半约束模型试验--一种验证随浪和斜浪中波浪力计算的手段

本文采用半约束模型试验技术，对一条高速船在规则波中随浪和斜浪工况进行了流体动力系列试验，以探讨航运的安全性，验证作用于船体上波浪力的估算方法。对每次试验，以波动方程的形式采用数值估算方法确定环绕船模的波浪运动的时间历程。并用同样的方法从测量数据中提取垂荡和纵摇与模型测量运动，一阶波导纵荡、横荡作用力和首摇力矩。因此合理比较理论计算的波浪力与力矩的时间历程成为可能。这表明SSPA海事动力学的研究所(MDL)模型试验设施可以提供高质量的测量，与所述计算方法结合起来可用来验证理论计算和建立半经验方法。     

减振降噪技术的应用设计

本文针对某型号测量船主要噪声振动源采取相应技术措施进行减振降噪综合治理研究，其中主机采用低频大载荷隔振器的单层隔振、辅机采用浮筏隔振装置、机座采用局部阻尼处理等措施。由于该船采用了先进的浮筏技术及其他隔振措施，在提高船上测量系统读取数值精度的同时，大大改善了船上水声设备测绘工作环境和船员的生活环境，提高了该船的设备使用寿命和船员体力极限。本船自噪声在低航速时已淹没在海洋背景噪声之中。特别是该船减振降噪装置在系统的声学匹配设计方面取得了进展，经实船验证，效果良好，证明该设计方法可行，对减振降噪技术在各型舰船上的工程应用开发研究有一定借鉴作用。     

水深平均k—ε紊流模型在大尺度水域中的应用研究

本文利用Patanker求解紊动输运方程标准的SIMPLEC计算程式,对小尺度丁坝绕流进行了模拟计算,取得了与水槽试验一致的流速分布结果。为了探讨大尺度水域紊动量K、ε壁面边界条件的给定,本文将水槽看成是一种比尺模型,将水槽试验流速分布按重力相似和阻力相似准则延伸到大尺度水域,并以此研究k—ε模型模拟大尺度回流的置信水平。计算结果表明通过选择合适的紊动量壁面边界条件,该模型对大尺度回流计算也能取得较好的结果。     

整治建筑物壅水及重力相似偏离影响的初步研究

简述整治建筑物的壅水及其机理,归纳出局部水头损失壅水的通用公式。将丁坝工程壅水区分为床面摩阻损失增大壅水和局部水头损失壅水2部分。在ΔFr>0的模型中,采用换算式ΔZp=ΔZm.hλ,定性地说是偏大的。可采用换算式Δhfp=Δhfmhλ。而丁、潜坝局部水头损失的壅水,则应采用hjp=Δhjmλu02。     

应用巴列特统计方法降低工程成本的实践

文章简述了巴列特（Pareto）统计分配法的基本要点，并结合天津港南疆工作船码头工程的施工实例，应用巴列特法进行了分析，明确了该工程中节省成本的重点项目、内容及节省成本的贡献率，从而有针对性地制定了相应的成本控制和节约措施，经过实践，收到了较好的效果。     

Statistical Approaches to Mapping QTL of Dynamic Traits

Dynamic traits are those that change with timein the development process of life or other quanti-tative factor (e. g. environmental condition).These traits also are called infinite-dimensionalcharacters by Kirkpatrick and Heckman[1]andfunction-valued traits by Pletcher and Geyer[2], be-cause they can be expressed as a function of someindependent and continuous variables. Dynamictraits are collected at many time points during thecourse of life. Therefore, studies of dynamic traitsare regarded…     

Fluxes of dissolved inorganic carbon in three estuarine systems of the Cantabrian Sea (north of Spain)

The diffusive and in situ fluxes of dissolved inorganic carbon (DIC) and total alkalinity (TA) have been measured and an estimation has been made of the water–atmosphere fluxes of CO₂ in three estuarine systems of the Cantabrian Sea during the spring of 1998. Each of these systems undergoes a different anthropogenic influence. The diffusive fluxes of dissolved inorganic carbon and total alkalinity obtained present values ranging between 0.54–2.65 and 0.0–2.4 mmol m⁻² day⁻¹, respectively. These ranges are in agreement with those of other coastal systems. The in situ fluxes are high and extremely variable (35–284 mmol TA m⁻² day⁻¹, 43–554 mmol DIC m⁻² day⁻¹ and 22–261 mmol dissolved oxygen (DO) m⁻² day⁻¹), because the systems studied are very heterogeneous. The values of the ratio of the in situ fluxes of TA and DIC show on average that the rate of dissolution of CaCO₃ is 0.37 times that of organic carbon oxidation. Equally, the interval of variation of the relationship between the benthic fluxes of inorganic carbon and oxygen (F_DIC/F_DO) is very wide (0.3–13.9), which demonstrates the different contributions made by the processes of aerobic and anaerobic degradation of the organic matter, as well as by the dissolution–precipitation of CaCO₃. The water–atmosphere fluxes of CO₂ present a clear dependence on the salinity. The brackish water of these systems (salinity<20), where maximum fluxes of 989 mmol m⁻² day⁻¹ have been estimated, act as a source of CO₂ to the atmosphere. The more saline zones of the estuary (salinity>30) act as a sink of CO₂, with fluxes between −5 and −10 mmol m⁻² day⁻¹.     

江淮气旋大风预报研究

江淮气旋大风预报研究的结果表明：气旋大风的预报实际上就是冷空气南下造成地面加压与气旋东移造成地面降压，这两个因素所造成气压梯度发展变化地以预报。还介绍用天气学原理建立的大风预报模式，以及用数理统计方法判别有无强风的预报，经过历史拟合和试报，在预报气旋大风中有一定的准确性。     

舰船模块化设计中信息集成化的数据信息模型研究

介绍了产品集成信息模型的基本框架和用STEP标准建立构件模型和装配模型的方法，并以球面隔壁为对象给出构件模型和装配模型的实例。