基于Flex技术的分布式地理信息系统在文物保护中的应用

通过与陕西省文物局合作,以不可移动文物中的古塔为例,利用FLEX技术建立基于B/S架构的Web地理信息系统,能够实现跨平台的文物数据存储和管理,利用自身优势为文物保护工作提供技术支持。     

测绘技术在大遗址保护中的应用

石峁遗址作为重要的考古发现具有重大的学术意义,本文利用三维激光扫描技术、无人机航摄技术、GPS技术、数字化测图技术等多种测绘技术对石峁本体及周边环境进行测量,得到了多种测绘成果,是利用多种信息化测绘技术服务于文物保护的成功应用,为以后开展同类大遗址保护项目积累了宝贵经验。     

日本九州岛地震震前电离层TEC异常

采用IGS发布的GIM数据,提出了一种结合滑动时窗法和临近格网点电离层TEC相关性分析法的联合分析方法,研究了震前电离层异常变化与地震的关系。通过分析震区附近5个格网点TEC的异常变化情况,发现震前电离层TEC发生明显异常变化,且格网点之间的TEC序列相关性受地震显著影响;通过分析二维电离层图的TEC异常空间分布,发现震前三天震中附近分别出现6h、12h和6h的异常。最后利用电离层层析的方法,对电离层异常时刻进行了电子密度的反演,进一步分析了电子密度在电离层异常时刻的分布情况。     

Studies on rickettsia-like organism(RLO)disease of tropical marine pearl oyster--Epidemiologicai investigation of RLO disease in juvenile populations of maricultured Pinctada maxima

The death which occurred in juvenile population was a severe problem in the course ofPinctada maxima artificial culture. With the methods of field investigation, histological study andstatistic analyses, the epidemiological study was carried out on the disease and death in juvenile popula-tions of Pinctada maxima in the Xinying Pearl Oyster Mariculture Farm of Lingao County (for the A,B and C batches of cultured juveniles hanged in the sea) and the Xincun Pearl Oyster Mariculture Farmof Lingshui County (for the D batch of cultured juvenile hanged in the pond), Hainan Province fromNovember 1993 to April 1995. The results show that the deaths which occurred in juvenile populations of Pinctada maxima pre-sented an outbreak pattern. The peak of mortality rates, in general, occurred in 4-to 6-month old pearloyster juveniles, and the mortality rates gradully declined with the extention of pearl oyster age after cul-turing 8 months. The correlation between the mortality rates of juvenile populations and mean bodylengths of juvenile populations show that the mortality rate become higher under 4 cm of mean bodylengths of juvenile population and become obvious declined over 5 cm of mean body lengths. The peak ofmortality rate occurred in 1 ～3 cm of mean body lengths. The results of histological observation showedthat rickettsia-like organism inclusions were common, histological widespread infective agent among ev-ery batches (A, B, C and D) of cultured juvenile populations. The mean severity indices (SI) of rick-ettsia-like organism (RLO) infection were positively correlated with mortality rates of juvenile popula-tions. After or within every peaks of RLO infection were all accompanied with the peaks of mortalityrates of host populations and the mortality rates declined with decreased RLO infection. So the evidencesof histological observation and epidemiology in this study indicated that rickettsia-like organism (RLO)may be as an important pathogenic organism of disease and death of cultured Pinctada maxima. In addi-tion, a few ciliates were discovered only in part of batch A of cultured juvenile population. The mortalityrates in juvenile populations were not correlated with the weekly mean temperature and salinity of seawater.     

刺激隐核虫生活史的光镜观察

本文对寄生于海水硬骨鱼体表组织的纤毛虫刺激隐核虫(Cryptocaryonirritans)的生活史进行了描述。该寄生虫生活史分3个阶段,即滋养体,包囊体和幼虫。滋养体主要营寄生生活。成熟的滋养体离开宿主后,在数小时内就发育成包囊体。包囊体的特点是具多层结构的囊壁,而且此阶段虫体的繁殖方式为不等分裂。每个成熟的包囊平均可形成273±64个幼虫。由于囊壁坚硬,幼虫游离后,包囊壁仍保持原样。进入水体的幼虫游动极快,不摄食,一旦遇到合适的宿主即侵入,并在宿主体内发育成滋养体。文中还将结果与淡水多子小瓜虫生活史进行了比较。     

云南莲峰、昭通—鲁甸断裂带面积—高程积分的构造地貌研究

笔者等基于ASTER GDEM数据,提取莲峰、昭通—鲁甸断裂带集水区,计算该区亚流域盆地的面积—高程积分值,并结合野外剖面特征、历史地震、断裂构造特征及活动特征等,初步探讨了莲峰、昭通—鲁甸断裂带的构造地貌特征及其动力学机制。得到以下几点认识：(1)研究区除鲁甸盆地外,大部分地区的地貌发育阶段为壮年期;(2)研究区面积—高程积分值(HI)主要受控于构造活动,岩性的抗侵蚀性和水系侵蚀发挥局部或次要作用;(3)面积—高程积分值(HI)对研究区不同构造抬升强度地区的响应方式不同：构造强烈抬升区,HI值反映了集水流域受到强烈的构造抬升和侵蚀的共同作用;构造抬升减弱区,HI值反映了缓慢的构造隆升和沉积作用的共同结果。     

东北那丹哈达岭中—新生代构造-热演化史:来自(U-Th)/He和裂变径迹热年代学的证据

中国东北的那丹哈达岭地区位于中亚造山带最东部,它的中新生代热演化史是认识陆内造山活动的关键,但该地区相关研究比较薄弱,其中—新生代的热演化史缺乏有效的约束.因此本文应用磷灰石裂变径迹、锆石和磷灰石(U-Th)/He等多种低温热年代学方法,对东北那丹哈达岭地区的侵入岩开展构造热演化历史研究.热年代学数据和热史模拟结果表明,该地区存在早白垩世晚期—晚白垩世(110～80Ma)、古新世—始新世(60～40 Ma)两期快速冷却事件,其冷却速率分别为3.42～4.81℃/Ma和1.43～1.83℃/Ma.结合区域构造和应力分析,我们认为两期冷却事件均受构造活动控制.第一期快速冷却事件是古太平洋板块北西向俯冲引发的构造叠加到鄂霍特莫茨克地块并与东亚大陆边缘碰撞引起;而第二期快速冷却事件是古太平洋俯冲的板片后撤使东亚陆缘处于伸展环境,造成东北大面积的剥露作用引起.这次研究增强了对东亚陆缘中新生代构造-热演化历史的认识,对于理解大陆内部造山带的构造变形过程与机理具有重要意义.     

云南宣威煤矿开发遥感调查研究

以2010年获取的WorldView -2遥感图像为主要数据源,以GIS平台为支撑,对云南宣威市(羊场、东山、海岱、田坝)煤矿矿山进行调查;结合野外实地查证及研究区矿权数据和地质资料,系统建立了煤矿矿山遥感解译标志,对矿山开采情况进行解译.结果表明,研究区内煤矿矿山硐口分布明显受含煤地层及断层限制,硐口越界现象较为普遍.建议矿政管理部门充分考虑矿区地形、地质条件,针对硐口越界矿山,变更采矿权范围,促进矿业秩序全面好转.     

数传通道遥测数据处理方法研究

天绘卫星在轨运行期间, 星务数据存储模块负责存储整星遥测数据, 并协同相机数据通过数传通道传到地面。本文根据数传通道遥测数据的格式, 提出一种处理遥测数据的方法, 该方法从地面站接收数传通道下传数据, 提取出整颗星遥测数据, 并通过电气地面支持设备对在轨遥测数据进行处理, 便于后期对整星遥测数据的分析。     

Summer Asian-Pacific Oscillation and Its Relationship with Atmospheric Circulation and Monsoon Rainfall

Using the ERA-40 data and numerical simulations, this study investigated the teleconnection over the extratropical Asian-Pacific region and its relationship with the Asian monsoon rainfall and the climatological characteristics of tropical cyclones over the western North Pacific, and analyzed impacts of the Tibetan Plateau （TP） heating and Pacific sea surface temperature （SST） on the teleconnection. The Asian-Pacific oscillation （APO） is defined as a zonal seesaw of the tropospheric temperature in the midlatitudes of the Asian-Pacific region. When the troposphere is cooling in the midlatitudes of the Asian continent, it is warming in the midlatitudes of the central and eastern North Pacific; and vice versa. The APO also appears in the stratosphere, but with a reversed phase. Used as an index of the thermal contrast between Asia and the North Pacific, it provides a new way to explore interactions between the Asian and Pacific atmospheric circulations. The APO index exhibits the interannual and interdecadal variability. It shows a downward trend during 1958-2001, indicating a weakening of the thermal contrast, and shows a 5.5-yr oscillation period. The formation of the APO is associated with the zonal vertical circulation caused by a difference in the solar radiative heating between the Asian continent and the North Pacific. The numerical simulations further reveal that the summer TP heating enhances the local tropospheric temperature and upward motion, and then strengthens downward motion and decreases the tropospheric temperature over the central and eastern North Pacific. This leads to the formation of the APO. The Pacific decadal oscillation and El Nino/La Nina over the tropical eastern Pacific do not exert strong influences on the APO. When there is an anomaly in the summer APO, the South Asian high, the westerly jet over Eurasia, the tropical easterly jet over South Asia, and the subtropical high over the North Pacific change significantly, with anomalous Asian monsoon rainfall and tropical cyclon