Measurement of Marine Picoplankton Cell Size by Using a Cooled, Charge-Coupled Device Camer

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基于单目视觉的无人水面艇水面目标测距方法

基于单目视觉的无人水面艇水面目标测距方法

2021年第40卷第2期传感器与微系统(Transducer and Microsystem Technologies)47DOI : 10.13873/J. 1000-9787(2021)02-0047-04基于单目视觉的无人水面艇水面目标测距方法**收稿日期:2019-08-13*基金项目:国家自然科学基金面上资助项目(61771223)赵明绘,王建华,郑翔,张山甲,张程(上海海事大学航运技术与控制工程交通行业重点实验室,上海201306)摘要:针对单目测距时相机高度和俯仰角难以测量的问题,提出一种相机高度和俯仰角的标定方法,在 此基础上提出一种水面目标的单目测距方法,并分析影响测距精度的因素。

通过相机标定,获得与水面共 面的标定板上的网格坐标系到相机坐标系的外参,计算相机高度和俯仰角;识别出图像中水面目标所在区 域,计算该区域像素纵坐标最大值,及其对应的横坐标的平均值,将组合得到的坐标作为观测点的像素坐 标;根据相机内参、透视投影关系和刚体变换,获得观测点在无人艇附体坐标系下的三维信息,进而计算观 测点的距离。

通过实验验证了所提方法的正确性和有效性。

关键词:单目视觉;无人水面艇;相机高度;相机俯仰角;观测点;测距中图分类号:TP212.9 文献标识码:A 文章编号:1000-9787(2021)02-0047-04Monocular vision based water-surface target distance measurement method for unmanned surface vehiclesZHAO Minghui , WANG Jianhua, ZHENG Xiang, ZHANG Shanjia, ZHANG Cheng(Marine Technology & Control Engineering Key Laboratory ,Shanghai Maritime University ,Shanghai 201306,China)Abstract : Aiming at lhe problem that lhe height and pilch angle are difficult to measure during monocular ranging , a method for calibrating camera height and pitch angle is proposed , and a water-surface target ranging method based on monocular vision is proposed , and lhe factors affecting lhe ranging precision are analyzed ・ Through camera calibration , obtain the extemal coordinate of the grid coordinate system on the calibration plate that is coplanar with the waler surface to lhe camera coordinate system , calculate the camera height and the pilch angle. The area of the target on water surface in the image is identified , the maximum value of the ordinate of the pixel in the area ,and lhe average value of the corresponding horizontal coordinate are calculated ,and the combined coordinate is taken as the pixel coordinate of the observation point. According to the camera internal reference , perspective projection relationship and rigid body transformation , the three-dimensional information of the observation point in the coordinate system of the unmanned boat is obtained , and then the distance of the observation point is calculated. The correctness and effectiveness of the proposed method are verified by experiments ・Keywords : monocular vision ; unmanned surface vehicle ; camera height ; camera pitch angle ; observation point ; ranging0引言无人水面艇由于其可以执行更危险的以及不适于有人 船只执行的任务而吸引了广大研究人员⑴。

无人船在水下地形测量中的应用

无人船在水下地形测量中的应用

科技创新与应用Technology Innovation and Application应用科技2021年15期无人船在水下地形测量中的应用秦亮亮(91550部队,辽宁大连116023)我国幅员辽阔、山川河流众多,仅流域面积就已经超过1000km2,随着国家对水下地形地貌调查进程的加快,对于湖泊乃至近海水域的水下地形测量调查工作要求也在不断提升。

长期以来,我国的水下地形测量工作停留在人工测量阶段,有关水下地形测量的技术手段较为落后,因此开展无人船水下地形测量优势极为明显。

近几年来,为了获得水下地形信息数据,无人船测量系统通过搭载GNSS-RTK设备、单波束测深仪等数据采集设备进行水下地形数据测量,可有效满足传统测量模式中人工测量技术无法达到的工程任务要求,可有效解决传统测量模式中所受到的地形环境因素制约,让水下地形测量人员获得高精度的数据信息,为水下3D模型的建立奠定坚实基础。

1无人船1.1无人船应用特点无人船作为进行水下地形测量数据获取的重要路径,现阶段已代替了大部分的传统人工测量作业方式。

自我国应用无人船技术以来,经由多年的技术创新发展,无人船的水下地形测量技术已趋近于成熟,而无人船的水下航行表现也趋于稳定。

现阶段的无人船发展方向为智能化。

在水下地形测量中无人船技术应用的最大优势就是高效、安全、轻便及小巧,再加上无人船测量运行成本低的应用优势,让无人船测量技术深受测绘单位的喜爱。

无人船测量技术的远程遥控系统,以及自动驾驶系统完摘要:在我国基础建设工作逐步开展的前提下,海洋战略发展步伐逐步加快。

近年来我国对近海滩涂、海底地形测绘调查及陆地水下地形测绘、监测工作的测量要求精准性,以及时效性逐步提升,确保水下地形测量的精准性是加快水利工程建设速度的重要路径。

水上测绘领域的环境条件较为艰苦,比陆地测量工作艰难很多。

水上测绘工作的开展不仅充满各种困难与艰辛,同时测绘人员需要面临测绘安全问题。

传统技术下的水下测量工作都是借助人工操作船只进行地形定位及地形测量,因此传统水下测量结果的精确度和测量人员的安全性相对较低。

基于Neumann谱和PM谱的海浪感应磁场能量分布计算

基于Neumann谱和PM谱的海浪感应磁场能量分布计算

基于OpenSceneGraph 的海洋环境三维可视化系统研究李新放, 刘海行, 周林, 贾贞, 宋转玲(国家海洋局第一海洋研究所, 山东青岛266061)摘要: 为了研究虚拟现实技术在海洋环境三维可视化中的应用, 对大气、海底地形、风浪流等数据产品进行了分析整理, 运用场景裁剪、level of details(LOD)细节层次、场景动态调度等关键技术方法, 结合VisualPlanetBuilder (VPB)、ARCGIS 多种数据处理工具, 在VC++和OSG2.8.7 的可视化开发环境上,构建了一个三维、动态、实时、可交互的海洋环境可视化模拟仿真系统。

这个系统可以为海洋科学研究和工程建设提供一个更加便捷、直观的可视化平台。

关键词: 虚拟现实; 海洋环境; 可视化中图分类号: P76 文献标识码: A 文章编号: 1000-3096(2012)01-0054-05在全球陆地资源日益紧张和环境不断恶化的今天, 世界各国纷纷将目光转向海洋, 开发海洋资源,发展海洋经济成为沿海国家国民经济的重要支柱,伴随着在海洋开发过程中人们日益多样化的海量信息需求, 原有的二维纸质海图、电子海图提供的海洋环境信息已经日渐不能满足实际生产研究的需要。

快速、高效的数据模型, 流畅、逼真的三维场景渲染方式, 日益成为海洋环境信息表达的一种趋势。

在海洋环境的三维可视化研究中, 海洋因其环境的复杂性和数据的难以获取, 较之陆地更加难以模拟。

目前, 国外在海洋环境三维可视化的研究和应用方面较为成熟, Flavio 等[1]对实时三维地形可视化中数据分析应用进行了研究, Wynne 等[2]对分等级不规则三角网的三维高程表示进行了研究, Kofler 等[3]对地形模型的大场景贴图进行了研究。

经过长期应用和推广, 形成了一系列可视化商业软件, 如Google Earth 、Skyline、Cadsoft 的Env is ioneer 和MaK Technologies 的Army Command 2010 等软件。

舰船内腐蚀海水管路剩余强度预测模型及试验验证

舰船内腐蚀海水管路剩余强度预测模型及试验验证

舰船内腐蚀海水管路剩余强度预测模型及试验验证潘兴隆1,张鲁君2,贺国1,张攀1(1.海军工程大学动力工程学院,武汉430033;2.91878部队,广东湛江524300)摘要:舰船海水管路内壁长期受海水侵蚀产生腐蚀缺陷,降低了管路结构强度。

腐蚀后的海水管路强度不足,在管路内压力作用下易发生破裂导致舰船安全事故。

本文在对比现有腐蚀工业油气管道剩余强度评价方法的基础上,基于DNV-RP-F101标准,建立了内腐蚀薄壁海水管路剩余强度预测模型,并进行了静水压爆破试验以验证模型的准确性。

试验表明,本文提出的内腐蚀薄壁海水管路剩余强度预测模型可用于评价不同材质的舰船薄壁海水管路受腐蚀后的剩余强度,且预测的剩余强度准确度较高,对管路合理维修具有指导意义。

关键词:舰船海水管路;内腐蚀;剩余强度;预测模型;静水压爆破试验中图分类号:TB37文献标识码:A doi:10.3969/j.issn.1007-7294.2021.02.008Prediction model for residual strength of warship seawater pipelines with internal corrosion and test verificationPAN Xing-long 1,ZHANG Lu-jun 2,HE Guo 1,ZHANG Pan 1(1.College of Power Engineering,Naval University of Engineering,Wuhan 430033,China;2.Unit 91878of PLA,Zhanjiang 524300,China)Abstract:The structural strength of marine pipelines of naval ships will be reduced after having been eroded by sea water for a long time.Because of the corrosion defects and structural strength decrease,the corroded seawater pipelines will break down under internal pressure and cause ship safety accidents.On the basis of comparison of existing residual strength evaluation methods for corroded oil and gas pipelines with DNV-RP-F101standard,the residual strength prediction model of corroded thin-walled seawater pipelines is estab⁃lished,the accuracy of which is verified by hydraulic blasting test.Experiment results show that the effective pressure prediction model proposed in this paper can be used to evaluate the residual strength of corroded thin-walled seawater pipelines of different materials,and that the prediction accuracy of failure pressure ishigh,which provides recommendations to reasonable maintenance of pipelines.Key words:warship seawater pipelines;internal corrosion;residual strength;prediction model;hydraulic bursting test 0引言舰船海水管路内壁与海水直接接触,长期经受海水的侵蚀,管道内壁会形成体积型腐蚀缺陷。

海洋低频电场传感器敏感电极材料的选择

海洋低频电场传感器敏感电极材料的选择

海洋低频电场传感器敏感电极材料的选择宋玉苏*张燕张坤左攀(海军工程大学理学院caosys@武汉430033)摘要:选择了九种不同的电极材料,根据海洋环境下低频、极低频电场的自身特点,通过直流电阻、交流阻抗、电极对极差漂移三个方面对电极性能进行了测试,研究了其用于海洋环境低频电场弱信号探测的可行性,筛选出了适合海洋环境低频电场测量的电极材料,并从理论上进行了解释。

结果表明,固态Ag/AgCl电极的直流电阻和交流阻抗均较小,且其极差漂移可控制在μV级,具有优良的极化效应和较低的极差漂移,是海洋环境低频电场探测的敏感电极材料。

关键词:海洋;低频电场;电极;材料中图分类号:TG174.42文献标志码:A海洋环境决定了电场信号必需经过液相介质到固相介质的传递过程,而每种电极材料都有着其固有的特性,其所表现出的材料电化学特性决定着探测结果的精确与否。

因此,寻找一种在海水环境下与海洋低频电场信号特征相匹配的敏感电极材料是电场探测的关键。

国内外对于这方面的研究仅在文献中有零星提及[1],并未进行系统的研究,因此探寻海洋环境低频电场敏感材料可为开发高灵敏度的海洋低频电场传感器提供材料储备。

海洋低频电场是静电场和交变电场及其谐波的叠加[2-4],场强较弱,且交变电场以低频和极低频为主。

电极在探测海洋低频电场时会受到直流信号及较低频带交流信号的扰动,并产生相应的直流电阻和交流阻抗。

有研究表明[5],电极与海水的接触阻抗小而均匀稳定,可以提高测量精度。

另外,电极的极差漂移是海洋低频电场探测的重要指标,为了达到准确探测海洋弱信号的目的,应选择极差漂移小的电极类型。

因此,本文从电极直流电阻,交流阻抗和电极对极差漂移三个方面对不同材料电极进行了研究。

1实验材料与方法1.1 电极材料类型铜电极、锌电极、镍电极、钛电极、铝电极、铂电极、石墨电极、饱和甘汞电极(SCE)、Ag/AgCl 电极。

这些电极在海洋环境中分别得到应用,电极电位稳定性满足一般海洋使用要求。

舰艇螺旋桨水下噪声预测

舰艇螺旋桨水下噪声预测

舰艇螺旋桨水下噪声预测杨琼方;王永生;张明敏【摘要】Cavitation noise of marine propellers is an important component of the ship's radiating underwater sound. Given the flat-slope characteristic of the source spectrum level of propeller noise, the spectrum decay index is presented,and the dependent parameters of the peak frequency and its spectral peak are analyzed at the same time.The cavitation noise spectrum formulations within part frequency band for the two special speed under propeller cavitation condition can be used to construct ship's propeller cavitation noise spectra at any speed by linear regression. Uniting the function of spectrum level at the given frequency versus propeller diameter under a given tip circumferential velocity condition and the increment of the spectrum level at the given frequency due to the change of tip circumferential velocity at some frequency,the spectrum level at the given frequency under non-cavitation can be derived for submarine,while the sound level increment on account of spectral level getting into the sharp spectral peak regime and the additional increase of rotating speed above the critical valve should be added under the cavitation condition,in which case the submarine propeller noise spectrum can be predicted at any speed within the whole band. Finally, the derived equations are validated by the exist data and the error is less than 4dB. The tip cavitation inception index used during the prediction and the existence of narrow band tonal noise should be determined by the cavitation tunnelexperiment.%螺旋桨空化噪声是舰艇最主要的辐射噪声源.文章分析了螺旋桨噪声平坡形谱曲线的特点,给出源声级谱级曲线的衰减指数值,分析了特征频率和峰值谱级的影响因素.由螺旋桨空化状态下两个特征航速对应的部分频段内的噪声谱级计算式拟合得到水面舰船螺旋桨空化后任意可达航速下的噪声谱曲线.结合叶梢周向速度一定时特征频率处谱级与螺旋桨直径的函数关系和频率一定时叶梢周向速度变化引起的特征频率处谱级变化量,得到潜艇螺旋桨无空化状态下特征频率处谱级,在空化状态下,还需要加上螺旋桨进入尖锐谱峰区和转速进一步升高引起的声级增加量,从而得到了潜艇在任意航态下整个频带内螺旋桨噪声谱级的计算式.利用已有数据对计算式进行了检验,计算声级误差小于4dB.计算中用到的叶梢初生空泡数和判定是否出现窄带调噪声要通过空泡筒试验确定.【期刊名称】《船舶力学》【年(卷),期】2011(015)004【总页数】8页(P435-442)【关键词】舰艇;螺旋桨;空化噪声;平坡形谱曲线;窄带调噪声【作者】杨琼方;王永生;张明敏【作者单位】海军工程大学,船舶与动力学院,武汉,430033;海军工程大学,船舶与动力学院,武汉,430033;海军工程大学,水声研究所,武汉,430033【正文语种】中文【中图分类】U664.33;O427.51 引言无论是水面舰艇还是潜艇,声隐身性能都是衡量其战斗力的重要指标。

海水沉积物中总汞甲基汞测定

海水沉积物中总汞甲基汞测定

BaselineTotal,methyl and organic mercury in sediments of the Southern BalticSeaJ.Bełdowski a ,M.Miotk a ,M.Bełdowska b ,J.Pempkowiak a ,⇑a Institute of Oceanology,Polish Academy of Sciences,P.O.Box 197,Sopot,Poland bInstitute of Oceanography,Gdansk University,Al.Pilsudskiego 46,Gdynia,Polanda r t i c l e i n f o Article history:Available online 31July 2014Keywords:Patchiness SpeciationOrganic mercury Extractiona b s t r a c tDistribution of sedimentary mercury in the Southern Baltic was investigated.Sediment samples were collected from the Southern Baltic in the period from 2009to 2011,and concentrations of sedimentary total mercury (average 102ng/g,range 5.8–225ng/g)and methyl mercury (average 261pg/g,range 61–940pg/g)were measured in the manner that the influence of both patchiness and seasonal changes were assessed.Moreover,sedimentary mercury extracted with organic solvent-the so-called organic mercury was also analyzed (average 425pg/g,range 100–1440pg/g).There is a statistically significant dependence between organic mercury and both methyl mercury and total mercury concentrations in the sediments.Methyl mercury contribution to total mercury varied from 0.12%to 1.05%,while organic mercury contributed to 2%of total concentration on average.The area studied,although mercury concentrations exceed threefold the geochemical background,can be regarded as moderately contaminated with mercury,and methylmercury.Ó2014Elsevier Ltd.All rights reserved.Mercury has been a subject of environmental chemistry interest for several decades (Pacyna et al.,2006).Although all chemical forms of mercury are toxic,public health concerns are focused on methylmercury (MeHg).Nowadays loads of mercury discharged to the environment from anthropogenic sources exceed several times these from natu-ral ones (Pacyna et al.,2006).Much of the mercury originating from both anthropogenic and natural sources is,eventually,brought to the marine environment.There,owing to its affinity to particulate matter,mercury is readily scavenged from the water column (Laurier et al.,2003)and deposited to bottom sediments (Cossa and Gobeil,2000)in particular in estuaries and coastal areas (Boening,2000).Distribution of mercury in marine sediments is influenced by physical transport,sediment texture,mineralogical composition,reduction/oxidation status of sediments,adsorption and desorp-tion processes and organic matter content (Boening,2000;French et al.,1999).Red-ox conditions are of particular interest as,in the reducing environment,mercury is readily transferred into organo-mercurial species (e.g.methylmercury-MeHg)that are both mobile and highly bioavailable.Thus,under specific condi-tions a fraction of mercury deposited to sediments re-enters the overlying water and constitutes threat to living organisms.As a result,sediments can act as both sink and source for mercury in aquatic environment (Zoumis et al.,2001).The Baltic Sea is a land locked basin surrounded by highly industrialized catchment area.Mercury concentrations in the sur-face Baltic sediments exceed the geochemical background by a fac-tor of three to five (Beldowski and Pempkowiak,2009).According to the recent pollution load compilation (HELCOM,2011)the input of mercury to the Baltic Sea had efficiently decreased within the previous two decades.Despite this,no corresponding decrease is observed in biota mercury concentrations (Saniewska et al.,2014).One of possible reasons is the re-emission of the previously accumulated mercury from sediments,in particular within sedi-mentation basins,due to anoxic conditions prevailing there (Bełdowski et al.,2009).Mercury in the Baltic sediments has been a subject of investiga-tions for several decades (Saniewska et al.,2010;Beldowski and Pempkowiak,2009;Bełdowski and Pempkowiak,2007;Borg and Jonsson,1996;Kannan and Falandysz,1998;Pempkowiak,1991;Pempkowiak et al.,1998).Concentration of the metal is well char-acterized (Bełdowski and Pempkowiak,2007;Borg and Jonsson,1996),as is the mechanism of mercury transport to the deposi-tional basins of the sea (Bełdowski and Pempkowiak,2007).How-ever,MeHg in the Baltic sediments have been seldom studied.So far just one report indicated the presence of MeHg in the Baltic/10.1016/j.marpolbul.2014.07.0010025-326X/Ó2014Elsevier Ltd.All rights reserved.⇑Corresponding author.E-mail address:pempa@iopan.gda.pl (J.Pempkowiak).Sediments(Kannan and Falandysz,1998).The authors of the report measured substantial contribution of MeHg to total mercury bas-ing on several results of methyl mercury in the Baltic sediments. Thus little is known regarding both contemporary concentrations of MeHg in the sediments and factors affecting the concentrations. This,at least partly,may be caused by relatively extensive analyt-ical procedure required to quantify sedimentary MeHg(Liang et al., 1994).Recently the so called organic mercury was suggested as a mercury fraction closely related to MeHg in fresh-water sediments (Boszke and Kowalski,2008).The authors used methylene chloride to separate organic mercury from sediments.Other organic sol-vents were also used for the purpose:toluene(Miller et al., 1995),and chloroform(Eguchi and Tomiyasu,2002;Tomiyasu et al.,2000).There are no reports regarding the usefulness of organic mercury as a substitute for MeHg in studies of marine sed-iments contamination.The aim of this study was to investigate concentrations of total mercury,and selected mercury fractions:total organic mercury and methylmercury in sediments of the Southern Baltic Sea and to compare the results with concentrations measured in other marine coastal areas.As sampling stations characterized by vary-ing red-ox conditions,sediment texture and organic matter con-tent were collected in close proximity to one another,factors affecting sedimentary mercury concentration and speciation were assessed too,as were relations between the measured mercury fractions.The Baltic Sea is a semi-enclosed water body surrounded by highly industrialized countries.Two main features characterize hydrology of the sea.Firstly,the surface water is brackish as a result of a large riverine input and the limited exchange of water with the North Sea.Secondly,there is a permanent halocline at a depth of about70m.The sub-halocline waters in the central basins are depleted of dissolved oxygen or even anoxic.Geochemical cycles in the Baltic have been strongly influenced by human activ-ities since the beginning of the20th century(Borg and Jonsson, 1996;Pempkowiak,1991).Much of the anthropogenic load is car-ried to the Baltic Sea with the river runoff.Subsurface groundwater discharge plays substantial role in case of nutrients and organic matter,and a minor role in the case of mercury(Szymczycha et al.,2013).The major rivers entering the Baltic can be divided into two broad categories:those separated from the sea by a lagoon,and those entering the sea directly.The lagoons act as traps for suspended and dissolved riverine loads(Borg and Jonsson, 1996;Pempkowiak et al.,2000).Samples for this study have been collected from the Southern and central Baltic.This area is,on average,quite shallow–mean depth being50m(Voipo,1981). Southern and central Baltic consists of series of deep basins sepa-rated by sills.Sedimentation regime in deep basins(>80m)may be considered as stable(Zaborska et al.,2014).In the intermediate areas(>50m)accumulation type of bed prevails,whereas in shal-lower regions erosion or no-accumulation bottoms predominate (Feistel et al.,2008;Voipo,1981).Sediments consist of silt and mud in the Gdan´sk Deep,the Bornholm Deep and the Gotland Deep-clay in the Słupsk Channel,and sand with occasional silt deposits in the Bay of Gdan´sk,the Słupsk Sill and the Pomeranian Bay(Feistel et al.,2008).For this study,three sedimentation basins of the Southern Baltic were sampled–Bornholm,Gdan´sk and Got-land Deeps,and two shallow areas adjacent to river mouths–the Gdan´sk Bay,close to the Vistula mouth and the Pomeranian Bay, close to the Odra mouth during cruise on the R/V Oceania in Spring 2009and2010from the Gdansk Deep,the Gotland Deep,the Pom-eranian Bay and the Gdan´sk Bay and in Autumn2009from the Gdan´sk Deep and the Gotland Deep.Location of the sampling sta-tions is shown in Fig.1.Samples were collected with a gravity corer.The top three cen-timeters of stratified sediments were sampled by cutting it away with a plastic spatula,mixed,transferred into polyethylene bags and stored frozen(À20°C)until analyses in laboratory.Before mercury analysis all the samples were homogenized under laminarflow hood and aliquots were taken for determina-tions of moisture,organic carbon andfine grain fraction contents. Moisture was used to calculate dry mass of sample,and all results are reported as mass per dry weight.Fine grained fraction (<0.067mm)content was determined by anic carbon content in sediments was determined after removal of carbonates (2M HCl)using an Elemental Analyzer Flash EA1112Series com-bined with the Isotopic Ratio Mass Spectrometer IRMS Delta V Advantage(Thermo Electron Corp.,Germany)and presented as percentage in the bulk of the dry sample.Quality control was car-ried out with standard materials supplied by the Thermo Electron Corp.The methodology used proved satisfactory accuracy and pre-cision(average recovery99.1±2.0%).Total mercury determination was performed via sample (500mg)pyrolysis in a stream of oxygen(Leco AMA254,Czech Republic).The AMA254technique of direct combustion features a combustion/catalyst tube where sediment decomposes in an oxygen-rich environment and removes interfering elements.Both recovery and precision given as Relative Standard Deviation proved satisfactory(97%±3%RSD)basing on a reference material analysis (NIST2584).Extractable fraction of mercury(organic mercury)was deter-mined according to procedure described for river sediments (Boszke et al.,2007).In short,a sediment sample(5.0g)was twice extracted with chloroform,reextracted by aqueous sodium thio-sulphate solution(0.01M;10mL)From the aqueous layer an ali-quot of5mL was collected,placed in a measuringflask(50mL) and treated with20l L65%HNO3,7.5mL33%HCl and5mL of a 1:1solution of0.0033M KBrO3and0.2M KBr to oxidize all mer-cury species to Hg(II).Resulting solutions were analyzed by means of atomicfluorescence spectrophotometry on automated Tekran 2600(Canada)apparatus,according to EPA1631method(EPA, 2002).Methylmercury has been determined in the Josef Stefan Insti-tute laboratories in Ljubljana(Slovenia),using the procedure developed by Liang et al.(1994)and used successfully by others (Logar et al.,2002;Quevauviller et al.,1998).Methylmercury defined by this procedure includes all monomethyl mercury spe-cies found in sediments(e.g.CH3Hg+,CH3HgCl,CH3HgOH,and CH3-HgS-R),which are amenable to complexation and extraction as CH3HgBr.In short,300mg sample of wet sediment was sequen-tially eluted with2.5ml of1.5M HBr solution and1ml of1M CuSO4.Then MeHg was extracted into methylene chloride.20ml of deionized water were added,and the organic fraction was evap-orated after dilution to a known volume with reagent water,fur-ther analysis was carried out by aqueous phase ethylation,and then analyzed using the GC/pyrolysis/CVAFS technique in a Brooks and Rand Model1Detector equipped with a gas chromatography column and a high temperature(300°C)desorption unit.All sam-ples were analyzed in triplicate,and blank samples were run for every six samples.Recovery and precision of measurements were assessed by the use of certified reference material(NIST2584for total mercury and BCR580for organic/methyl mercury).Those were equal to98%and3%RSD,for total mercury,while for HgOrg and MeHg RSDs did not exceed7.4%while recovery equaled91%.The common problem with mercury analysis in marine sedi-ments is the random component,associated with the so called ‘‘patchiness’’–mosaic properties of sediments,which vary,even on a very local scale.The Baltic sediments were reported to be characterized with substantial patchiness(Zaborska et al.,2014; Zalewska and Suplinska,2013;Winterhalter,2001),which may cause the measured concentration of mercury to be non-represen-tative for a given area,if it is based on a single sample analyses.J.Bełdowski et al./Marine Pollution Bulletin87(2014)388–395389Therefore in this study,cores were collected in triplicate,within a one square km area.Moreover in order to assess possible seasonal variability,samples were collected in three seasons(Spring2009, Autumn2009and Spring2010)in the area of Gdan´sk and Gotland Deeps,and in two seasons in the remaining stations(Bornholm Deep,Pomeranian Bay and Gdan´sk Bay).Results of the so designed exercise are presented in Fig.2,sep-arately for each station,error bars represent seasonal differences.Since variability in stations close to shore,especially near the Vistula mouth(V)is visibly greater than in the accumulation basins,near shore areas and deeps(accumulation basins)will be discussed separately.Seasonal variability for total mercury in the accumulation basins(GD,BO,and GO)within the same station varied in the range from5%to33%,except one case in Bornholm Deep,where it reached67%.The variability related to patchiness ranged from 9%to34%.Thus the average uncertainty,given as Relative Standard Deviation,attached to a singular total mercury result is in the range of20%.For organic mercury seasonal variability varied from 4%to32%,while the spatial variability ranges from4%to31%. Methyl mercury spatial and temporal distributions were similar, amounting to4–36%RSD for seasonal and2–34%RSD for spatial differences,resulting in15%average uncertainty.Thus the average concentrations of mercury obtained in this study can be regarded as representative for the sediments of the Southern Baltic accumu-lation basins.The uncertainty is less than20%of the average values (Fig.2).Different situation is observed in the coastal areas–there sea-sonal variability given as RSD reaches103%,115%and121%respec-tively for total,organic and methyl mercury,while patchiness related uncertainty reaches77%,44%and45%for the respective forms.This translates to an average uncertainty of44%for all stud-ied mercury species.Such differences might be attributed to both the dynamics of shallow sediments and variable riverine mercury input.The latter directly controls composition of marine sediments in those areas(Huzarska,2013).Especially pronounced differences observed close to the Vistula mouth might be caused by theflood in May2010,the biggest one since1850.At the time of theflood exceptionally large quantities of mercury were transported with the run-off(Saniewska et al.,2014;Wielgat-Rychert et al.,2013).Observed seasonal variability and patchiness is not limited to mercury species and results from heterogeneity of sediment and environmental conditions.The former could be characterized by organic matter content,granulometry and oxidative state–factors that strongly influence sedimentary mercury concentration (Pempkowiak et al.,1998).Variability of thefine fraction contribu-tion,organic carbon content and redox potential is presented in Table1.Organic carbon variability in the whole data set was similar for accumulation and coastal areas,and varied from5.56%to13.58%, whilefine fraction contribution was markedly more variable closer to the coast.Redox potentials varied in the range from3.9%to309% of the average.Thus the observed heterogeneity in mercury con-centrations(Fig.2)can be attributed to sediment texture differ-ences(in coastal areas)and combined effect of both organic carbon and redox conditions variabilities.Concentrations of total mercury(THg),organic mercury (HgOrg)and methylmercury in marine sediments from the South-ern Baltic varied in the range5.8–225(average:103)ng gÀ1dry weight,90–1240(320)pg gÀ1dry wt.and60–940(230)pg gÀ1dry Fig.1.Distribution of sediment sampling stations.wt.,respectively (Fig.3).The highest levels of THg and MeHg were found in sediments from the Gdansk Deep and the vicinity of the Vistula mouth,respectively.The lowest concentrations of both THg and MeHg were found in sediments collected close to the Odra mouth located in the Bay of Pomerania.This can be attributed to the morphology of the Odrariver estuary,where the Szczecin Lagoon acts as ‘filter’for the river run-off discharged to the Pomeranian Bay (see Fig.1).In the case of the Vistula River estuary,the morphology is different –the river run-off and the loads of chemicals it carries are discharged directlyto the Gulf of Gdan´sk (Pempkowiak et al.,2000).Craig (1986)reported concentration ranges of 200–400ng g À1THg for uncontaminated marine sediments,whereas heavily pol-luted sediments in urban,industrial or mining areas can contain up to 100l g g À1of total mercury.Sedimentary levels of THg and MeHg reported in the literature are presented in Table 2.Our results indicate that the mercury concentrations averages and ranges,determined in sediments from the study area,are lower than those reported in other areas (Covelli et al.,2001;Jin et al.,2012;Kannan and Falandysz,1998;Mzoughi et al.,2002;Spada et al.,2012)with the exception of the level reported by Asmund and Nielsen (Asmund and Nielsen,2000)who indicated back-ground mercury levels of 24ng g À1in sediments from the Green-land Shelf.The highest values were recorded in sediments from Gulf of Trieste (the Adriatic),influenced by the contaminated river Soca/Isonzo,for centuries draining the cinnabar-rich deposits of the Idrija mining district,in the Northwestern part of Slovenia (Covelli et al.,2001).MeHg concentrations measured in the study area are character-istic of anoxic polluted sediments (Kwokal et al.,2002).Concentra-tions measured within this study are lower than these reported for period 1992–1994by Kannan and Falandysz (1998)by a factor of two for the same region,a feature difficult to explain taking into account that both seasonal and spatial variability of mercury con-centrations do not exceed 20%of the average,and the fact,that total mercury concentration observed in this study are comparable to the values observed in 1993–1995(Pempkowiak et al.,1998).This suggests a change in methylating potential of the Baltic sediments since 1990s,which could be attributed i.e.to the overall improvement of oxic conditions on the bottom (Feistel et al.,2008).The contribution of methylmercury to total mercury in sedi-ments of the study area ranged from 0.14%to 1.05%which falls within the range reported in the literature for marine environ-ments (Cossa et al.,1996;Mason et al.,1994).This might suggest a low methylation potential of marine sediments in the study area.Correlation analyses showed that THg was strongly correlated with MeHg in sediments (Spearman R =0.82,p <0.01).The established relation is calculated for all analyzed samples,except three samples collected close to the Vistula mouth,(Fig.4),since the samples in question were collected shortly after major flood in May,2010.The flood has introduced large loads of both mercury and organic matter to the Baltic Sea (Saniewska et al.,2014),and may well explain the elevated concentrations of both THg and MeHg there.In the remaining areas,reducing conditions were observed in sediments (the measured red-ox potential was in the range from À122to 66mV).The measured redox potential indicates that the conditions in sediments were appropriate for the sulfate reducing bacteria to reduce sulfate to sulfide.As a result labile mercury forms are transformed to mercury sulfide (Bełdowski and Pempkowiak,2007)that is sparingly soluble in aqueous solution.Once deposited as HgS,mercury is presumably not available for methylation (Boening,2000).However,bioturbation or physical mixing can introduce oxygen to sediments that leads to oxidation of HgS and thus remobilize a fraction of HgS (Stein et al.,1996).Moreover,even within the same location,the percentage of methyl mercury varied to some extend suggesting that other factors such as organic matter and microbial activity may influence or even play a significant role in the methylation process (Bełdowski et al.,2009)Most pronounced differences were observed in the Born-holm Deep (0.21–1.03%)and in the vicinity of river mouths (Vistula –0.14–0.61%;Odra –0.64–1.05%).Fig.2.Concentrations of total mercury (A),organic mercury (B)and methylmer-cury (C)in sediments of the Gdansk Deep (GD),Gotland Deep (GO),Bornholm Deep (BO),Gdansk Bay (V)and Pomeranian Bay (O).Bars represent the three seasonal samplings (Spring,2009;Autumn,2009;Spring,2010).Error bars represent one standard deviation of three samples collected within 1km 2at a given location.Table 1Median values in the studied sediments and ranges of organic carbon (Corg)concentration (mg/g),fine fraction contribution (<0.063)(%)and redox potential (Eh)(mV).Corg (mg/g)<0.063(%)Eh (mV)GD 7.9(6.2–9.1)92.61(89.65–94.87)À76(À129À+9)GO 11.8(10.8–12.9)87.94(83.58–91.51)+5(À15À+15)BO 7.7(6.3–9.1)62.72(59.41–66.72)+47(+30À+66)V 4.4(3.6–5.2) 4.23(2.54–5.99)+158(+76À+236)O2.5(2.1–3.0)0.93(0.49–1.31)+234(+221À+245)Bulletin 87(2014)388–395391Organomercury compounds are those in which mercury is bonded directly to the carbon atom e.g.CH3Hg(I)and C2H5Hg(I) (Hintermann,2010).Several extracting agents were used for sepa-rating organomercury compounds from sediments so far:toluene (Miller et al.,1995),chloroform(Eguchi and Tomiyasu,2002; Tomiyasu et al.,2000)and dichloromethane(Renneberg and Dudas,2001).However,with the use of these solvents not only the organomercury compounds but also a fraction of the mercury complexed by organic ligands is extracted(Eguchi and Tomiyasu,2002).In this study chloroform was used as an extracting agent to separate this operationally defined fraction of mercury,called here organic mercury(HgOrg).Obviously organic mercury com-prises methyl mercury as defined in this study.The average con-centration of mercury in this fraction in the study area is 0.42ng gÀ1(range0.10–1.44ng gÀ1).Concentrations of organic mercury in the range:0.9–26ng gÀ1were determined in the mar-ine bottom sediments from the Yatsushiro Sea in Japan(Tomiyasu et al.,2000),in the soil samples from the area strongly pollutedTable2Total mercury and methylmercury levels reported for sediments in different coastal seas.Study area THg conc.(ng gÀ1)MeHg conc.(pg gÀ1)SourceAverage Range Average RangeGulf of Trieste5240100–23,30016900200–60,100Covelli et al.(2001)Adriatic seaLagoon of Bizerte13010–650530nd–3200Mzoughi et al.(2002) Mediteranean off TunisiaGulf of Taranto2770360–7730108001000–40,000Spada et al.(2012)Ionian SeaJade Bay10835–243––Jin et al.(2012)North SeaVistula Mouth7117–15335468–940This study(Gulf of Gdansk)Odra mouth96–137561–94This study(Pomeranian Bay)Gdan´sk Deep315220–420––This studyGulf of Gdansk16437–88064535–1700Kannan and Falandysz(1998) Baltic SeaGdan´sk Basin17628–473Bełdowski and Pempkowiak(2007) Gdan´sk Deep190130–370Pempkowiak et al.(1998) Bornholm Deep64Bełdowski and Pempkowiak(2007) Bornholm Deep5625–84This study392J.Bełdowski et al./Marine Pollution Bulletin87(2014)388–395with mercury near the cinnabar mine and processing plant: 1–28ng gÀ1(Bloom and Katon,2000;Bloom et al.,2003;Miller et al.,1995),or near a chlor-alkali producing plant:9ng gÀ1 (Bloom and Katon,2000;Bloom et al.,2003).Much higher concen-trations of organic mercury were found near a gold mine: 1000ng gÀ1(Miller et al.,1995).Contribution of HgOrg to THg in the study area amounts to2%, on the average.In general,the contribution of HgOrg to THg in sed-iments of other marine areas is low.For example,in bottom sedi-ments from the Minamata Bay(Japan),the contribution varied from1%to4%.On occasion it can be much higher,however–e.g. in the Kagoshima Bay(Japan)where submarine fumaroles affect mercury speciation the range was from7%to37%,(Eguchi and Tomiyasu,2002;Sakamoto et al.,1995).In the samples of soil and sediments from the regions polluted with mercury e.g.near cinnabar mines or near chlor-alkali plants,the contribution of organic mercury to the total mercury concentration was very low (Bloom and Katon,2000;Bloom et al.,2003;Martian-Doimeadios et al.,2000;Miller et al.,1995;Renneberg and Dudas,2001).There is a linear dependence between methyl mercury and organic mercury in the analyzed sediments.Relationships pre-sented in Fig.5shows that in the study area it is possible to estimate methylmercury using the organic mercury concentration,with a limited certainty,however.The contribution of methylmercury to organic mercury concentrations in sediments ranges from42%to 77%,while the dependence sets the contribution of MeHg to HgOrg at63%.In the Southern Baltic,accumulation areas of sediments are located in the so-called deeps,at the depths greater than80m. As the halocline,in the Southern Baltic,persists at the depth of 60–70m the sediments of the accumulation areas are anoxic, and characterized by low red-ox potentials.Relationships between MeHg,HgOrg and redox potentials are linear with high Spearman rank coefficients(R=À0.75for MeHg and R=À0.71for HgOrg), especially for MeHg(Fig.6)and both are statistically significant with p<0.01.This suggests,that although both forms of mercury are closely related,organic mercury fraction includes also species that do not comprise mercury bonded to organic carbon atoms, i.e.mercury complexed by humic substances.Such complexes may comprise up to40%of THg in the Baltic sediments (Bełdowski and Pempkowiak,2007).Obviously not all of the com-plexes are extracted with organic solvent,as the contribution of organic mercury fraction to total mercury is just2%.High concentrations of methyl mercury and organic mercury in the vicinity of the Vistula mouth in sediment samples collected in 2010were measured.These are associated with relatively high val-ues of the redox potential(76–115mV)and thus seem to contra-dict the conclusion.However,mercury could be methylated in the inundated areas,and brought to the Baltic Sea as methyl mer-cury(Saniewska et al.,2014),during the extremeflood in2010. Methylation of mercury in inundated areas was reported in other areas of the world(Heaven et al.,2000).To characterize concentrations of sedimentary mercury in a given area one sample collected at a single sampling point is insuf-ficient as substantial variability at short distances needs to be taken into account.This study proved that in the Southern Baltic the short distance spatial variability,as characterized by the Rela-tive Standard Deviation,is close to20%of the average(n=3).The highest variability was observed in coastal areas,which results most probably from variable riverine input of mercury,and inho-mogeneity of sediments in the shallow areas.Concentrations of total mercury in the Baltic surface sediments exceed the background values by a factor of three(Pempkowiak, 1991).Despite this sediments of the Southern Baltic can be regarded as moderately contaminated with mercury on the back-ground of sedimentary concentration in other coastal areas.The obtained results characterize distribution of mercury spe-cies in sediments of the Southern Baltic Sea.The highest concentra-tions of THg were found in the stations located in the Gdansk Deep. MeHg concentrations,measured in this study,are characteristic of anoxic polluted sediments world-wide.The so called organicJ.Bełdowski et al./Marine Pollution Bulletin87(2014)388–395393mercury that is operationally defined as mercury extracted with organic solvents is well correlated to methylmercury.The latter constitutes,on average some62%of organic mercury.Methylmer-cury originates from the in situ methylation of inorganic mercury as there is a highly significant linear dependence with red-ox potential.However,there are indications that methyl mercury is also brought to the Southern Baltic with river run-off.In the coastal areas,surface sediments showed high levels of MeHg,most likely,as a response to the extremeflood that affected the region shortly before sampling.Since majorfloods occur every few years,it seems that methyl mercury originating fromfloods does not persist for long time periods(several years)(Huzarska, 2013;Wielgat-Rychert et al.,2013).According to previous studies, most mercury in Baltic sediments is converted to either insoluble HgS or mercury(II)complexed to refractory organic substances (Bełdowski et al.,2009).This suggests that the historical study (Kannan and Falandysz,1998)showing methylmercury concentra-tions twice higher than the contemporary ones,most likely,repre-sented either specific situation that is not typical of the region,or reflects a change that has occurred in the region since1992–94 until present day.Gdan´sk Deep is characterized by the highest con-centration of total mercury,organic mercury and methyl mercury from all studied accumulation basins(Gdan´sk,Gotland and Born-holm Deeps).This can be attributed to the influence of the Vistula River–the second largest river in the Baltic Sea.Thus it seems,that river borne mercury contamination of surface sediments must be considered,in the Baltic Sea,on equal terms with the atmospheric input of this metal.AcknowledgementsThis study is a part of the Institute of Oceanology Polish 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D.A.,Anderson,M.R.,Schneider, D.C.,1999.Influence of physical and chemical characteristics on mercury in aquatic sediments.Water Air Soil Pollut.110,347–362.Heaven,S.,Ilyushchenko,M.A.,Kamberov,I.M.,Politikov,M.I.,Tanton,T.W.,Ullrich, S.M.,Yanin,E.P.,2000.Mercury in the River Nura and itsfloodplain,Central Kazakhstan:II.Floodplain soils and riverbank silt deposits.Sci.Total Environ.260,45–55.HELCOM,2011.The Fifth Baltic Sea Pollution Load Compilation(PLC-5),Baltic Sea Environment Proceedings.HELCOM,220pp.Hintermann,H.,anomercurials.Their Formation and Pathways in the Environment.RSC publishing,Cambridge,pp.365–401.Huzarska,K.,2013.Spatial distribution of biological and physical sediment parameters in the western Gulf of Gdansk.Oceanologia55,453–470.Jin,H.F.,Liebezeit,G.,Ziehe,D.,2012.Distribution of total mercury in surface sediments of the Western Jade Bay,Lower Saxonian Wadden Sea,Southern North Sea.Bull.Environ.Contam.Toxicol.88,597–604.Kannan,K.,Falandysz,J.,1998.Speciation and concentrations of mercury in certain coastal marine sediments.Water Air Soil Pollut.103,129–136.Kwokal,Z.,Franciskovic-Bilinski,S.,Bilinski,H.,Branica,M.,2002.A comparison of anthropogenic mercury pollution in Kastela Bay(Croatia)with pristine estuaries in Ore(Sweden)and Krka(Croatia).Mar.Pollut.Bull.44,1152–1157. Laurier, F.J.G.,Cossa, D.,Gonzalez,J.L.,Breviere, E.,Sarazin,G.,2003.Mercury transformations and exchanges in a high turbidity estuary:the role of organic matter and amorphous oxyhydroxides.Geochim.Cosmochim.Acta67,3329–3345. Liang,L.,Horvat,M.,Bloom,N.S.,1994.An improved speciation method for mercury by Gc Cvafs after aqueous-phase ethylation and room-temperature precollection.Talanta41,371–379.Logar,M.,Horvat,M.,Akagi,H.,Pihlar,B.,2002.Simultaneous determination of inorganic mercury and methylmercury compounds in natural waters.Anal.Bioanal.Chem.374,1015–1021.Martian-Doimeadios,R.C.R.,Wasserman,J.C.,Bermejo,L.F.G.,Amouroux, D., Nevado,J.J.B.,Donard,O.F.X.,2000.Chemical availability of mercury in stream sediments from the Almaden area,Spain.J.Environ.Monit.2,360–366. Mason,R.P.,Fitzgerald,W.F.,Morel,F.M.M.,1994.The biogeochemical cycling of elemental mercury–anthropogenic influences.Geochim.Cosmochim.Acta58, 3191–3198.Miller,E.L.,Dobb,D.E.,Heithmar,E.M.,1995.Speciation of mercury in soils by sequential extraction.In:USEPA Metal Speciation and Contamination of Surface Water EPA,Jekyll Island,GA,USA.Mzoughi,N.,Stoichev,T.,Dachraoui,M.,El Abed,A.,Amouroux,D.,Donard,O.F.X., 2002.Inorganic mercury and methylmercury in surface sediments and mussel tissues from a microtidal lagoon(Bizerte,Tunisia).J.Coast.Conserv.8,141–145. Pacyna,E.G.,Pacyna,J.M.,Steenhuisen,F.,Wilson,S.,2006.Global anthropogenic mercury emission inventory for2000.Atmos.Environ.40,4048–4063. Pempkowiak,J.,1991.Enrichment factors of heavy-metals in the southern Baltic surface sediments dated with Pb-210and Cs-137.Environ.Int.17,421–428. Pempkowiak,J.,Cossa, D.,Sikora, A.,Sanjuan,J.,1998.Mercury in water and sediments of the southern Baltic Sea.Sci.Total Environ.213,185–192. Pempkowiak,J.,Chiffoleau,J.F.,Staniszewski,A.,2000.The vertical and horizontal distribution of selected trace metals in the Baltic Sea off Poland.Estuar.Coast.Shelf Sci.51,115–125.Quevauviller,P.,Andersen,K.,Merry,J.,van der Jagt,H.,1998.Interlaboratory study to improve the quality of trace element determinations in groundwater.Analyst 123,955–957.Renneberg, A.J.,Dudas,M.J.,2001.Transformations of elemental mercury to inorganic and organic forms in mercury and hydrocarbon co-contaminated soils.Chemosphere45,1103–1109.Sakamoto,H.,Tomiyasu,T.,Yonehara,N.,1995.The contents and chemical forms of mercury in sediments from kagoshima bay,in comparison with Minamata Bay and Yatsushiro Sea,Southwestern Japan.Geochem.J.29,97–105. Saniewska,D.,Beldowska,M.,Beldowski,J.,Saniewski,M.,Kwasniak,J.,Falkowska, L.,2010.Distribution of mercury in different environmental compartments in the aquatic ecosystem of the coastal zone of the Southern Baltic Sea.J.Environ.Sci.–China22,1144–1150.Saniewska,D.,Bełdowska,M.,Bełdowski,J.,Je˛druch,A.,Saniewski,M.,Falkowska,L., 2014.Mercury loads into the sea associated with extremeflood.Environ.Pollut.191,93–100.Spada,L.,Annicchiarico,C.,Cardellicchio,N.,Giandomenico,S.,Di Leo,A.,2012.Mercury and methylmercury concentrations in Mediterranean seafood and surface sediments,intake evaluation and risk for consumers.Int.J.Hyg.Environ.Health215,418–426.Stein, E.D.,Cohen,Y.,Winer, A.M.,1996.Environmental distribution and transformation of mercury compounds.Crit.Rev.Environ.Sci.Technol.26,1–43. Szymczycha, B.,Miotk,M.,Pempkowiak,J.,2013.Submarine Groundwater Discharge as a Source of Mercury in the Bay of Puck,the Southern Baltic Sea.Water Air and Soil Pollution,224.394J.Bełdowski et al./Marine Pollution Bulletin87(2014)388–395。

海洋观测浮标中英文对照外文翻译文献

海洋观测浮标中英文对照外文翻译文献

中英文对照外文翻译文献(文档含英文原文和中文翻译)译文:支持美国航天局地球科学事业的下一代海洋观测浮标简介伍兹霍尔海洋研究所与杰克逊和图尔正在开发一款改良版的支持美国航天局地球科学事业的系船测定浮标系统。

此项新型设计运用了伍兹霍尔海洋研究所在浮标、系泊、传感系统方面的海洋经验,并结合了杰克逊和图尔在航空遥测和计算机系统方面的专长。

浮标系统包括一整套气象传感器、水温、传导性(盐度)、生物光学传感器和辐射计在不同深度的性能,以及应用于海流的声学多普勒海流剖面仪。

此系统可以对海洋科学研究在全世界范围内的陆架区域进行部署调配,包括海洋水色卫星地面真实性验证。

它将新一代近地轨道通信卫星(LEO)应用于两方面,高通量指挥控制和数据遥测。

1.浮标结构这些美国航空局浮标系统由钢和一个铝制的泡沫浮圈制成。

钢,用于低成本和简单的结构建造,它们被热镀锌,并且为了防止腐蚀而被涂层。

一些旧的钢护浮标(潜水式有塔状物的网状浮子)在20年后仍然还在使用,所以其使用寿命不是问题。

而且,基底用重钢棒线材制成可以减少同铝制浮标一样必须要增加锌制或铅制重物来进行压载。

浮标塔由6061-T6铝材制成,因为这种材料轻,塑料垫圈可以使钢基底与电隔离。

安装在塔上的有一个雷达反射器、闪光灯式海洋监视巡防、遥测天线、气象传感器、太阳能电池板和一个阿尔戈斯定位信标天线。

太阳能电板可以通过摆动从而进入到浮标中心的仪表井。

这个井直径24”深45”为电池、太阳能电池板调节器、电力输送系统、数据处理和储存系统、遥测系统和后备阿尔戈斯定位信标提供了足够的空间。

可以从其顶部的一个开口进入到浮标的水密电子井。

较大直径可以允许一个人侧身进入到井中以对其底部的电池进行作业。

为了简易维修而装配电子器件一直以来都是一个问题。

在类似但是较小的GLOBEC(GLOBEC)浮标中,电池和电子器件被拧在电子井每一面的栏杆上。

俯身在小井中对这些器件进行作业的确很困难。

在这个新型的浮标中,电子器件安装在支架上,支架可以由焊接在井内部的四个分开的导管进行滑动。

写一篇关于海洋勘测的意义和建议的英语作文

写一篇关于海洋勘测的意义和建议的英语作文

写一篇关于海洋勘测的意义和建议的英语作文The Significance and Suggestions on Marine Seismic SurveyIntroductionMarine seismic survey plays a crucial role in modern marine research and exploration. With the development of technology, the significance of marine seismic survey is becoming increasingly apparent. In this essay, I will discuss the importance of marine seismic survey and provide some suggestions for future research.Significance of Marine Seismic Survey1. Understanding the Earth's StructureMarine seismic survey allows researchers to study the Earth's structure beneath the ocean floor. By using seismic waves to image the subsurface, scientists can gain insights into the composition of the Earth's crust and mantle. This information is vital for understanding plate tectonics, seismic activity, and natural resource exploration.2. Natural Resource ExplorationMarine seismic survey is essential for locating and extracting natural resources such as oil, gas, and minerals. By mapping thesubsurface structure of the ocean floor, researchers can identify potential reservoirs and assess their economic viability. This information is crucial for the energy industry and plays a significant role in ensuring a stable and secure energy supply.3. Environmental ProtectionMarine seismic survey can also contribute to environmental protection by providing valuable data on the marine environment. By mapping the seafloor and identifying biodiversity hotspots, researchers can help inform conservation efforts and marine protected area designation. This information is essential for preserving marine ecosystems and protecting endangered species.Suggestions for Future Research1. Develop Advanced Seismic Imaging TechniquesTo improve the resolution and accuracy of marine seismic survey data, researchers should focus on developing advanced imaging techniques. This includes the use of higher frequency seismic sources, multi-component sensors, and advanced processing algorithms. By enhancing the quality of seismic images, researchers can gain a more detailed understanding of the subsurface and improve resource exploration efforts.2. Incorporate Machine Learning and AIMachine learning and artificial intelligence can play a significant role in enhancing the efficiency and accuracy of marine seismic survey data interpretation. By training algorithms with large datasets, researchers can automate the processing and interpretation of seismic data, leading to faster and more reliable results. This approach can also help identify subtle subsurface features that may be missed by traditional interpretation methods.3. Enhance Collaboration and Data SharingTo maximize the impact of marine seismic survey research, researchers should increase collaboration and data sharing efforts. By working together and sharing data, researchers can combine their expertise and resources to address complex research questions and improve the overall quality of scientific knowledge. This approach can also help reduce duplication of efforts and increase the efficiency of marine seismic survey projects.ConclusionIn conclusion, marine seismic survey plays a vital role in understanding the Earth's structure, natural resource exploration,and environmental protection. By developing advanced imaging techniques, incorporating machine learning and AI, and enhancing collaboration and data sharing, researchers can improve the efficiency and accuracy of marine seismic survey research, leading to new discoveries and insights into the marine environment.。

海洋测绘领域常用英语词汇

海洋测绘领域常用英语词汇

海洋测绘领域常用英语词汇001海洋测量marine survey002海洋大地测量marine geodetic survey003海底控制网submarine control network004岛陆联测island-mainland connection survey005海洋水准测量marine leveling006当地平均海面local mean sea level007日平均海面daily mean sea level008月平均海面monthly mean sea level009年平均海面yearly mean sea level010多年平均海面multi-year mean sea level011平均海面季节改正seasonal correction of mean sea level012海面地形sea surface topography013海洋测量定位marine survey positioning014光学[仪器]定位optical instrument positioning015卫星定位satellite positioning016无线电定位radio positioning017水声定位acoustic positioning018组合定位integrated positioning019圆一圆定位(又称“距离一距离定位”)range-range positioning 020双曲线定位(又称“测距差定位”)hyperbolic positioning021极坐标定位(又称“距离方位定位”)polar coordinate positioning 022差分法定位differentiation positioning023位置线line of position, LOP024位置线方程equation of LOP025位置[线交]角intersection angle of LOP026位置面surface of position,SOP027定位点间距positioning space028等角定位格网equiangular positioning grid029辐射线格网radial positioning grid030双曲线格网hyperbolic positioning grid031等距圆弧格网equilong circle arc grid032等精度[曲线]图equiaccuracy chart033岸台(又称“固定台”)base station034船台(又称“移动台”)mobile station035跟踪台track station036监测台(又称“检查台”)monitor station,check station037台链station chain038主台main station039副台slave station040相位周(又称“巷”)phase cycle,lane041相位周值(又称“巷宽”)phase cycle value,lane width042相位稳定性phase stability043相位多值性phase ambiguity044相位漂移phase drift045固定相移fixed phase drift046联测比对comparison survey047联测比对点point of comparison survey048接收中心receiving center (注:船台接收岸台发射的无线电信号的实际接收点,该点有时与天线位置不一致。

关于用军用仪器监测鲸英语阅读

关于用军用仪器监测鲸英语阅读

关于用军用仪器监测鲸英语阅读(实用版)目录1.引言2.军用仪器在鲸鱼监测中的应用3.鲸鱼监测的重要性4.军用仪器的优势和局限性5.结论正文一、引言随着科技的发展,军用仪器在各个领域的应用越来越广泛。

其中,在鲸鱼监测领域,军用仪器也发挥着重要作用。

本文将探讨军用仪器在鲸鱼监测中的应用,以及其优势和局限性。

二、军用仪器在鲸鱼监测中的应用鲸鱼作为地球上最大的生物,其生存状态和生态环境备受关注。

近年来,军用仪器在鲸鱼监测中发挥着重要作用。

例如:1.声纳技术:声纳是一种利用水中声波传播原理来探测目标的技术。

在鲸鱼监测中,声纳可以捕捉到鲸鱼的声音,从而帮助研究人员了解鲸鱼的种类、数量、位置等信息。

2.红外热像仪:红外热像仪是一种利用物体的红外辐射特性来探测目标的技术。

在鲸鱼监测中,红外热像仪可以在夜间或者低能见度条件下,捕捉到鲸鱼的体温和体表特征,从而实现对鲸鱼的远距离监测。

3.无人机:无人机作为一种新兴的监测手段,在鲸鱼监测中具有广泛的应用前景。

无人机可以在远距离观察鲸鱼的同时,避免对鲸鱼造成干扰。

此外,无人机还可以搭载其他监测设备,如摄像头、声纳等,实现对鲸鱼的多方位监测。

三、鲸鱼监测的重要性鲸鱼作为海洋生态系统的顶级捕食者,对维持海洋生态平衡具有重要意义。

通过对鲸鱼的监测,可以了解鲸鱼的种群数量、分布状况、生态环境等信息,从而为保护鲸鱼提供科学依据。

四、军用仪器的优势和局限性军用仪器在鲸鱼监测中具有明显优势,如精度高、距离远、抗干扰能力强等。

然而,军用仪器也存在一定的局限性,如设备成本高、操作复杂、能耗大等。

因此,在实际应用中,需要根据具体情况选择合适的军用仪器。

五、结论军用仪器在鲸鱼监测中发挥着重要作用,其应用有助于更好地保护鲸鱼资源。

用于舰艇探测潜水艇距离和方位的声纳

用于舰艇探测潜水艇距离和方位的声纳

用于舰艇探测潜水艇距离和方位的声纳
潘积惠
【期刊名称】《船电通讯》
【年(卷),期】1991(000)002
【总页数】2页(P5,32)
【作者】潘积惠
【作者单位】无
【正文语种】中文
【中图分类】U666.7
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arine Picoplankton Cell Size by Using a Cooled, Charge-Coupled Device Camera with Image-Analyzed Fluorescence Microscopyt
CHARLES L. VILESt AND MICHAEL E. SIERACKI§* School of Marine Science and Virginia Institute of Marine Science, College of William and Mary, Gloucester Point, Virginia 23062
In the last 10 to 15 years, marine scientists have begun to recognize the important role that the smallest components of the plankton play in the aquatic food web and in organic- and inorganic-nutrient cycling. Concurrently, the need for faster, more accurate, and more detailed measurements of these plankton populations has increased. Nanoplankton (2 to 20 ,um) and picoplankton (0.2 to 2.0 ,um) are often identified and enumerated by fluorescence microscopy and visual counting (19, 20). This procedure is tedious, slow, and prone to operator error and inconsistency. It is especially difficult to measure the sizes of enough individual cells to adequately characterize population cell size distributions. Accordingly, there has been much interest in the development of new methods and technology to automate these measurements. Two complementary technologies for rapid cell measurement have emerged: flow cytometry and imageanalyzed fluorescence microscopy. Both techniques have been used with success to measure nanoplankton and autofluorescing phototrophic picoplankton (3, 22, 23, 26, 28). The ability to accurately and precisely measure the small end of the picoplankton size range, and particularly nonphotosynthetic bacteria, has proved to be problematic (18, 21). With recent advances in camera technology, we believe that image-analyzed fluorescence microscopy has good potential in this regard. Charge-coupled device (CCD) and video cameras. Digital image analysis using video cameras has been used success* Corresponding author. t Virginia Institute of Marine Science contribution no. 1727. t Present address: Department of Computer Science, University of Virginia, Charlottesville, VA 22903. § Present address: Bigelow Laboratory for Ocean Sciences, McKown Point, West Boothbay Harbor, ME 04575.
APPLIED AND ENVIRONMENTAL MICROBIOLOGY, Feb. 1992, p. 584-592
0099-2240/92/020584-09$02.00/0 Copyright © 1992, American Society for Microbiology
Vol. 58, No. 2
Received 9 May 1991/Accepted 19 November 1991
Accurate measurement of the biomass and size distribution of picoplankton cells (0.2 to 2.0 ,um) is paramount in characterizing their contribution to the oceanic food web and global biogeochemical cycling. Image-analyzed fluorescence microscopy, usually based on video camera technology, allows detailed measurements of individual cells to be taken. The application of an imaging system employing a cooled, slow-scan charge-coupled device (CCD) camera to automated counting and sizing of individual picoplankton cells from natural marine samples is described. A slow-scan CCD-based camera was compared to a video camera and was superior for detecting and sizing very small, dim particles such as fluorochrome-stained bacteria. Several edge detection methods for accurately measuring picoplankton cells were evaluated. Standard fluorescent microspheres and a Sargasso Sea surface water picoplankton population were used in the evaluation. Global thresholding was inappropriate for these samples. Methods used previously in image analysis of nanoplankton cells (2 to 20 ,um) also did not work well with the smaller picoplankton cells. A method combining an edge detector and an adaptive edge strength operator worked best for rapidly generating accurate cell sizes. A complete sample analysis of more than 1,000 cells averages about 50 min and yields size, shape, and fluorescence data for each cell. With this system, the entire size range of picoplankton can be counted and measured.
fully for enumerating nanoplankton (23, 26). However, video cameras have some inherent problems that make them inappropriate for measuring cells in the 0.2- to 2-p,m size fraction, a class dominated by bacteria, cyanobacteria, and small eukaryotes in aquatic environments. The fluorescence of small marine particles such as fluorochrome-stained bacteria is often at or below the noise level of video cameras, making such particles undetectable. When they are detectable, accurate sizing is difficult because of video noise. Video systems generally digitize 256 grey levels. Geometric stability, the ability of the camera to consistently sample the same spot in the scene, can also be a problem with video, especially when multiple images of the same scene are averaged to reduce noise. Nonlinearities in video camera response and analog-to-digital conversion make it difficult to compare the brightness of objects both within and between images (10). CCD cameras perform better than video in all of the areas described above. Originally employed in astronomy (11), they have found use in basic biological and biomedical research as well (7). Because they are cooled and scan slowly, random electronic and thermal noise is essentially absent (13). As with photographic cameras, exposure times can be varied. With longer exposures (e.g., 10 s), fluorescing objects invisible to the naked eye are detectable. CCD cameras are extremely sensitive and have brightness resolution as high as 16,000 real grey levels. Geometric stability is excellent, and camera response is extremely linear. Edge detection and cell sizing. A digital image is only an approximation of the true scene. The optics and electronics of the imaging device and the sampling process introduce errors that result in blurring. This can be partially removed by image restoration techniques that specifically account for optical blurring and sampling (6, 15). Because of blurring and
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