Grain Size Analysis and Depositional Environment Condition along the Beaches between Ovari and Kanyakumari,Southern Tamilnadu Coast,India

Textural analysis is the epicenter of any sedimentological research. Granulometric analyses of unconsolidated sediments are used as an index to decipher the depositional environment. The granulometric analysis display a significant fluctuation in mean size, sorting, skewness, and kurtosis due to the variation in wave energy and the extent of turbulence affecting the beach environment during the crosshore and alongshore movement of sediments. The present study is to document the variation in grain size distribution within foreshore sediments, i.e., between the high water line and the plunge point wherein the sediments are deposited under different wave energy conditions.     

近岸波浪和波生流环境中泥沙输运的数值模拟

Owing to lack of observational data and accurate definition,it is difficult to distinguish the Kuroshio intrusion water from the Pacific Ocean into the South China Sea(SCS).By using a passive tracer to identify the Kuroshio water based on an observation-validated three-dimensional numerical model MITgcm,the spatio-temporal variation of the Kuroshio intrusion water into the SCS has been investigated.Our result shows the Kuroshio intrusion is of distinct seasonal variation in both horizontal and vertical directions.In winter,the intruding Kuroshio water reaches the farthest,almost occupying the area from 18°N to 23°N and 114°E to 121°E,with a small branch flowing towards the Taiwan Strait.The intrusion region of the Kuroshio water decreases with depth gradually.However,in summer,the Kuroshio water is confined to the east of 118°E without any branch reaching the Taiwan Strait;meanwhile the intrusion region of the Kuroshio water increases from the surface to the depth about 205 m,then it decreases with depth.The estimated annual mean of Kuroshio Intrusion Transport(KIT) via the Luzon Strait is westward to the SCS in an amount of –3.86×106 m3/s,which is larger than the annual mean of Luzon Strait Transport(LST) of –3.15×106 m3/s.The KIT above 250 m accounts for 60%–80% of the LST throughout the entire water column.By analyzing interannual variation of the Kuroshio intrusion from the year 2003 to 2012,we find that the Kuroshio branch flowing into the Taiwan Strait is the weaker in winter of La Ni?a years than those in El Ni?o and normal years,which may be attributed to the wind stress curl off the southeast China then.Furthermore,the KIT correlates the Ni?o 3.4 index from 2003 to 2012 with a correlation coefficient of 0.41,which is lower than that of the LST with the Ni?o 3.4 index,i.e.,0.78.     

平均海面同步改正传递法的误差分析

给出了平均海面同步改正法中异步效应及余水位引起的误差的表达式。对中国沿海3组典型验潮站进行了数值计算,统计分析了异步效应与余水位引起的误差的量值与规律。     

电位测定法测海水氧化还原电位的不确定度评定

采用电位测定法对实际海水的氧化还原电位进行测定,分析了影响测量不确定度的主要来源,对曲线拟合、测定过程的标准溶液的使用、仪器使用和测量重复性等影响不确定度的分量进行分析,按JJF1059—1999《测量不确定度评定与表示》的规定进行合成,最终给出扩展不确定度。结果表明,实际海水电位值的合成标准不确定度为14.18 mV,扩展不确定度为28.4 mV(近似95%置信概率)。这样结果的表达更加客观和真实,更具有参考意义。     

胜利油田孤东海堤保滩促淤工程二维潮流数值模拟研究

以胜利油田孤东海堤保滩促淤工程为实例，采用二维潮流数值模拟方法，利用实测流速资料对该海区进行潮流计算，对所提出的不同工程方案进行比较，并分析其促淤效果，在此基础上给出工程方案的推荐结论。     

厦门海域贝类养殖环境中的大肠菌群和异养细菌

2005年和2006年春季(4月)和秋季(10月)研究了厦门海域贝类养殖环境(海水、底质)和养殖贝类中大肠菌群(TC)和异养细菌(HB)数量分布及其在不同介质中数量之间的相关性,并对贝类养殖环境卫生质量进行了评价。结果表明:潮间带贝类养殖区TC数量较高,虾池和浅海贝类养殖区的较低;虾池贝类养殖区HB数量较高,潮间带和浅海贝类养殖区的较低。总体上,厦门海域贝类养殖环境中TC和HB数量分布呈同安湾湾内和西海域高,同安湾湾口和大嶝海域低的格局。大多数站位海水中TC和HB数量春季稍高于秋季,养殖贝类体中TC和HB数量秋季高于春季,底质中HB数量春、秋季无明显差异,TC数量则秋季稍高于春季。浅海和虾池贝类养殖区海水与贝类、底质与贝类中TC和HB的数量之间均成显著正相关。贝类养殖区底质中HB和TC数量,软泥>粉砂质软泥>粉砂,贝类体内器官组织中HB和TC数量,僧帽牡蛎:外套膜>外套腔液>内脏团;缢蛏和菲律宾蛤仔:外套腔液>外套膜>内脏团。厦门海域贝类养殖环境受到TC和HB不同程度的污染,潮间带贝类养殖区和虾池贝类养殖区分别受到TC和HB的较重污染。     

海岛管理信息系统用户需求分析

中国是一个海岛大国,但在海岛管理方面还很落后。鉴于海岛信息的复杂性和信息时代的要求,应该建立一个涵盖全国海岛的管理信息系统。为此,从用户需求的角度,对建立海岛管理信息系统的问题进行了初步探讨。     

渤、黄海海冰的变化和预报结果分析

利用1951—2000年的渤、黄海的海冰资料，用小波分析和最优气候均态法对渤、黄海的海冰冰级进行分析和预测。小波分析结果较好地反映了渤、黄海海冰的变化规律，使对海冰的研究更符合实际情况。这必将有助于研究海冰变化的机理和不同尺度变化的相互作用。最优气候均态法较好地实现了对渤、黄海海冰的预测。此方法在海冰预报中不失为一种可用的方法。     

临港新城海域波浪影响下的码头不利作业天数分析

使用临港新城海域连续1 a的波浪实测资料,并依据码头不利作业标准,进行波浪影响下不利作业天数的分析论证。同时,使用芦潮港同步风资料建立相关关系,利用多年连续风资料推算的波浪影响下不利作业天数进行验证。     

茂名海域水体表层悬浮泥沙浓度时空分布特征的遥感分析

利用Gorden关系式,从茂名海域的多时相卫星影像定量反演了表层悬浮泥沙浓度的时空分布特征。经近期该海域实测悬沙资料验证表明,茂名沿海水体表层悬浮泥沙浓度偏低,一般低于200 mg/L;表层悬浮泥沙浓度在空间尺度上由岸向海呈带状分布,并逐渐降低,其中-1 m以浅区悬沙浓度最高,一般可超过100 mg/L,-10 m以深区浓度最低,一般低于20 mg/L。此外,沿海水体表层悬沙浓度往往在冬季高于夏季,大风天气高于平常天气。     

近红外光谱识别模拟海面溢油

对模拟溢油的石油类样品进行近红外光谱检测并进行了主成分分析,以主成分得分作为聚类的特征变量进行模糊聚类,采用近红外光谱测量结合主成分分析和模糊聚类法快速识别模拟溢油种类,并建立了样品聚类与识别模型。采用此模型对柴油、汽油和润滑油等334个与海水体积分数≥4∶10 000的模拟溢油样品进行了准确快速的分类和识别,为近红外光谱技术判别实际溢油样品提供了科学依据。     

浅海环境观测专用浮标和潜标锚泊系统的研究

文中着重介绍为改进浅海环境观测专用浮标和潜标锚泊系统所做的三件工作。一是提高水面标志浮标的抗台风、抗倾覆和抗沉能力以及连接件的流线型化;二是通过理论计算和水池试验,选用抗风能力强的配套的浮标／潜标系统系列;三是应用设计新型的打捞钩,及时而方便地将丢失在海底的仪器等打捞回来。     

南海北部陆架坡折附近表层沉积物的粒度特征和其输运趋势

对南海北部陆架坡折附近取的50个表层沉积物样品,作粒度测试,计算粒度参数。粒度分析表明研究区的沉积物主要存在4种类型:含砾砂、砾质砂、砂质砾和含砾泥质砂;沉积物组分中砾石和砂占绝对优势,基本上不含黏土。综合因子分析和聚类分析的结果把研究区划分为4类沉积区:Ⅰ类沉积区属于内陆架沉积区,Ⅱ类沉积区属于陆架坡折上部沉积区,Ⅲ类沉积区属于陆架坡折下部沉积区,Ⅳ类沉积区区属于陆架边缘沉积区,每类沉积区都代表着不同的沉积环境。研究区沉积物的粒径趋势分析结果显示,陆架坡折附近的沉积物主要向内陆架和外陆架边缘或上陆坡输运,同时存在着跨陆架输运和沿陆架坡折输运现象,这与研究区实测的底流方向相一致。本研究表明,南海北部陆架坡折附近的沉积环境和沉积物输运模式比较复杂和特殊。本研究对今后陆架和陆坡区其他相关的研究具有十分重要的指导和借鉴意义。     

海底沉积物保真采样器保温性能的数值模拟与实验研究

提出了一种新型海底沉积物原位保真采样系统.该系统通过机械机构实现样品舱原位转移和封装.并且样品舱的保温保压性能决定着样品分析数据的真实性.依据能量守恒定律.建立了样品舱保温模型非稳态传热的导热微分方程,并用有限元法对非稳态传热进行了数模计算;根据保温模型试验和温度场变化规律仿真数据,构建了参数优化设计模型.为海底沉积物保真采样系统快速设计提供了理论依据.实验和模拟分析结果表明.所建模型与实际情况吻合较好,可以满足实际工程要求.对海底油气勘探具有重要意义.     

Sensitivity analysis of nitrogen and carbon cycling in marine sediments

Biogeochemical cycles in coastal sediments encompass numerous interconnected processes and are sensitive to a high number of external forces. Usually a small subset of these factors is considered when developing state-of-the-art models of marine nutrient cycling. This study therefore aims to assess the degree of complexity required in the model to represent the dependency of major biogeochemical fluxes on both intrinsic as well as external factors. For this, a sensitivity analysis (SA) of the generic Integrated Sediment Model (ISM) was performed comparing two different model setups: 1) a back barrier tidal flat in the German Wadden Sea and; 2) a deep sea site in the Argentine Basin. Both setups were first calibrated to fit pore water profiles of SO₄²⁺, NH₄⁺ and CH₄. We then employed a new type of SA that evaluates parameter impact rather than targeting variable change.General structural stability of the model is demonstrated by similar sensitivity patterns of both setups regarding carbon and nitrogen cycling. Mean temperature, organic carbon bio-availability, bacterial adaptation and sediment texture emerge as the most influential parameters of ubiquitous importance. It appears that in coastal settings, transport and sediment mixing and the composition of suspended particles in the bottom water are especially important. The nitrogen cycle displays a high responsiveness to internal feedback mechanisms as well as interdependencies to carbon and metal cycling, which is statistically reflected by sensitivities to 79% of all parameters. In contrast, the carbon cycle appears to be mainly controlled by organic matter decay. The SA also pointed to unexpected responses of the sediment system, which are analyzed by further scenario calculations. These, for example, reveal a nonlinear response of nitrification, denitrification and benthic fluxes of NH₄ and NO₃ to changing bioturbation and bioirrigation due to the interactions of different metabolic pathways.     

一种古海洋环境的静态恢复法

研究地质历史中古海洋和古大气环境的演变具有十分重要的意义。古环境定量分析的关键是如何确定古环境的各种特征参数，如古气温、大气中O2分压、C02分压、海水pH值及海水的化学组成等。目前，国际上常用的方法包括：①沉积岩分析法；②包裹体分析法；③同位素分析法。我们系统地介绍了这几种方法，论述了海水pH值的梯度变化特征和蒸发环境下古海水的化学组成演变特征，并尝试提出了一条获得古海水化学组成的途径。     

Dynamic Risk Analysis of Permanent Deformation of Sea Embankment

For evaluation of the permanent deformation of a sea embankment under stochastic earthquake excitation, a robust dynamic risk analytical method is presented based on conventional permanent deformation analysis and stochastic seismic response analysis. This method can predict not only the mean value of maximum permanent deformation but also the reliability corresponding to different deformation control standards. The earthquake motion is modelled as a stationary Gaussian filtered white noise random process. The predicted average maximum horizontal permanent displacement is in agreement with the conventional result. Further studied are the reliability of permanent deformation due to stochastic wave details at one seismic motion level and the risk of permanent deformation due to stochastic seismic strength, i. e., the maximum acceleration in a long period. Therefore, it is possible to make the optimal design in terms of safety and economy according to the importance of a sea embankment. It is suggested tha     

胜利埕岛海域海底松软沉积物声学探测方法探讨

胜利埕岛海域位于复杂的黄河三角洲沉积体系中．由于黄河的断流,在风浪和海流作用下原三角洲体系受到侵蚀．在部分海底具有松散沉积物沉积。采用侧扫声纳、双频测深仪及浅地层剖面仪3种海上物探方法,对埕岛海域海底松软沉积物进行声学探测,确定了浮泥、软土层顶、海底界面及浮泥和软土层和海底界面及浮泥和软土层的厚度,研究了埕岛海域海底松软沉积物的基本分布变化规律,为今后海洋工程地质勘察海底松软沉积物奠定了基础。     

南黄海辐射沙脊群悬沙总体输运特征分析

利用2006年夏季江苏近海调查中流速流向以及含沙量资料,采用通量机制分解法,重点计算了南黄海辐射沙脊群地区悬沙输移总量以及各个分量,并对总体悬沙输运特点进行分析。辐射沙脊群地区悬沙输运受到潮汐系统影响,近岸有很强的向岸输沙,且呈现从近岸向外逐渐减小的趋势。在辐射沙脊群区域,悬沙浓度大,地形复杂,悬沙输移也较强较复杂。悬沙输运主要以平流输移为主,其他项贡献很小,其中潮汐捕获项与垂向净环流项表现出与潮汐系统特点相关的辐聚辐散现象。     

变分伴随数据同化方法在断面海温数值计算中的应用研究

以二维断面海温分布模型为例,利用海温实际观测数据,将变分伴随方法应用于断面海温初始场的优化。讨论了变分伴随方法的基本思想,分别从模型方程的连续和离散形式出发推导伴随模型系统,并对这两种途径建立的伴随系统之间的相互关系进行了分析。数值试验的结果表明了变分伴随数据同化方法在海温数值计算和数值预报业务中的良好的应用前景。