offshore platformsaremost prolificandprevalentintheoffshoreindustrytoday .Asthefun damentalinstallationsofdevelopmentofoceanre sources ,designingrequirementsofoffshoreplatformsarebecomingmoreandmoreimportant.Underenvironmentalloadsduetowind ,cur rent ,waveandevenseismicprotectionattack ,off shoreplatformsinevitablyvibrateduringtheirlife time .While ,foranormalconditionthisvibrationissmallandtheoccupantsontheplatformdon tsenseitatall.…     

Multisymplectic five-point scheme for the nonlinear wave equation

In this paper, we introduce the multisymplectic structure of the nonlinear wave equation, and prove that the classical five-point scheme for the equation is multisymplectic. Numerical simulations of this multisymplectic scheme on highly oscillatory waves of the nonlinear Klein-Gordon equation and the collisions between kink and anti-kink solitons of the sine-Gordon equation are also provided. The multisymplectic schemes do not need to discrete PDEs in the space first as the symplectic schemes do and preserve not only the geometric structure of the PDEs accurately, but also their first integrals approximately such as the energy, the momentum and so on. Thus the multisymplectic schemes have better numerical stability and long-time numerical behavior than the energy-conserving scheme and the symplectic scheme.