辽宁省国土规划编制的依据

辽宁省国土资源特点 辽宁省位于我国东北地区的南部,东南濒临黄渤两海,陆域与吉林、内蒙、河北接壤.处于东北经济区与环渤海经济区的结合部.陆域面积14.81万平方公里,占全国的1.5%:海域面积6.8万平方公里,其中近海3.5万平方公里.由东部山地、中部平原、西部丘陵、北黄海、辽东湾五元模块组成.区间自然地理差异较大,地势东西高,中间低,落差为70C米.地处温带大陆性季风气候区,四季分明.     

中国周边“海洋圈地”调查

5月13日,是联合国大陆架界限委员会接受各国提交海洋划界案的最后一天。根据各国提交的资料数据,委员会将做出技术性审定,决定所提交的划界案是否符合《联合国海洋法公约》。而这一决定将成为海洋划界的重要支持依据。     

福州市1:10 000海岸线修测的误差分析与探讨

针对数字海洋测绘产品的特点及其质量控制,对福州市1∶10 000海岸线修测成果的平面数学精度检测的测点误差分析进行分析和探讨。     

海域使用论证管理探讨

近年来,海域使用论证制度日趋完善,海域使用论证管理呈现不断加强和逐步规范的良好局面.海域使用论证作为科学用海、管海的重要技术依据,在海洋管理工作中具有极其重要的地位和作用.鉴于此,笔者针对海域使用论证管理的现状及存在的问题,探讨强化海域使用论证管理的措施,以兹交流.     

Suspended sediment transport and deposition in the Zhoushan Archipelago sea area

The transport mechanism and settlement characteristics of suspended sediments are analyzed in this article on the basis of measured data. Results indicate that the concentration and flux of suspended sediments decrease sharply from Hangzhou Bay to the offshore area. Suspended sediment transport is mainly controlled by advection transport and gravitational circulation transport. The settling velocity of suspended sediments gradually decreases from Hangzhou Bay to the offshore area. The settlement of suspended sediments mainly takes place during the turning phase of the tidal currents.     

湛江海域6种常见经济海藻的营养成分分析

分析采自湛江海域的粗枝软骨藻Chondria crassicaulis、日本沙菜Hypnea japonica、鱼栖菜Acanthophora sp、芋根江蓠Gracilaria blodgettii、平卧松藻Codium repens、网地藻Dictyota dichotoma等6种经济海藻的营养成分。结果表明:碳水化合物是这些海藻的主要营养成分,占藻体干重的42.81%～66.11%,平均为55.93%;粗蛋白含量6.63%～11.13%;粗脂肪含量最低,除网地藻D.dichotoma(2.85%)外,其余5种皆不足藻体干重的1%;粗纤维和灰分含量在种间差别较大;矿物质含量丰富,其中磷、铁和锌分别在平卧松藻C.repens、网地藻D.dichotoma和鱼栖菜Acanthophora中占藻体干重的0.093%、0.13%和0.0055%;氨基酸含量较高,其中Thr、Val、Ile、Leu、Phe几种必需氨基酸的含量均高于FAO标准;不少种类中汞、镉、铅、砷等含量超出我国食品卫生标准。海藻体内的营养成分含量因海藻种类和生长海域的不同而有差异。     

A culture-dependent survey of thermophilic bacteria from hot springs in Xiamen area in China

Microbes are believed to play important roles in ecosystem function in many environments. The hot springs of Xiamen Island are close to the Xiamen Sea, and may have some characteristics different from those of inland hot springs. Microbes living in the hot springs of Xiamen may have new characteristics. However, little is known about microbial communities of hot springs close to the Xiamen Sea. A cuhure-dependent survey of microbial population in the Xiamen hot springs was pcrformed by using an approach combining total cellular protein profile identification and 16S rRNA gene sequencing. A total of 328 isolates of bacteria were obtained from liquid and sediment samples from the Xiamen hot springs, including neutrophilie thermophilic bacteria and moderately thermophilic acidophiles. Neutrophilic thermophilic bacteria, which grow at a temperature range of 55-90℃ including Rhodothermus marinus (Strain 1) , Thermus thermophilus (Strain 2), Thermus thiopara (Strain 3) , Geobacillus stearothermophilus(Strain 4) , Geobacillus thermoleovorans (Strain 5) , and Pseudomonas pseudoal-caligenes (Strain 6), were recovered by 2216E plates. Moderately thermophilic acidophiles, which can grow at temperatures above 50℃ and a pH range of 1. 8-3.5 such as Alicyclobacillus acidoterrestris (Strain 8) , Sul-fobacillus acidophilus (Strain 9), and Sulfobacillus thermosulfidooxidans (Strain 10), were isolated on selective solid medium containing sulfur and Fe2+. Among these strains, Rhodothermus marinus, Thermus thermophilus and Geobacillus stearothermophilus are not only thermophilcs, but also halophiles. One bacterium strain (Strain 6) shared 99% nucleotide sequence homology with Pseudomonas pseudoalcaligenes on the 16S rRNA gene se-quence, but was quite different from Pseudomonas pseudoalcaligenes in biological characteristics, suggesting that it may represent a novel thermophilic species. Results indicated that various species of neutrophilic thermophiles and moderately thermophilic acidophiles were widely distributed in the Xiamen hot springs and that Rhodother-mus marinus and Thermus thermophilus dominated the cultivable microbial community.     

厦门湾沉积物对石油的吸附解吸规律研究

为了研究海洋沉积物对0#柴油配制的石油溶液的吸附解吸规律,采集了厦门湾15个站点的沉积物作为研究对象,分析了沉积物的主要理化特征之后,在实验室条件下,以SS5号站点沉积物为代表,模拟沉积物对石油的吸附-解吸过程,测定了沉积物对石油吸附、解吸的动力学曲线和吸附等温线.研究结果表明：沉积物对石油的吸附的平衡时间为0.76 h,解吸的平衡时间为7.8 h,沉积物对石油的吸附速率高于解吸速率,并且石油被沉积物吸附以后不会完全解吸出来.沉积物对石油的吸附等温线具有线性规律,接近理想吸附.研究还表明：沉积物对石油的吸附量与石油的浓度,沉积物粒径等因素有关.     

台湾海峡及其邻近海域潮汐数值计算

建立二维潮波模式,模拟了台湾海峡及其邻近海域（18～30°N,110～130°E）八个主要分潮（M2、S2、K1、O1、P1、Q1、K2、N2）,并利用中国大陆及环台湾岛20多个潮位站的实洲资料进行验证,计算结果与实测值吻合良好。此外,给出了八个主要分潮的同潮图,并逐个讨论了潮汐特征。结果艟示：（1）台湾海峡中的潮波运动是北部蜕化了的旋转潮波系统和南部的前进潮波系统共同作用的结果。（2）半日分潮南、北两支潮波在台湾海峡中部汇合,而今日分潮则在台湾海峡南部海域汇合后继续朝西南方向传播。（3）半日分潮振幅最高值发生在福建省湄洲湾－兴化湾一带,全日分湖最高值则出现在雷州半岛以东一带近岸海域。（4）N2、K2和O1、P1、Q1分湖的振幅、迟角分布分别同M2与K1分潮的整体分布趋势相似。     

环厦门海域沉积物放射性核素分布与沉积速率

用HPGe探测器γ谱仪测定了厦门海域两个沉积物岩心的放射性核素,研究了40K、137Cs、210Pb、226Ra、228Ra、228Th和238U 7种放射性核素的垂直分布特征.综合文献数据与我们的研究结果给出沉积物中7种核素的比活度分别为510～1 096、2.64～4.01、48.4～129、9.6～40.0、49.9～94.3、56.3～89.2、11.5～82.3Bq/kg.用210Pbex方法计算得到的厦门西南和东北海域的沉积速率为2.62、2.43cm/a.文献给出的环厦门海域沉积速率范围值为0.07～13.2cm/a,算术平均值为3.2cm/a,主要集中在0.07～2.5、3.5～6.0cm/a范围内.