象山港分区水交换数值研究

在验证良好的三维斜压潮流数学模型的基础上,将象山港划分成7个海区,以7种不同的溶解态保守性物质为示踪剂,建立对流-扩散型的海湾水交换数值模型,采用关联矩阵法来描述各区之间以及各区与外海之间的水交换特性。通过不同示踪剂的浓度分布,计算了15、30、45、60和80d的水交换矩阵。由各时刻水交换矩阵可知,在象山港的7个子区中与湾外水的水交换速度最快的为Ⅰ区,最慢的为Ⅶ区。Ⅲ区(西沪港)、Ⅵ区(黄墩港)和Ⅶ区(铁港)内水体与湾外海水之间的水交换速度缓慢,但与区域外水体之间的交换速度要明显快于其他几个海区。从水交换矩阵可以看出西沪港、黄墩港和3个内港之间相互交换的海水量很小。     

潜器在冲击载荷下的运动和控制研究

潜器在水下发射火箭时会产生复杂的运动变化,对其研究很有实际意义。参照格特勒运动方程,建立潜器运动的非线性数学模型。导入实验模型的参数,对其六自由度基本运动进行了仿真,并与水池实验结果相比较,验证了仿真模型的有效性。导入发射火箭时潜器受到的完整载荷,计算分析了不同航速下潜器的运动响应和运动控制。结果表明,发射载荷对潜器运动将产生较长时间的显著影响,包括速度损失、升沉运动和纵倾角振荡。航速越小,运动变化越大,恢复所需时间越长,控制越困难。     

Selected trace metals (As,Cd and Hg) distribution and contamination in the coastal wetland sediment of the northern Beibu Gulf,South China Sea

Contamination with As, Cd and Hg, their spatial and temporal distribution are reported from the coastal wetland sediments of the northern Beibu Gulf, South China Sea. The content of As, Cd, Hg and TOC in surface sediments is 8.1 ± 5.8 μg g^?1, 0.08 ± 0.14 μg g^?1, 0.034 ± 0.028 μg g^?1 and 0.45 ± 0.39%, respectively. The mean sedimentation rates are 0.93–1.37 cm year^?1 during 1920s to 2008 determined by ²¹⁰Pb and ¹³⁷Cs dating in three cores. The vertical profiles of As, Cd and Hg content in the cores retrieved from Qin and Nanliu River estuaries show increasing trends during 1985–2008 due to anthropogenic impact caused by local economic development. Locally the surface sediments have potential ecological risk of As to benthos according to the NOAA sediment quality guidelines.     

PANDA和BERNESE软件的PPP比较分析

分析了PANDA和BERNESE软件的精密单点定位方法及解算策略上的差异。采用IGS站BJFS站2007年年积日7～13-周的观测数据,分别利用PANDA和BERNESE软件PPP模块进行解算,求得2h松弛解和单历元解,并对解算结果进行比较分析。结果显示：在解算方案相同的情况下,PANDA的解算结果与BERNESE能很好的符合,存在毫米级的差异,表明PANDA软件具有很高的稳定性及可靠性。     

Electronic chart display and information system

This paper introduces the most advanced form of electronic chart display and information systems (ECDIS) which complies with the Performance Standards for ECDIS established by the International Maritime Organization (IMO) and the International Hydrographic Organization (IHO). It also describes the key features and the important functions of ECDIS. Then the future development of ECDIS in marine is discussed.     

辽宁省经济与生态环境系统耦合发展分析

基于区域经济与生态环境系统的发展速度,选取24个评价指标,利用耦合度模型并结合剪刀差分析评价辽宁省1996-2011年经济系统与生态环境系统的耦合发展,分析耦合度发展趋势及系统发展速度的差异性.结果表明:经济发展速度呈“U”型,而生态环境系统呈倒“U”型,二者耦合度发展呈“U”型,先后经历了发达型—协调发展型—发达型—过度发展型几个不同耦合度阶段,1996-2002年经济与生态环境系统发展耦合程度较高,2003-2011年发展趋势逐渐远离和谐;剪刀差显示经济系统与生态环境系统速度差异发展过程呈“U”型,2001年差异度最小,2002-2011年差异度值逐年加大,经济与生态环境系统发展速度有显著差异性,二者的发展速度并不协调同步.     

青藏高原东缘重力观测及对芦山M7.0地震的反映

介绍了青藏高原东缘地区相对重力与绝对重力的观测情况,系统分析了该区域2010以来的区域重力场变化及其与2013年4月20日四川芦山7.0级地震发生的关系。结果表明:(1)芦山7.0级地震前青藏高原东缘重力变化剧烈,芦山地震发生在沿龙门山断裂带南段的重力变化高梯度带的转弯部位;(2)芦山地震距2008年汶川地震不到100km,芦山震中及汶川地震震中均处于重力变化四象限中心,表明汶川地震震后恢复调整变化对芦山地震具有促进作用;(3)基于流动重力异常变化在芦山7.0级地震前做过一定程度的中期预测,尤其是地点预测。     

Gravity observations along the eastern margin of the Tibetan Plateau and an application to the Lushan Ms7.0 earthquake

This paper introduces relative and absolute gravity change observations in the eastern portion of the Tibetan Plateau. We analyze and discuss a change that occurred in 2010 in the gravity along the eastern margin of the plateau and the relationship between this change and the 2013 Lushan Ms7.0 earthquake. Our results show that： （1） before the Lushan MsT.0 earthquake, gravity anomalies along the eastern margin of the Tibetan Plateau changed drastically. The Lushan earthquake occurred at the bend of the high gradient zone of gravity var- iation along the southern edge of the Longmenshan fault zone. （2） The 2013 Lushan earthquake occurred less than 100 km away from the epicenter of the 2008 Wenchuan earthquake. Lushan and Wenchuan are located at the center of a four- quadrant section with different gravity anomalies, which may suggest that restoration after the Wenchuan earthquake may have played a role in causing the Lushan earthquake. （3） A medium-term prediction based on changes in gravity anoma- lies was made before the Lushan Ms7.0 earthquake, in par- ticular, a prediction of epicenter location.     

The Calculation of Solar Gamma-Rays by TALYS

Solar gamma-ray lines, produced from nuclear reactions of accelerated particles interacting with the solar atmospheric medium, are the most direct diagnosis for the acceleration and transportation of energetic electrons and ions in solar flares. Much information about composition, spectrum, and angular distribution of the accelerated ions, as well as the elemental abundances of the ambient solar atmosphere can be derived from solar gamma-ray line spectra. A new gamma-ray calculation program has been developed by using an efficient nuclear code − TALYS. The theory of gamma-ray production in solar flares is treated in detail. The characteristics of gamma-ray spectrum are also presented.     

黔西南者相二金矿龙潭组沉积特征与金富集规律研究

本文利用岩心、样品分析化验等资料对龙潭组的沉积环境、岩性组合、隐伏断裂构造以及含矿特征进行了研究,结果表明:研究区龙潭组为陆表海局限台地、潮控三角洲以及重力流沉积。区内存在两条隐伏断裂,走向为北西向,倾向北东的逆断层(F_(20))和走向为北东向,倾向北西的逆断层(F_x);龙潭组一段(P_3l~1)零星含矿段、龙潭组二段(P_3l~2)Ⅲc～Ⅲb含矿层、龙潭组三段(P_3l~3)的Ⅳc～Ⅳb含矿层具滑动擦痕、滑动镜面、碎裂化和角砾化特征,含矿层中的生物碎屑灰岩和粉砂质粘土岩、粘土质粉砂岩和钙质粘土岩,均有不同程度的见矿,是金富集的有利场所,为后期找矿预测方向提供了依据。