牛顿迭代法在海图与地形图坐标相互转换中的应用

根据地图投影变换原理,提出了一种新的地图投影变换方法,即牛顿迭代法。在海图与地形图之间的坐标相互转换过程中,从平面直角坐标到地理坐标的地图投影的反解变换是通过计算机迭代处理来完成的,这种方法具有变换精度高、算法收敛速度快、软件编程实现简便等优点。     

Simulation of Fully Nonlinear 3-D Numerical Wave Tank

A fully nonlinear numerical wave tank (NWT) has been simulated by use of a three-dimensional higher order bouodary element method (HOBEM) in the time domain. Within the frame of potential flow and the adoption of simply Rankine source, the resulting boundary integral equation is repeatedly solved at each time step and the fully nonlinear free surface boundary conditions are integrated with time to update its position and boundary values. A smooth technique is also adopted in order to eliminate the possible saw-tooth numerical instabilities. The incident wave at the uptank is given as theoretical wave in this paper. The outgoing waves are absorbed inside a damping zone by spatially varying artificial damping on the free surface at the wave tank end. The numerical results show that the NWT developed by these approaches has a high accuracy and good numerical stability.     

西天山松湖铁矿床磁铁矿标型特征及其对矿床成因的限定

松湖铁矿床位于新疆西天山伊犁地块东北缘阿吾拉勒成矿带西段,赋矿围岩为下石炭统大哈拉军山组安山岩及安山质火山碎屑岩.现有研究对于该矿床成因尚有争议,焦点在于是否存在矿浆(或岩浆)成因磁铁矿.据此,系统采集松湖铁矿床内各类典型矿石开展详细的磁铁矿标型特征研究,并利用LA-ICP-MS技术分析了磁铁矿的微量元素组成.结果表明...     

一个中国边缘海的风-浪-流预报系统

海洋预报是进行海上活动的安全保障,海洋预报系统技术已经成为现代海洋气象业务的技术支撑。海洋观测、数据同化、数值模拟和高性能计算机等技术的进步极大地推动着海洋业务化预报的发展。采用大气数值模式（WRF）、海洋数值模式（CROCO）和海浪数值模式（SWAN）的多模式高分辨率离线耦合方式,添加南京信息工程大学“海洋数值模拟与观测实验室”团队自主研发的一系列海洋模式参数化方案,包括浪致混合参数化方案、亚中尺度参数化方案、海山诱导混合参数化方案以及涡旋诱导的沿等密度面和跨等密度面混合参数化方案,并通过同化技术和最新的人工智能技术与观测资料相结合,构建一种面向中国边缘海的风浪流多参数耦合预报系统,用于海上风电功率的预报和其他海洋灾害预警。实际观测资料的验证表明,该预报系统能较准确地模拟海上风场、海流、海温、波浪、潮汐等海洋气象要素。同时实现了按需实时可视化全景展示。     

Microbial community changes in the digestive tract of the clam Meretrix petechialis in response to Vibrio parahaemolyticus challenge

Disease in clams frequently occurred over the last decade and has become a serious threat to the clam aquaculture industry and natural stocks.Mass clam mortality events were reported to be associated with the presence of opportunistic pathogen vibrio.However,the complexity of infection that occurs in the natural environment remains poorly understood.In this study,we smulated a natural disease outbreak by vibrio immersion infection to study the diversity and dynamics of microbiota in the digestive tract of clam Meretrix petechialis during the infection process.Dramatic changes in operational taxonomic unit richness and phylum composition of the bacterial communities were observed during pathogen invasion.In addition,we investigated the potential relationship between microbiota dynamics and host status during disease progression.Results reveal that,at the end stage of vibrio infection,interindividual variation in the digestive tract microbiota increased,as did the diff erence in individual health status.The moribund clams displayed signs of microbial community shifts to low diversity,and the microbial community was characterized by mass proliferation of a few operational taxonomic units.     

利用网格划分软件和缓坡方程计算港内波浪场

提出了一套可方便应用于波浪场计算的方法。该方法包含了准确的边界输入输出技术,简便的地形输入技术,高质量的计算网格生成以及加速查寻、排序的数据结构。应用双曲型缓坡方程计算了港湾内的波浪场,数值计算时提出了处理建筑物表面部分反射边界条件的方法。将计算结果与边界元方法的结果和实验值进行了比较,证明该方法应用于波浪场可得到较理想的结果。对大连港区内的波浪折射绕射进行了计算,表明本方法可以应用于实际港口的波浪场计算中。     

A composite numerical model for wave diffraction in a harbor with varying water depth

A composite numerical model is presented for computing the wave field in a harbor. The mild slope equation is discretized by a finite element method in the domain concerned. Out of the computational domain, the water depth is assumed to be constant. The boundary element method is applied to the outer boundary for dealing with the infinite boundary condition. Because the model satisfies strictly the infinite boundary condition, more accurate results can be obtained. The model is firstly applied to compute the wave diffraction in a narrow rectangular bay and the wave diffraction from a porous cylinder. The numerical results are compared with the analytical solution, experimental data and other numerical results. Good agreements are obtained. Then the model is applied to computing the wave diffraction in a square harbor with varying water depth. The effects of the water depth in the harbor and the incoming wave direction on the wave height distribution are discussed.     

车载导航系统的高精度定位算法

提出了一种基于联合卡尔曼滤波理论和地图匹配技术的高精度车载导航系统定位方法。该方法一方面对联合卡尔曼滤波器的结构进行简化,简化后的联合滤波器能够较好地将全球定位系统（GPS）与航位推算系统（DR）获取的空间信息进行融合,不仅较大程度地减小滤波计算量,而且避免了子滤波器间误差的互相干扰,提高了空间定位精度。另一方面提出了根据行车方向与位置匹配行车道路的技术,该技术不仅具有较好的行车道路匹配效果,而且能够对各种行车异常情况进行处理。实验证明,本文提出的方法能够较好地满足车载导航系统对空间定位方法实时性及高精度的要求。     

南海东沙深海冷泉区973-5重力柱沉积物古菌多样性

中国南海东沙一带冷泉发育,但目前国内外对深海冷泉区微生物研究甚少,特别是缺乏利用高通量测序的记录。对东沙深海冷泉区973-5站位(该站位水深约3 000 m)长约935 cm的重力岩心进行了高通量分析。结果显示:该站位微生物细胞丰度为5.3×10⁸~34.0×10⁸个/g,随深度变深而增加,其变化趋势与甲烷含量变化可对比,与粒度、有机碳的变化也具有相关性。测序结果显示,岩心中主要古菌类群是MBGB(39.9%)、C3(15.8%)以及ANME-1(12.0%),随着深度的变化群落组成有所改变。硫酸盐-甲烷界面(SMI,760 cm)上下出现了大量的MBGB和ANME-1类群,pH也不断增加,暗示了这一区域存在不断增强的甲烷厌氧氧化作用。岩心底部出现了一定量的ANME-1和ANME-2类群,暗示除了在SMI附近甲烷氧化和硫酸盐还原反应强烈,其下部可能还有水合物的分解与甲烷的上涌,为ANME类群生存提供了营养物质。与东沙海区其他站位相比,973-5站位的甲烷通量较高,但没有发现产甲烷菌,推测该区沉积物中高浓度的甲烷来源为周边浅部或深部断裂系统运移供给。     

黏土中桶式基础的宏单元模拟

本研究旨在对黏土中的桶式基础进行从完整的有限元分析到简化的宏单元的建模。首先通过有限元方法分析了在不同单调组合荷载作用下的黏土中吸力桶基础。为保证模拟结果的可靠性,采用了硬化土模型（HS）对正常固结黏土地基进行模拟。通过对比离心试验验证了使用HS模型的有限元分析的有效性,并通过径向位移试验进一步延伸到V-H-M（竖向力-水平力-弯矩）空间的破坏模式研究,并在此基础上,提出了的V-H-M空间三维破坏包络面公式。接着,应用此三维破坏包络面公式,采用亚塑性框架提出了黏土中桶式基础的宏单元设计模型。通过与试验结果的比较,验证了宏单元模型在模拟单调和循环荷载条件下桶式基础的强度与变形响应的有效性。所提的宏单元模型对于海洋岩土工程设计实践将很有帮助。