基于多尺度的Canny边缘检测算法研究

为了解决传统边缘检测算法检测精度不高、稳健性不好和抗噪能力差等弱点,文章提出了一种基于多尺度的Canny边缘检测算法,该算法充分利用了小尺度影像和大尺度影像的优点,既能检测出图像边缘的整体轮廓,又能检测出图像细节。并运用MATLAB编程与几种经典边缘检测算法做了详细对比,采用ROC曲线进行了精度定量评价分析。实验结果表明,基于多尺度的Canny边缘检测算法检测结果更清晰,稳健性更好,而且抗高斯噪声能力也相当理想,能够有效地提取图像边缘信息。     

海底MT信号采集电路的设计

设计海底大地电磁信号采集电路，需考虑海底信号特征、海上作业以及海底环境等各种因素。分析表明，除遵循电路设计的一般原则外，海底大地电磁测量要重点解决微弱信号检测、智能化数据采集、海底环境监测和同步记录等4个方面的问题。在设计方案中，电路灵敏度达到微伏级；使用嵌入式计算机实现采集控制；对方位、倾斜、振动、温度等参数进行巡回记录；仪器的时钟精度精准到微秒。所研制的电路经过了室内模拟测试和海洋试验。首次采集到中国海域的大地电磁数据。     

胜利油田火山岩辉石中岩浆包裹体成分及有关成因问题

对胜利油田火山岩中辉石及其中岩浆包裹体成分的研究表明：ＣＯ２气藏区和非ＣＯ２气藏区新生代火山岩辉石及其中岩浆包裹体成分有明显区别,前者中辉石为普通辉石,成分相对富ＳｉＯ２,而贫Ａｌ２Ｏ３、ＴｉＯ２、ＭｇＯ和挥发成分;而后者中辉石为透辉石,成分相对贫ＳｉＯ２和挥发份,而富Ａｌ２Ｏ３、ＴｉＯ２和ＭｇＯ。前者岩浆包裹体玻相中富含ＣＯ２,包裹体中的金属子矿物多为黄铁矿;而后者岩浆包裹体玻相中贫ＣＯ２;包裹     

台湾海峡西部柱状沉积物粘土矿物的分析

根据台湾海峡西部10个柱102个样品的X 射线衍射等分析,鉴定了该区粘土矿物组合与含量变化,分析了其与沉积环境的关系.结果表明,该区粘土矿物组合大多数站位以伊利石含量占首位,绿泥石和高岭石次之,且含少量蒙脱石;伊利石含量随距岸、水深的增加而递增,高岭石则反之;蒙脱石含量与火山活动密切相关,绿泥石含量呈斑块状分布;775和819号站有典型的陆相层,为早玉木冰期的“台湾陆桥”或“东山陆桥”提供有力证据.     

灾害天气国家重点实验室成功举办数值预报系统理论高级讲座

为了使数值预报中心的研究人员和研究生能够了解数值预报的历史、发展以及现今研究的最前沿，灾害天气国家重点实验室数值预报研究部2006年底举行了“数值预报理论基础”系列讲座。讲座每星期两次，邀请了我国在数值模式方面做出突出成绩和贡献的老专家，如中科院大气物理所的纪立人、陈嘉滨先生，从数值预报的基础公式和数值解法，一直到国内外的最新研究成果进行了完整的介绍。     

超声波对湛江等鞭金藻生长和脂肪酸组成的影响

设计了一个超声频率、超声功率和处理时间三因素四水平的正交实验,研究了超声波对湛江等鞭金藻的生物学效应.实验结果表明,超声频率对湛江等鞭金藻的生物学效应显著,而超声功率和处理时间的影响相对较小.对于提高湛江等鞭金藻生长速率常数,最佳超声条件为20kHz,6W,10s3次;对于提高其脂肪酸不饱和度和主要不饱和脂肪酸百分比,最佳超声条件为20kHz,4～6W,30s.在最佳超声条件下,湛江等鞭金藻生长速率常数最高可达0.630d,是对照组的2.02倍,其脂肪酸不饱和度最高可达79.6%,比对照组提高7.8%,其中主要不饱和脂肪酸的百分含量均得到不同程度的提高.     

An Review of International Climate Change Conference and Analysis on Recent Hot Issues

The international climate change negotiation has been carried out over 20 years. The issue of climate change has shifted from a scientific question into a complex political matter which is related to the sustainable development of mankind. Based on the overview of major processes and stages of international climate conferences, this paper analyzed the key measures that major countries have taken to address climate change, as well as the primary tasks of Paris climate conference and recent international actions. The recent international climate policy issues were also analyzed in order to provide suggestions for China’s activel participation in the development of a new round of international climate change system.     

云南省雷灾特征分析及灾情评估

根据云南省2007 2008年的雷电灾害资料以及地闪资料,分析了云南省16个地级市的雷电灾害分布特征,讨论了雷灾分布与地闪分布的关系,并从雷灾记录中提取了6个灾度指标,通过AHP法(层次分析法)建立灾情评估层次模型和灾度评估方程,计算了云南省522次雷灾的灾度值,用SAS中聚类分析过程将灾度值分为4级,并统计分析了各级雷灾在各地区的分布情况,得出云南雷电灾害中小型雷灾分布较广、出现几率较大,而大型和特大型雷灾发生几率较低、主要集中在昆明和德宏地区.该文结论为区域防雷减灾规划提供了科学依据.     

Interactive Effects of Ultraviolet Radiation and Dissolved Organic Carbon on Phytoplankton Growth and Photosynthesis in Sanya Bay,Northern South China Sea

Ocean Science Journal - The effects of a simulated climate change scenario, i.e., increased ultraviolet radiation (UVR) and dissolved organic carbon (DOC), on the growth and photosynthesis of...     

The influence of hydrocarbon expulsion on carbon isotopic compositions of individual n-alkanes in pyrolysates of selected terrestrial kerogens

Expulsion of petroleum from source rock is a complex part of the entire migration process. There exist fractional effects on chemical compositions in hydrocarbon expulsion. Does the carbon isotopic fractionation occur during expulsion and to what extent? Here the influence of hydrocarbon expulsion on carbon isotopic compositions of individual n-alkanes from pyrolysates of selected terrestrial kerogens from Tuha basin and Fushun, Liaoning Province of China has been experimentally studied. The pyrogeneration-expulsion experiments were carried out under semi-closed system. The carbon isotopic compositions of individual n-alkanes were measured by GC-IRMS. The main conclusions are as follows. First, there is carbon isotopic fractionation associated with hydrocarbon expulsion from Type III kerogens in Tuha Basin. There exist differences of carbon isotopic compositions between the unexpelled n-alkanes and expelled n-alkanes from Tuha desmocollinite and Tuha mudstone. Second, there is almost no carbon isotopic fractionation associated with hydrocarbon expulsion from Type II kerogens in Fushun and Liaohe Basin. Third, carbon isotopic fractionation in hydrocarbon expulsion should be considered in making oil-source correlation of Type III kerogens at least in the Tuha Basin. Further studies need to be carried out to determine whether this is true in other basins. Fourth, oil and source at different maturity levels cannot be correlated directly for Type III kerogens since the carbon isotopic compositions of expelled hydrocarbons at different temperatures are different. The expelled hydrocarbons are usually lighter (depleted in ¹³C) than the hydrocarbons remaining in the source rock at the same maturity.