地质条件复杂地区瑞雷波勘探正演模拟

为研究复杂地质条件对瑞雷面波频散曲线的影响,采用有限差分地震数值模拟方法,对3种模型进行正演模拟,得出了某一时刻的波场快照与单炮记录。对模拟记录进行频散分析的结果表明：单层均匀介质没有频散现象;起伏地表两层均匀介质的频散曲线相速度只和介质本身的参数有关,不受地形的影响;水平地表含软夹层介质中,瑞雷波频散现象非常明显。     

基于BSA及固定碘速率探讨不同浓度对比剂对肝静脉CT成像效果的影响

目的：探讨基于体表面积（BSA）和固定碘速率给药,不同浓度对比剂对CT肝静脉成像质量的影响。方法：选取2020年1月至11月符合纳入标准,行上腹部增强CT扫描的患者130例,根据所用对比剂浓度不同,分为高浓度组（62例）和低浓度组（68例）,高浓度组对比剂为碘帕醇（含碘370mg/mL）,低浓度组对比剂为碘佛醇（含碘320mg/mL）;根据BSA计算患者所用对比剂的总量,固定碘速率注射,进行分期动态扫描。选取肝静脉期数据行肝静脉血管重建,对图像质量进行评价,测量两组图像肝静脉和肝实质的CT值及其标准差值,计算信噪比和对比噪声比,并对图像质量进行主观评分;采用独立样本t检验比较两组间客观评价指标的差异,采用Mann-Whitney U检验比较主观评分的差异。结果：高、低浓度组图像评分分别为（3.74±0.47）分和（3.77±0.53）分,差异无统计学意义;两组间肝静脉左、中、右三支主干和同层面肝实质的CT值、SD值、SNR及肝静脉相对于肝实质的CNR,差异无统计学意义。结论：基于BSA及固定碘速率注射对比剂,两种不同浓度对比剂在肝静脉CT成像中的效果同样清晰利于诊断。     

中层大气中重力波饱和机制的数值分析

通过对向上传播的重力波波包在中层大气中的非线性传播过程进行数值模拟,讨论中层大气中重力波的饱和机制.数值模拟结果表明,向上传播的重力波波包的扰动振幅在接近波包的本征水平相速度之前随高度单调增长,而当波振幅接近本征水平相速度时,在对流不稳定区域出现等位温面的翻转,同时波振幅的增长达到饱和（波振幅随高度不发生变化）.小尺度对流在等位温面的翻转和波饱和发生后产生,随后波包开始破碎,这些非线性过程的最终结果产生湍流.表明导致重力波饱和的关键因素是等位温面的翻转而不是诸如波破碎、湍流、波-流相互作用等其他的一些物理过程.     

土壤天然热释光法在相山火山岩型铀矿床中的应用

介绍了天然热释光法在火山岩铀矿床上的应用效果,表明矿体上方热释光异常较大,无矿区域异常较小,矿体的分布范围与高值异常范围一致,还发现在一些构造薄弱带,裂隙、断层处出现大的异常,试验证明土壤天然热释光测量可以为评价火山岩铀资源提供线索。     

高访问量的“SARS网络地理信息系统”解决方案

介绍了高访问量条件下“SARS网络地理信息系统”解决方案,指出瘦服务器模式是研制具有高访问量特点的网络地理信息系统的最佳解决方案。     

INFLUENCE OF THE SURFACE AIR TEMPERATURE OVER ASIAN-PACIFIC REGION ON THE SUMMERTIME NORTHEASTERN ASIAN BLOCKING HIGH*

Synthesis analysis and singular value decomposition (SVD) methods were used to study the impact of surface air temperature (SAT) over Asian-Pacific region on the summertime northeastern Asian blocking high (NABH) with NCEP/NCAR Reanalysis Data.The results showed that 500 hPa geopotential height and SAT fields over Asian-Pacific region shared the similar pattern of East Asian Pacific (EAP) wave train;there was steady remote response relationship between the EAP wave train in summer and the "+-+" pattern of tropical SAT in zonal direction from former winter to summer;there were two relative negative(positive) Walker circulations over the tropical Indian Ocean and Pacific when being more(less) summertime NABH. The influence of sea surface temperature anomaly (SSTA) on the summertime NABH was possibly as follows.The special distribution of SSTA in tropical zonal direction continuously forced the tropical convection and zonal circulation from former winter to summer,and led them to act anomaly.Finally the abnormal conditions were transported to middle-high latitudes through EAP wave train and yielded the advantageous or disadvantageous atmospheric circulation background for the summertime NABH.     

Timing of Magma Mixing in the Gangdisě Magmatic Belt during the India-Asia Collision： Zircon SHRIMP U-Pb Dating

Abstract  Abundant mafic microgranular enclaves (MMEs) extensively distribute in granitoids in the Gangdisê giant magmatic belt, within which the Qüxü batholith is the most typical MME‐bearing pluton. Systematic sampling for granodioritic host rock, mafic microgranular enclaves and gabbro nearby at two locations in the Qüxü batholith, and subsequent zircon SHRIMP II U‐Pb dating have been conducted. Two sets of isotopic ages for granodioritic host rock, mafic microgranular enclaves and gabbro are 50.4±1.3 Ma, 51.2±1.1 Ma, 47.0±1 Ma and 49.3±1.7 Ma, 48.9±1.1 Ma, 49.9±1.7 Ma, respectively. It thus rules out the possibilities of mafic microgranular enclaves being refractory residues after partial melting of magma source region, or being xenoliths of country rocks or later intrusions. Therefore, it is believed that the three types of rocks mentioned above likely formed in the same magmatic event, i.e., they formed by magma mixing in the Eocene (c. 50 Ma). Compositionally, granitoid host rocks incline towards acidic end member involved in magma mixing, gabbros are akin to basic end member and mafic microgranular enclaves are the incompletely mixed basic magma clots trapped in acidic magma. The isotopic dating also suggested that huge‐scale magma mixing in the Gangdisê belt took place 15–20 million years after the initiation of the India‐Asia continental collision, genetically related to the underplating of subduction‐collision‐induced basic magma at the base of the continental crust. Underplating and magma mixing were likely the main process of mass‐energy exchange between the mantle and the crust during the continental collision, and greatly contributed to the accretion of the continental crust, the evolution of the lithosphere and related mineralization beneath the portion of the Tibetan Plateau to the north of the collision zone.     

基于区域特征的小波差值变化检测方法

小波变换在图像处理与分析方面的应用已取得很大的成功,如基于小波变换的图像编码、去噪、融合等,但在多时相的遥感影像变化检测方面的研究还很少.提出并实验了一种基于区域特征的小波差值变化检测方法,该方法对于高分辨率的遥感影像具有较好的检测效果,同时提高了运算速度.实验结果表明了该方法的可行性和有效性.     

美国德克萨斯州人工鱼礁建设及对我国的启示

文章对美国德克萨斯州墨西哥湾海域人工鱼礁建设情况进行介绍,从目的、计划、分布、效益、管理等方面进行分析,通过查阅相关资料,吸取美国人工鱼礁建设过程中管理、技术等方面的经验,对我国人工鱼礁建设提出参考建议。人工鱼礁建设是一项系统工程,需要全方位、多方面地开展工作,应重点从政府机构协调运作、法律体系建设、加大科研投入、完善管理措施、有效利用新型材料等方面入手,积极有效地进行人工鱼礁建设和管理。     

滨海新区温带风暴潮灾害风险评估研究

建立了一套基于非结构三角网、适用于滨海新区的高分辨率风暴潮漫滩数值模式,在陆地区域分辨率达到50~80 m,对两次典型的温带风暴潮进行模拟得到满意结果。计算了塘沽站19 a平均天文高潮值并根据对历史天气过程的分析,选取制定了4个强度的天气系统,而后模拟得到不同强度下滨海新区的温带风暴潮最大淹没范围。综合考虑风暴潮淹没风险与承灾体脆弱性制作出滨海新区温带风暴潮灾害风险图。结果表明:大部分地区都存在风暴潮灾害风险,沿海地区风险大于内陆,其中天津新港、临港工业区、海河北岸地区、大港地区南部的灾害风险最大。