海河口地区全新世海侵层的相变与海面波动的对应关系

B_2孔揭示海河口地区全新世海侵层厚达19.2m,自下往上依次出现潮间滩、近岸浅海、前三角洲、三角洲湾、河口砂坝及河口边滩六个亚相,下部两个亚相呈海进层序,上部四个亚相呈海退层序。除河口边滩亚相底界外,其他所有亚相间的界面均为不连续面,显示海侵层为不连续沉积。研究表明该不连续沉积与海面波动有关.在全新世海侵高峰后,海面一直处于幅度不大(约1m 左右)的振荡运动状态,一次振荡波就在海岸线上留下一道贝壳堤,近5000余年来发生了5次振荡波,在海退平原中就有5道贝克堤与之对应。B_2孔海退层序中曲不连续面与贝壳堤基底侵蚀面相对应,也与振荡波的上升坡段相对应。海退层序所表现出来的海岸向海推进现象不是海面大幅度下降的反映,而主要是河口区沉积物迅速加积的结果。     

Hilbert transform and its application to modulation of capillary gravity waves

INTRODUCFIONlt is well known that the stability and interaction of nonlinear waves lead to modulations ofwavenumber and frequency, as well as arnplitude, with the frequency dePendent on bothwavenumber and arnplitude (Witham, l974; Philips, l98l ). These medulations are not justtheoretical curiossities but have important conSequences in oceanography and meteorology, aswell as naval architecture and ocean engineering (honguer-Higgins, l980).By means of Hilbert transfOrm technique, Melvill…     

Observation of Luzon Strait transport in summer 2007

A field experiment was conducted across the Luzon Strait in July 2007, and a total of 51 profiles covering variables of horizontal velocity, temperature, salinity, and pressure were collected at 11 stations. Using this observation, the volume transport through the Luzon Strait, its differences between July 2007 and October 2005, and the distribution of subtidal flow and geostrophic flow have been investigated. The net transport has a two-layer vertical structure, which is eastward both in the upper layer (<26 kg m^?3 σ₀), and in the intermediate layer (26–27.3 kg m^?3 σ₀), while it is westward in the deeper layer (>27.3 kg m^?3 σ₀), with respective values of 3.0, 4.0, and ?1.5 Sv. The net transport is eastward, and estimated to be 5.5 Sv. The distribution of the subtidal flow in the intermediate layer shows that a westward flow exists in the northern part, countered by an eastward flow existing in the southern part of the strait. This distribution is in direct contrast to the previous results obtained in October 2005, in which a westward flow occurs in the south countered by an eastward flow in the north in the intermediate layer. This suggests that the flow pattern varies greatly from October 2005 to July 2007 not only in the upper layer but also in the intermediate layer. The deep layer, on the other hand, shows few changes between the two observation periods.     

面向地质图的知识图谱构建及智能问答应用

海量地质图件蕴含着丰富的地学基础知识及专家经验知识。地质图主要表达了通过区域地质调查、矿产地质调查所获取的地球表面的地质知识（如地层单元、岩体、断裂等）。如何快速地从矢量地质图件中抽取地质知识并形成知识服务是目前地学知识图谱及知识服务研究的前沿。由于传统的地质图知识抽取主要依赖人工方式进行综合分析,本文聚焦于矢量地质图件知识表达与抽取研究,提出了一种地质图知识表达框架,提取地质图中所包含的地质实体及关系,将地质图信息以知识图谱的形式表达,并开展了基于地质矢量知识图谱的智能问答应用。最后以江西省于都县银坑幅矢量数据集为例开展实验验证分析,结果表明,本文方法能够较为全面地获取地质图中各个地质对象的信息,提高了地质图语义表达的效果,同时也可以提高地质学习人员对地质图的理解和认识,让计算机能够大规模获取地质图的知识内容。

     

Effects of Degrees of Motion Freedom on Free-Fall of A Sphere in Fluid

Free-fall of a sphere in fluid is investigated at a Galileo number of 204 by direct numerical simulations (DNS). We mainly focus on the effects of different degrees-of-freedom (DOFs) of the sphere motion during free-fall. The characteristics of free-fall are compared with those of flow past a fixed sphere. Additional numerical tests are conducted with constraints placed on the translational or rotational DOFs of the sphere motion to analyze different DOFs of sphere motion. The transverse motion contributes significantly to the characteristics of free-fall; it results in the retardation of the vortex shedding, leading to the decrease of the Strouhal number. In addition, the transversal sphere motion exhibits the tendency to promote the sphere rotation. On the contrary, the effects of the sphere rotation and vertical oscillations during free-fall are negligible.     

便携式潮汐预报仪的开发与研究

讨论了一种便携式潮汐预报仪的开发与实现。其内部集成嵌入式μC/OS-Ⅱ实时操作系统以及潮汐预报软件,能够根据用户需要实时计算待测港口的潮位信息。将预测数据与实测数据进行比对,说明本系统与传统纸质潮汐表及微机版电子潮汐预报仪相比,具有便携、使用方便、预测精度高等优点。     

可用于相关亚历山大藻(Alexandrium affine)检测的一个寡核苷酸探针

针对分离自南海的相关亚历山大藻,在进行核糖体大亚基DNA（LSU rDNA）全序列测序及比对的基础上,设计了针对其核糖体大亚基RNA（LSU rRNA）D10区的一个新的荧光素（FITC）标记寡核苷酸探针,并建立了相应的荧光原位杂交检测方法。在GenBank数据库中,BLAST检索的结果显示所设计的探针具有较高的特异性。杂交实验的结果也表明,这条探针对相关亚历山大藻的标记具有特异性,且标记效率可以达到100％,标记信号清晰明亮。本研究结果为相关亚历山大藻的监测及其种群动态研究提供了方法学依据,也为其它微藻特异性探针的设计提供了新的思路。     

西湖凹陷裂陷期构造样式及其对沉积充填的控制作用

西湖凹陷裂陷期构造主要是指从断陷开始形成(Tg界面)至始新世末(T30界面)的构造,它控制着盆内裂陷期地层的发育和沉积体系的总体展布特征.裂陷期原盆地的构造格架总体为一复杂的半地堑结构,主要受控于三组NE向的断裂带:东缘陡坡断裂带、中央洼陷断裂带、西部缓斜坡断裂带.西湖凹陷裂陷期古构造格局对裂陷期构造层序沉积、沉降中心...     

黄海冷水团附近沉积物中的趋磁细菌及磁小体的特性研究

对黄海冷水团附近海域的沉积物进行了富集、荧光显微镜观察、电镜观察,并对其中大小均匀、形状规则的高密度颗粒进行了能谱分析。结果显示,在黄海冷水团附近有趋磁细菌和磁小体的存在。