黄河口现代海洋沉积高分辨率地震地层学研究

本文运用地震地层学的知识,结合KDG2和S3钻孔资料,对2002年得到的现代黄河口地区的浅地层地震剖面进行了分析解释,共划分出中更新世以来11个地震地层单元,对每个地震地层单元进行了地震相的有关描述,对剖面上出现的地质现象给予了合理推测和详细分析,并结合相邻的钻孔资料,与全球冰期进行对比,构筑了黄河口地区晚第四纪以来地层的沉积模式。     

应用Argo资料分析西北太平洋冬、夏季水团

应用Argo剖面浮标观测的温、盐度资料,分析了西北太平洋海域冬、夏季的温、盐度分布、水团结构及其分布。首先采用T-S点聚图法分析了该海域水团分布的基本情况,由点聚分析结果可知,该海域至少存在6种以上水团;再用模糊聚类软化法对水团作进一步划分,分别计算了该海域6至11类水团的F和△F值,结果表明,冬、夏季的△F值都以划分为8类时为最大,这与大洋水团的稳定性是一致的,因此,该海域冬、夏季水团以划分为8类最佳,它们分别是北太平洋热带表层水、北太平洋次表层水、北太平洋中层水、北太平洋副热带模态水、北太平洋深层水和赤道表层水,以及南太平洋次表层水和南太平洋中层水。     

基于单元复制的通用化离散格网系统生成算法

本文提出一种基于单元复制的通用化格网系统生成新算法。其核心是采用"简单单元复制+有效区域控制"。首先,建立坐标系,确定待计算剖分格网系统的种类,从而确定格网剖分类型的3个关键因素。在此基础上,确定各类多尺度格网有效控制边界。然后对多尺度格网进行合适的数学变换,计算单一三角面格网系统单元节点坐标,并建立不同层级单元节点的关联关系。最后,以六边形格网为例展开验证,直接生成正二十面体表面格网。实验结果证明,该算法具有很好的通用性,可以通过调整相应的起算参数,生成各类多尺度格网。避免了传统定制算法的局限性,实现了统一化生成各类格网系统的目标,为不同剖分类型全球离散格网系统间互操作性问题研究提供了一种解决思路。     

基于分区间泛化Kriging近似模型的船舶局部结构形状优化

为提高Kriging近似模型在船舶结构性能多维度响应预测方面的适用性,对常规Kriging近似模型进行分区间泛化改进:一是对设计样本点的各个维度(分量)进行划区,并在每一个分区间内采用最优拉丁超立方(OLhd)取样;二是引入比例系数w1组合高斯与指数型相关函数提高模型对数据的泛化能力,从而在每个划分的区间内建立泛化的Kriging近似模型。通过SCH测试函数,验证了构造的分区间泛化Kriging模型有效性。结合参数化建模和改进Kriging近似模型对某过渡肘板和舱口角隅边界进行形状优化,优化第一阶段由改进的近似模型通过多岛遗传算法得到全局初步的最优解,第二阶段在初步解的基础上缩小优化变量范围,由少量的FEM计算即可在小范围内搜寻到精确的最优设计变量。结果表明:分区间泛化Kriging近似模型在预测多维度响应时较常规Kriging模型预测精度更高;分阶段的形状优化流程在保证极小误差和缩小计算成本的情况下能够得到理想的应力分布和重量优化结果,有助于船舶结构的轻量化研究。     

江苏海岸带景观及其生态旅游的开发

海岸带是陆地、海洋生态系统相互作用的生态过渡地带,也是人类赖以生存的非常独特的景观资源。由于人口增长和对资源的不合理开发,海岸带环境遭到破坏而面临着资源枯竭的危险,保护海岸带景观异质性和生态整体性对海岸带的可持续利用显得尤为重要。江苏海岸带异质景观的形成是受自然驱动要素和干扰共同作用的结果,其影响因素主要包括江苏海岸地貌演化、气候水文条件、土壤植被条件等自然要素和台风暴潮灾害、米草引种和人类开发活动等干扰。江苏海岸带景观具有结构的复杂性、功能的多样性、生态的脆弱性、环境质量较高和高、低对比度兼有等特征。从风景地貌学和旅游开发角度考虑,将江苏海岸带景观划分为北部山海景观类、中部滩涂景观类和南部河口景观类,并在景观类的基础上进一步划分出景观亚类和景观型两个层次。提出了加强景观生态建设,维持景观的异质性,建设射阳河—新洋港流域的荷兰式国家低地生态公园和盐城国家海洋湿地生态公园,适度开发沿海自然保护区景观生态旅游,打造北部山海景观生态旅游特色项目,深入开发南部江海交汇景观,挖掘海岸带旅游景观资源的文化异质性,以及启动辐射沙洲海洋世界自然遗产的申报和建设8项生态旅游规划。     

引进种金头鲷养殖研究

2007年引进179尾金头鲷Sparusaurata放于遮阳水泥池(17.5m3)进行养殖试验,长度约3cm鱼苗,经过366d的养殖,体重平均307.9g(260.0-380.0g);全长平均25.8cm(23.5-28.2cm);体高平均8.8cm(8.2-9.5cm).成活率92.2%,饵料系数2.3.试验结果表明,该品种生长速度较快,抗病力强,适合于广西工厂化养殖.     

The application of hyperspectral remote sensing to coast environment investigation

Requirements for monitoring the coastal zone environment are first summarized. Then the application of hyperspectral remote sensing to coast environment investigation is introduced, such as the classification of coast beaches and bottom matter, target recognition, mine detection, oil spill identification and ocean color remote sensing. Finally, what is needed to follow on in application of hyperspectral remote sensing to coast environment is recommended.     

Formation and evolution of the modem warm current system in the East China Sea and the Yellow Sea since the last deglaciation

To reconstruct the formation and evolution process of the warm current system within the East China Sea (ECS) and the Yellow Sea (YS) since the last deglaciation, the paleoceangraphic records in core DGKS9603, core CSH1 and core YSDPI02, which were retrieved from the mainstream of the Kuroshio Current (KC), the edge of the modem Tsushima Warm Current (TWC) and muddy region under cold waters accreted with the Yellow Sea Warm Current (YSWC) respectively, were synthetically analyzed. The results indicate that the formation and evolution of the modem warm current system in the ECS and the YS has been accompanied by the development of the KC and impulse rising of the sea level since the last deglaciation. The influence of the KC on the Okinawa Trough had enhanced since 16 cal kyr BE and synchronously the modem TWC began to develop with the rising of sea level and finally formed at about 8.5 cal kyr BP. The KC had experienced two weakening process during the Heinrich event 1 and the Younger Drays event from 16 to 8.5 cal kyr BP. The period of 7-6 cal kyr BP was the strongest stage of the KC and the TWC since the last deglaciation. The YSWC has appeared at about 6.4 cal kyr BP. Thus,the warm current system of the ECS and the YS has ultimately formed. The weakness of the KC,indicated by the occurrence of Pulleniatina minimum event (PME) during the period from 5.3 to 2.8 cal kyr BE caused the main stream of the TWC to shift eastward to the Pacific Ocean around about 3 cal kyr BP. The process resulted in the intruding of continent shelf cold water mass with rich nutrients. Synchronously, the strength of the YSWC was relatively weak and the related cold water body was active at the early-mid stage of its appearance against the PME background, which resulted in the quick formation of muddy deposit system in the southeastern YS. The strength of the warm current system in the ECS and the YS has enhanced evidently, and approached to the modern condition gradually since 3 cal kyr BP.     

基于公平性的水环境容量分配研究——以沱江流域为例

公平与效益是容量分配的两个重要原则.在我国目前采用的水环境容量无偿分配方式下,公平原则是需遵循的首要原则,在公平的基础上追求效益.以沱江流域为对象,综合考虑涉及区域的社会、经济、自然等客观因素,筛选指标确定系数对流域容量进行分配.应用经济学中衡量收入公平的基尼系数概念,对分配结果的公平性进行评估,给出综合体现社会性、经济性和历史性的水环境容量分配方案.     

莺歌海盆地莺歌海组二段泥岩盖层封闭性综合评价

通过实测莺歌海盆地莺歌海组二段泥岩盖层的排替压力,建立了盖层排替压力与声波时差的线性关系,进而提出了利用声波时差及地震速度资料求取排替压力的方法.接着,利用测井声波时差和地震速度资料,按等效深度法确定莺歌海组二段下部泥岩盖层的超压分布.综合考虑盖层累计厚度、排替压力、剩余压力、气藏内部压力、断裂对盖层破坏程度和天然气本...