渤海南部早-中更新统湖相沉积的粒度特征及其对沉积环境的指示

通过对莱州湾南岸Lz908孔下部47m沉积物的粒度分析,揭示了该地区沉积物的粒度特征:平均粒径介于3.2Φ~7.4Φ,大部分为黏土质粉砂,少部分为砂质粉砂,亦含有少量粉砂质砂;分选系数介于1.1~2.5,分选较差;偏度绝大多数介于0.7~2.4,表现为正偏和极正偏;峰度介于1.9~3.4,表现为平坦和正态。通过粒级组成、粒度象特征、粒度结构散点图等的综合分析,表明:钻孔下部沉积物与上部沉积物相比,指示了相对低能稳定的水动力环境;莱州湾南岸地区在早-中更新统处于浅湖相与深湖相交替存在的沉积环境。因此,本文认为对渤海莱州湾南岸地区沉积物粒度特征的研究可以有效的判断沉积环境,提取古环境信息,是沉积环境的重要替代指标。     

南极普里兹湾海域湍流扩散系数估计

基于Thorpe尺度方法,利用CTD数据,计算了南极普里兹湾海域的Thorpe尺度和湍流扩散系数,分析了观测区域(64°～69°S,66°～80°E)湍流翻转现象的强弱及分布。结果表明,在海底和地形粗糙区存在较大的Thorpe尺度(较强湍流翻转)和湍流扩散系数,湍流扩散系数最大值能达到10^-2m²/s量级,比平坦开阔海洋高2～3个数量级,部分观测站位的湍流扩散系数和湍动能耗散率表现出大-小-大的垂向分布结构,总水深较深的区域尤为明显;深水区域的浮力频率在海表面到500 m层比较大,浅水区域该现象不明显;湍动能耗散率在(67.25°S,73°E)周围和经度为78°E的各站位都表现相对较大,能达到10^-6 w/kg量级,个别站位甚至能达到10^-5 w/kg量级。     

热废水对大亚湾三种经济鱼类热效应的研究

对大亚湾3种重要经济鱼类包括黑鲷Sparusmacrocephalus、平鲷Rhabdosargussarba和细鳞Theraponjarbua的多项温度指标进行室内热效应模拟研究。结果表明：在驯化温度为25—33℃条件下,黑鲷、平鲷和细鳞3种鱼类的起始致死温度分别为34．96─36．42,34．78─35.62,38．75─39.39℃;最高起始致死温度分别为36.35,35.52℃和39.32℃;临界热最大值分别为38．08─40.50,38．28─40.40℃和42.40─43.64℃;最适生长温度分别为28,28℃和32℃;生长的最高周平均温度分别为30．78,30.51℃和34．44℃;短期暴露最高温度分别为34.04,33.57℃和37．90℃。根据黑鲷、平鲷和细鳞的多项温度指标,结合这些鱼类的生活习性分析和大亚湾基本环境特征的调查资料,就大亚湾核电站温排水对渔业资源影响的热效应问题进行初步探讨。     

锦州湾沾污沉积物急性毒性的海洋端足类检验

１９９２年９月￣１９９３年１月对锦州湾沾污沉积物的海洋端足类急性毒性效应进行了研究。从锦州湾湾顶到湾口沿西南－－东北方向每２ｋｍ等距离采集２７个表层沉积我校 品,应用海洋端足类Ａ ｍｐｅｌｉｓｃａ ａｂｄｉｔａ对这些样品进行了１０ｄ直流式急性毒性检验,检验指标为死亡率。结果表明,五里河河口处受试生物死亡率最高,为１００％,从湾顶该河口处沿东北方向随着距离增加,死亡率逐渐递减,笔架山处最低,仅为２．     

胶州湾北部水层生态动力学模型与模拟 Ⅱ.胶州湾北部水层生态动力学的模拟研究

利用建立起的浅海水层生态动力学箱式模型,模拟了胶州湾北部１９９５年的浮游植物、浮游动物、无机氮、无机磷、溶解氧以及ＤＯＣ和ＰＯＣ年变化特征。结果是合理的。通过模型参数敏感性实验分析,揭示了该模型系统的一些动力学特征     

海湾扇贝对海水池塘浮游生物和水质的影响

滤食性贝类可从天然水体和养殖水体中滤取大量的浮游物,并将滤食的物质以组织生长、粪便、排泄物等形式重新分配,进而对水质状况产生直接或间接的影响。已有的报道表明,滤食性贝类较多的湖区、海区浮游植物的数量、叶绿素a含量明显减少[1,2],浮游物颗粒规格的结构也会发生变化[3],水柱中小型浮游动物、细菌及水体的水流速度等也会受到一定的影响[4,5]。     

深圳大鹏湾大鹏半岛沿岸海域的一次调查与分析

一九九八年三月,我们在大鹏半岛海域调查时,恰逢深圳大鹏半岛近岸海域赤潮发生。结合我们对该区域内沿海水域调查结果进行分析,给出该海域的潮汐、潮流的基本特征及当时该海域的水质状况,为规划、保护该海域的海洋环境提供科学依据,并为研究赤潮发生成因提供参考资料。     

Quantitative analysis for maritime delimitation: Reassessing the Bay of Bengal delimitation between Bangladesh and Myanmar

This article examines technical aspects of the maritime boundary dispute between Bangladesh and Myanmar (the ‘Bay of Bengal case’). This dispute was the first maritime delimitation determined by the International Tribunal for the Law of the Sea (ITLOS). The 2012 decision was also the first time that a maritime boundary for the seabed and subsoil of the Exclusive Economic Zone (EEZ) and the extended continental shelf (ECS) was determined by international adjudication. This was also therefore the first time that detailed technical quantification of seabed areas within the EEZ and ECS was needed for achieving an equitable division of these maritime zones in an international forum. Following review of the principles of maritime delimitation on which the ITLOS reached its determination, this article analyzes the legal status and delimitation effect of St. Martin's Island. Concerning the question of whether the legal regimes of the EEZ and continental shelf should be treated differently in a single delimitation line, although the ITLOS determined that the legal regimes should not be distinguished in the present case, a different approach is proposed for future cases. The article identifies how quantitative modelling can be used to achieve an equitable boundary and proposes a model to adjust provisional equidistance lines in accordance with the complex geophysical rules prescribed for the outer limits of the ECS in Article 76 of the United Nations Law of the Sea Convention (LOSC).     

Status of Macrobenthic Community and Its Relationships to Trace Metals and Natural Sediment Characteristics

Laizhou Bay, located in the northwest of Shandong Peninsula, has complex transitional environments between terrestrial and marine ecosystems. In the present study, a total of 122, 131, and 139 species were collected in spring, summer, and autumn 2011, respectively. Species constitutions of macrobenthos were grouped into four phyla, of which annelida were the most abundant phylum, the average biomass proportion of echinodermata was the lowest, and the proportion of important species for mollusca was the highest. The structure of the macrobenthic community showed significant differences between sites, and greater divergence was observed between the third site (S03) and other stations. The ABC plots showed that the biomass curve lay below the abundance curve, and the W‐statistic value was negative. The result of the BOPA index showed that two stations had moderate ecological status in spring and that there were two heavily polluted sites and one moderately polluted site in summer. The BIO‐ENV analyses indicated that the grain‐size fractions together with trace metals (Hg, Pb, Zn, Cu, and Cr) could be considered as the major environmental variables influencing the macrobenthic patterns. The results together demonstrated that the macrobenthic communities in Laizhou Bay were negatively affected, perhaps by the tremendous impact of heavy metals in the sediments.     

胶州湾冬季浮游植物光合作用特征原位研究

目前关于中国近海浮游植物光合作用特征的研究较少,尤其是海洋浮游藻类冬季光合生理生态方面的研究少见报道。本实验利用浮游植物荧光仪Phyto-PAM测量了胶州湾浮游植物最大光化学量子产量、快速光曲线、光化学淬灭以及非光化学淬灭,通过显微镜镜检获得浮游植物群落结构组成与丰度结果,结合相应的环境因子,对胶州湾冬季浮游植物进行了原位光合作用特征研究。结果表明:调查期间胶州湾浮游植物具有较高的光合活性与潜力,最大光化学量子产量保持在0.69左右,光能利用效率大部分处于0.2—0.3之间,快速光曲线十分典型,当光强超过1000μmol/(s·m2)后依然能保持较好的光合活性,光化学淬灭值较高;当光强超过1500μmol/(s·m2)后,相对电子传递速率开始下降,实际光量子收益达到最低,非光化学淬灭升高,此时海洋浮游植物将光合机构吸收的过量光能以热能的形式耗散掉,有效地保护了胶州湾浮游植物的光合器官不因高光强的照射而受到损伤。冬季大部分时期胶州湾浮游植物丰度极低,但是湾内浮游植物具有较强的光合活性,加上相对稳定的水文、生物等环境以及较丰富的营养盐和相对有利的营养盐结构,是推动冬季浮游植物高峰期出现的关键生理生态因素。