畸形波作用下张力腿浮式风力机动力响应特性

针对张力腿系泊浮式风力机的基础运动,忽略柔性构件的影响,建立气动—水动—系泊非线性耦合运动方程。在运动控制方程中包含张力腿系泊系统的非线性回复刚度,桨距角控制以及浮式基础运动对空气动力载荷的影响。在波浪载荷的计算中考虑二阶波浪载荷的作用。采用随机频率相位角调制法生成畸形波波面时历,计算在畸形波作用下张力腿型浮式风力机的动力响应特性。数值模拟结果表明,在畸形波作用下,浮式基础的运动及空气动力性能均受到了显著的影响。其中浮式基础的纵荡和纵摇运动分别受二阶差频与和频波浪力的影响,而垂荡运动的增加则主要是受下沉运动的影响。在畸形波经过的时刻,风力机的功率系数迅速下降,水平方向的风载荷波动先减小,随后其数值急剧下降,而垂直方向的风载荷波动增大。     

浅水浮式风机基础水动力特性及波浪荷载的CFD数值分析

采用计算流体动力学(CFD)方法对OC4-DeepCwind半潜式风机基础在30～100 m水深下的水动力特性和非线性波浪荷载进行了研究。基于验证的数值波浪水池,通过结构自由衰减运动及规则波下浮式基础的幅值响应算子(RAO)计算,分析了浮式风机基础的结构动力特性及水动力特性随水深的变化规律,研究了浅水条件下非线性波浪荷载特征。研究结果表明,随着水深的减小,风机基础结构垂荡固有周期略有增大,垂荡和纵摇的阻尼比均呈现逐渐增大的趋势;与黏性流理论计算结果相比,势流结果在浅水波浪工况下对垂荡和纵摇RAO存在显著低估;在浅水波浪作用下,风机基础所受波浪荷载的三倍波频成分占比可超过5%,体现了浅水条件下波浪与结构之间较强的非线性作用。     

一种新型Semi-Spar式海上风机平台系泊系统优化分析

参考英国的Kincardine风机采用的新式的Semi-Spar概念,结合spar式基础和半潜式基础的特点,提出了一种新式海上浮式风机平台模型,并基于三维势流理论,利用AQWA软件进行水动力计算,验证新式平台可靠性。分析了在风、浪、流荷载联合作用下,锚链竖向夹角、系缆数量对风机浮式平台运动性能和系泊张力的影响,对系泊系统进行优化,并验证极端工况下的可靠性。结果证明风机平台水平运动和纵摇运动幅值较小,但垂荡幅值略大,而通过减小锚链竖向夹角可以控制平台运动响应幅值,增加系缆数量可以同时减小系泊张力大小。计算结果证明了新型Semi-Spar式海上风机平台可行性,为浮式风机平台及系泊系统的设计提供参考。     

基于非线性数学模型的半潜式平台共振运动特性研究

共振运动是深海浮式平台设计的关键考虑因素之一,对海洋平台的作业具有重要影响。采用半潜式平台运动的非线性耦合数学模型,考虑浮筒和横撑出入水以及垂荡、横摇和纵摇运动耦合对平台浮力和恢复力的影响,研究半潜式平台非线性共振运动特性,以及不规则波浪参数对运动的影响。研究表明:在非线性耦合运动和浮力变化的影响下,半潜式平台纵摇和垂荡运动的固有周期会随运动幅值的增大而逐渐减小,且最终趋于稳定,对纵摇运动周期的影响更为显著;非线性效应会使半潜式平台产生显著的低频纵摇共振响应,以及共振频率漂移的现象,且受随机种子和波浪周期的影响较小。     

圆筒形FWPSO水动力性能模型试验研究

针对一圆筒形FWPSO设计概念开展水动力性能模型试验研究,研究发现圆筒形FWPSO纵摇运动受二阶波浪力作用明显,存在显著的低频运动;同时由于垂荡固有周期与波浪周期接近,该平台在大的波浪环境中出现较大幅度的垂荡运动而在小的波浪环境下纵摇和垂荡运动性能优良。该问题应当引起设计者足够的重视。     

10MW级海上浮式风机运动特性研究

以DTU 10 MW基准风机为研究对象,单柱式平台作为基础支撑结构,使用FAST软件计算分析,考虑单独风、单独波浪以及风浪组合三种环境条件,对10 MW级海上浮式风机的运动特性进行研究。研究发现:系统摇荡是风激励的低频运动和波浪激励的波频运动的合成,气动阻尼削弱系统的波频运动;系统纵荡和纵摇运动存在明显的耦合现象,而垂荡运动和其他方向的运动没有耦合关系;受纵摇影响,转动的风轮产生陀螺惯性力矩,激励首摇运动;随着风机单机容量的增加,风激励的低频运动比例增大,波浪激励的波频运动比例减小。     

波流组合作用下SPAR平台垂荡-纵摇耦合运动研究

探讨SPAR平台在波流组合作用下的运动响应机理。运用Matlab程序分析了SPAR平台产生内共振的运动过程,运用刚体动力学理论建立了平台垂荡-纵摇耦合方程,对波流共同作用下Spar平台的垂荡、纵摇运动进行数值模拟,结果表明:流的加入对于内共振的影响并不明显;同时采用AQWA软件研究了流的加入对于纵荡二阶慢漂力的影响,研究发现,当波流同向时能大大增加Spar平台的纵荡运动,而波流反向时却能明显削弱纵荡运动。本文研究成果对于指导深海浮式结构设计开发具有一定的理论借鉴作用。     

垂荡板对浮式风机水动—气动耦合性能影响研究

随着风电产业向深远海发展,浮式风机已经成为海上风机未来的发展趋势.由于复杂的风浪联合环境载荷作用,浮式风机作业时通常会产生大幅度的运动响应,这一方面会使得浮式风机系统受到的水动力载荷更加复杂,另一方面会影响浮式风机的输出功率.因此,如何有效地抑制浮式风机系统的运动响应就成为了设计的关键.基于非稳态致动线模型和两相流求解器naoeFOAM-SJTU,进行了带垂荡板的浮式风机耦合性能研究.首先在OC3-Hywind Spar平台上附加垂荡板,并结合NREL-5 MW风力机建立带垂荡板的浮式风机模型.其次对比不同形状的垂荡板对Spar-5 MW型浮式风机气动—水动耦合结果,分析相同风浪联合作用条件下垂荡板形状对浮式风机耦合响应的影响.研究结果表明:垂荡板能够减小纵荡和垂荡等运动响应幅值,但是对纵摇运动响应影响较小;当垂荡板直径和吃水位置相同时,相同风浪条件下圆形垂荡板能使浮式风机的气动平均功率增大约0.844％,而正方形垂荡板却使平均功率减小1.492％,这说明圆形垂荡板对浮式风机系统的作用效果整体而言优于正方形.     

新型全潜式浮式风机在不同风况下的动力响应分析

针对一种新型全潜式浮式风机,应用FAST软件建立风电机组-塔筒-浮式平台-系泊系统的时域耦合分析模型,研究其在不同风况下的动力响应。计算结果表明:风速对于该浮式风机的动力响应影响明显,浮式平台的纵荡、纵摇以及风机叶片根部弯矩与风机在不同风速下受到的推力相关,由于新型全潜式浮式风机垂荡方向刚度很大,风速变化对于其垂荡运动影响相对较小;各风况下,系泊缆始终处于张紧状态,新型全潜式浮式风机运动幅值较小,具有良好的运动性能。     

海上浮式风机气动性能数值模拟

采用计算流体动力学(CFD)方法,基于RANS方程和SST k-ω湍流模型,对OC3-Hywind Spar浮式平台支撑的NREL5 MW风机进行气动性能模拟。对固定式风机的数值模型做网格无关性验证,同时考虑垂直风切变的影响,并将数值结果与NREL设计数据进行对比以验证模型的有效性。在FLUENT软件中,设定嵌入式滑移网格和用户定义程序(UDF)来模拟风机叶轮随平台的周期运动,分别研究浮式平台的纵荡、纵摇和首摇运动对风机气动荷载的影响。数值结果表明平台的纵荡和纵摇运动对输出功率影响较大,且平台运动幅值越大周期越低,其气动荷载变化越剧烈。合理控制平台的运动幅值对提高浮式风机的发电性能和疲劳强度有很大作用。     

Bed load transport on the shoreface by currents and waves

Tide-driven bed load transport is an important portion of the net annual sediment transport rate in many shoreface and shelf environments. However, bed load transport under waves cannot be measured in the field and bed load transport by currents without waves is barely measurable, even in spring tidal conditions. There is, consequently, a strong lack of field data and validated models. The present field site was on the shoreface and inner shelf at 2 to 8.5 km offshore the central Dutch coast (far outside the surfzone), where tidal currents flow parallel to the coast. Bed load transports were carefully measured with a calibrated sampler in spring tidal conditions without waves at a water depth of 13–18 m with fine and medium sands. The near-bed flow was measured over nearly a year and used for integration to annual transport rates. An empirical bed load model was derived, which predicts bed load transports that are a factor of > 5 smaller than predicted by existing models. However, they agree with laboratory data of sand and gravel transport in currents near incipient motion. The damped transport rates may have been caused by cohesion of sediment or turbulence damping due to mud or biological activity. The annual bed load transport rate was calculated using a probability density function (pdf) derived from the near-bed current and orbital velocity data which represented the current and wave climate well when compared to 30 years of data from a nearby wave station. The effect of wave stirring was included in the transport calculations. The net bed load transport rate is a few m²/year. This is much less than predicted in an earlier model study, which is partly due to different bed load models but also due to the difference in velocity pdf. The annual transport rate is very sensitive to the probability of the largest current velocities.     

海洋中β-二甲基巯基丙酸内盐降解过程的研究进展

二甲基硫(DMS)是海水中一种最重要的、含量最丰富的还原态挥发性生源有机硫化物,前体β-二甲基巯基丙酸内盐(DMSP)的降解过程受各种因素影响。其中主要包括温度、DMSP的浓度、氧气、盐度、酸度、颗粒粒度、藻类生长期、季节变化、氧化压力、抑制剂等。它们均与DMSP降解速率呈一定的函数关系,并对DMSP的降解产物产生影响。藻类是DMSP的主要来源,因此着重讨论了温度、盐度、酸度等对不同浮游植物细胞内DMSP与DMS生物生产和转化过程的影响。结合海洋硫循环的研究现状和海洋化学发展的趋势,探究了用颗粒态DMSP与Chla的比率来量化碳和硫通量的方法及DMSP裂解酶活性的检验技术。大气中CO2压力持续增加导致的海洋酸化对藻类中DMSP降解过程的影响也是进一步研究的重点。     

Tracing dissolved organic matter cycling in the eastern boundary of the temperate North Atlantic using absorption and fluorescence spectroscopy

Apparent oxygen utilization (AOU), dissolved organic carbon (DOC), coloured dissolved organic matter (CDOM) absorption spectra, and CDOM fluorescence characteristic of aromatic amino acids (excitation/emission 280 nm/320 nm; F(280/320)) and marine-humic like substances (320 nm/410 nm; F(320/410)) were measured in full depth during a cruise in the temperate Eastern North Atlantic (ENA). An optimum multi-parameter (OMP) inverse method was run to calculate water mass proportion-weighted average (archetypal) concentrations of these chemical parameters for all water masses and samples. Archetypal concentrations retain the variability due to water mass mixing and basin scale mineralization from the water mass formation sites to the study area. Conversely, the difference between measured and archetypal concentrations, retain the variability due to dissimilarities in mineralization processes within the study area. Our analysis indicates that DOC supported 26±3% of the AOU in the dark temperate ENA and that basin scale processes occurring at and from the formation area of the water masses explained 63% of the total DOC variability. Our data also suggests that DOC remineralized at the basin scale was of lower molecular weight, and with a lower proportion of fluorescent aromatic amino acids than found within the study area. The relationship between the absorption coefficient at 254 nm (a_CDOM(254)) and AOU indicates that a_CDOM(254) was consumed during organic matter remineralization in the dark ocean, with 55% of the variability being explained by basin scale processes. The relationships of F(320/410) with AOU and DOC confirmed that marine humic-like substances are produced by microbial degradation processes, at a rate of 6.1±0.9×10⁻³ mg equivalents of QS mol AOU⁻¹. Our results also indicate that basin-scale remineralization processes account for 85% of the total variability of F(320/410), emphasizing that large scale processes control the formation of humic-like substance in the dark ENA.     

南海名浅考

根据历史文献分析,已知南海海名最早出现于周宣王（827BC--782BC在位）时的《江汉》诗中。秦汉之间214BC—111BC时著的《山海经·海内东经》篇,记述了现时广东省三水和广州以南地区当时为海,称南海。这可从《史记》和《汉书》的记述,以及现代珠江三角洲的考古学、第四纪地质学和河口演变的研究成果所证实。南海古时别名涨海,明清时期外国人称为大明海和大清海。清朝以来,外国人把它翻译成（或称作）英文“South China Sea”,而近代某些中国人再把这个英文名词直译成汉文“南中国海”,忽视“南海”固有的中文名称。民国和中华人民共和国政府先后出版的地图和其他正式出版物,皆只用“南海”名。     

Dissolved organic matter cycling in the confluence of the Atlantic and Indian oceans south of Africa

The boundary between the Atlantic and Indian sectors of the Southern Ocean is a key spot of the thermohaline circulation, where the following water masses mix up: Indian Central water (ICW), South Atlantic Central Water (SACW), Antarctic Intermediate Water (AAIW), Circumpolar Deep Water (CDW), North Atlantic Deep Water (NADW), Weddell Sea Deep Water (WSDW) and Antarctic Winter Water (WW). An optimum multiparameter analysis based on the distributions of potential temperature, salinity, NO (=O₂+9.3×NO₃) and silicate during the GoodHope 2004 (GH04) cruise allowed us to (i) define the realms of these water masses; (ii) obtain the water mass proportion weighted-average (archetypal) apparent oxygen utilization (AOU) and dissolved organic carbon (DOC) concentrations of each water mass; and (iii) estimate the contribution of DOC to the oxygen demand of the study area. WW represented only 5.2% of the water volume sampled during GH04, followed by WSDW with 10.8%, NADW with 12.7%, SACW with 15.3%, AAIW with 23.1% and CDW with 32.8%. The distributions of DOC and AOU were mainly explained by the mixing of archetypal concentrations of these variables, 75±5% and 65±3% respectively, which retained the variability due to the basin-scale mineralization from the formation area to the barycentre of each water mass along the GH04 line. DOC accounted for 26±2% and 12±5% of the oxygen demand of the meso- and bathypelagic ocean, respectively. Conversely, local mineralization processes, retained by the residuals of the archetypal concentrations of DOC and AOU, did not contribute to improve significantly the mixing model of DOC.     

基于MapInfo数据格式在GIS应用环境下等值线综合方法实现

等值线构建是G IS开发、数字地图绘制重要的研究内容之一。重点讨论了基于M apInfo数据格式在G IS应用环境下等值线综合方法的实现,首先根据高程采样点跟踪等高线通过点,再利用五点光滑法、正轴抛物线加权平均光滑法以及M apX提供的光滑方法对等值线通过点进行光滑处理,从而绘制出光滑度好、准确美观的等值线,同时发现M apX所提供的光滑方法可能利用的就是正轴抛物线加权平均光滑法。通过大量的数据验证了绘制的正确性。     

基于Maplnfo数据格式在GIS应用环境下等值线综合方法实现

等值线构建是GIS开发、数字地图绘制重要的研究内容之一。重点讨论了基于Maplnfo数据格式在GIS应用环境下等值线综合方法的实现，首先根据高程采样点跟踪等高线通过点，再利用五点光滑法、正轴抛物线加权平均光滑法以及MapX提供的光滑方法对等值线通过点进行光滑处理，从而绘制出光滑度好、准确美观的等值线，同时发现MapX所提供的光滑方法可能利用的就是正轴抛物线加权平均光滑法。通过大量的数据验证了绘制的正确性。     

莱州湾海域水体中有机氯农药和多氯联苯的浓度水平和分布特征

以固相萃取/气相色谱法测定了莱州湾海域水体中22种有机氯农药和多氯联苯类化合物的浓度水平和分布特征。结果表明,莱州湾海域表层水体中有机氯农药浓度范围为N.D.~32.7ng/L,底层水中的浓度范围为N.D.~11.7ng/L。在该海域水体中共检出有机氯农药3种,β-666是水体中主要的有机氯农药污染物。多氯联苯类在底层水样中检出2种,总浓度范围在4.5~27.7ng/L之间。该海域有机氯农药和多氯联苯的分布特征是近岸高,离岸低,由近岸向湾外延伸方向依次递减。并对莱州湾表层水中总有机氯农药与海水盐度、氯度、溶解氧和pH间的关系作了初步探讨,得出总有机氯农药与盐度、氯度间有一定的相关关系,相关系数均为0.59。方法测定5种有机氯农药化合物的空白加标回收率为97.3%~126.0%,相对标准偏差为2.8%~8.6%;测定5种多氯联苯类化合物的空白加标回收率为88.6%~151.8%,相对标准偏差为6.7%~10.4%。     

Factors determining the vertical profile of dimethylsulfide in the Sargasso Sea during summer

The major source of reduced sulfur in the remote marine atmosphere is the biogenic compound dimethylsulfide (DMS), which is ubiquitous in the world's oceans and released through food web interactions. Relevant fluxes and concentrations of DMS, its phytoplankton-produced precursor, dimethylsulfoniopropionate (DMSP) and related parameters were measured during an intensive Lagrangian field study in two mesoscale eddies in the Sargasso Sea during July–August 2004, a period characterized by high mixed-layer DMS and low chlorophyll—the so-called ‘DMS summer paradox’. We used a 1-D vertically variable DMS production model forced with output from a 1-D vertical mixing model to evaluate the extent to which the simulated vertical structure in DMS and DMSP was consistent with changes expected from field-determined rate measurements of individual processes, such as photolysis, microbial DMS and dissolved DMSP turnover, and air–sea gas exchange. Model numerical experiments and related parametric sensitivity analyses suggested that the vertical structure of the DMS profile in the upper 60 m was determined mainly by the interplay of the two depth-variable processes—vertical mixing and photolysis—and less by biological consumption of DMS. A key finding from the model calibration was the need to increase the DMS(P) algal exudation rate constant, which includes the effects of cell rupture due to grazing and cell lysis, to significantly higher values than previously used in other regions. This was consistent with the small algal cell size and therefore high surface area-to-volume ratio of the dominant DMSP-producing group—the picoeukaryotes.     

网格虚拟地理环境体系结构研究

通过将网格技术与虚拟地理环境结合,以服务为核心,构造虚拟数据库,形成网格虚拟地理环境(G ridV irtual Geograph ic Environm ent,G rid-VGE),实现异构数据的集成与共享、任务的分解、闲散资源的充分利用、扩充虚拟地理环境的服务等。在详细阐述了G rid-VGE的框架结构及其关键技术的探讨后,以三维可视化地形漫游为例展示G rid-VGE中的一个应用实例。