基于组件模型技术的地磁数据干扰抑制系统     

谢凡  滕云田  徐沁 《地震地磁观测与研究》2012,33(2):152-158

地磁观测数据中的人工干扰抑制等预处理工作需要一套高效、便捷、交互性好的预处理系统.将基于Matlab的核心干扰识别和抑制算法以组件对象技术的形式提供给其他编程语言调用,在系统架构上采用Windows DNA架构,在界面的开发上采用微软成熟的MFC架构.同时,给出系统架构模型及关键技术实现.该系统在实际应用中取得良好效果.  相似文献   

对称性与西藏南部Ms≥6.6级地震趋势判断     

张玲玲  董婕  延军平  王腾 《高原地震》2012,24(3):1-5

在掌握西藏南部(26°～32°N,78°～98°E)19次历史地震数据后,从时间对称性方面研究该区域历史地震发生规律,分析未来地震发生的可能时间,从而为西藏地震灾害的监测提供一定的依据。从三元、四元和五元可公度信息提取法和蝴蝶结构法进行分析,得出未来10年内,西藏南部Ms≥6.6级地震的信号在2012年、2013年和2015年较强,有发生6.6级以上地震的可能。  相似文献   

绝对重力仪测量结果的振动划线处理方法初步研究   总被引：2，自引：0，他引：2       下载免费PDF全文

龙剑锋  黄大伦  滕云田  吴琼  郭欣 《地震学报》2012,34(6):865-872

针对自主研发的高精度绝对重力仪样机测量结果中引入的振动误差, 提出了一种全新的振动抑制算法．本算法利用一簇斜率相同的平行直线与记录到的参考棱镜振动曲线相交, 通过提取这些交点的时间信息, 确定落体下落轨迹上进行重力加速度计算的时间和位移坐标． 然后, 利用最小二乘算法获取测点的绝对重力加速度值．对不同重力加速度值的适用性和不同类型振动干扰的抑制效果模拟计算发现, 对于优势频率大于0.2 Hz, 峰峰值小于500 counts的干扰, 算法可以有效提高测量结果的系统偏差和测量精度．最后, 实际实验样机的测量结果表明, 本算法使最终测量精度提高了一倍, 为绝对重力仪的小型化和流动测量提供了软件技术支持。   相似文献   

Coupled dynamic analysis for wave interaction with a truss spar and its mooring line/riser system in time domain     

M. Yang  B. Teng  D. Ning  Z. Shi 《Ocean Engineering》2012

A full time-domain analysis program is developed for the coupled dynamic analysis of offshore structures. For the hydrodynamic loads, a time domain second order method is developed. In this approach, Taylor series expansions are applied to the body surface and free-surface boundary conditions, and the Stokes perturbation procedure is then used to establish the corresponding boundary value problems with time-independent boundaries. A higher-order boundary element method (HOBEM) is developed to calculate the velocity potential of the resulting flow field at each time step. The free-surface boundary condition is satisfied to the second order by fourth order Adams–Bashforth–Moultn method. An artificial damping layer is adopted on the free surface to avoid the wave reflection. The mooring-line/tendon/riser dynamics are based on the rod theory and the finite element method (FEM), with the governing equations described in a global coordinate system. In the coupled dynamic analysis, the motion equation for the hull and dynamic equations for mooring-lines/tendons/risers are solved simultaneously using the Newmark method. The coupled analysis program is applied for a truss Spar motion response simulation. Numerical results including motions and tensions at the top of mooring-lines/risers are presented, and some significant conclusions are derived.  相似文献   

Response of Water Quality and Macroinvertebrate to Landscape at Multiple Lateral Spatial Scales in the Sha River Basin,China          下载免费PDF全文

Teng Wen  Sheng Sheng  Chi Xu  Delin Xu  Yun Wan  Shuqing An 《洁净——土壤、空气、水》2015,43(3):341-350

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重庆北碚和平水库剖面下侏罗统大安寨段湖相碳酸盐岩岩石类型及沉积环境   总被引：1，自引：1，他引：0       下载免费PDF全文

施开兰  陈芳文  段卓  罗思聪苏成鹏  马腾  唐浩  谭秀成 《古地理学报》2015,17(2):198-212

四川盆地下侏罗统自流井组大安寨段一直是四川盆地致密油勘探的重要层位之一。针对该层位的研究已逾半个世纪,但岩石类型分类粗略、沉积环境及储集岩类型认识不清等问题是导致该层段致密油勘探未获重大突破的重要原因。鉴于此,笔者等开展了对四川盆地东部重庆北碚和平水库剖面下侏罗统自流井组大安寨段湖相碳酸盐岩岩石类型及沉积环境的研究。研究发现,该剖面大安寨段为湖相碎屑岩与碳酸盐岩的混合沉积,由5大类岩石组成,可细分为14种岩石类型。碳酸盐岩厚度占剖面总厚度的60％以上,以泥晶灰岩为主,介壳灰岩和介屑灰岩次之;在纵向上形成了4个较为典型的向上变浅沉积序列。根据各岩石类型宏观、微观沉积特征及岩石纵向组合形式,进一步分析了各岩石类型的沉积环境,结果表明,北碚地区下侏罗统大安寨段沉积时期为滨、浅湖环境,以低能碳酸盐沉积为主;高能与较低能环境成因的介壳滩并非碳酸盐沉积的主体。湖泊进入碳酸盐沉积阶段和钙质骨壳生物的大量繁育是大安寨期湖相碳酸盐岩形成的主要原因。结晶介屑灰岩和泥晶白云岩可能是川东地区致密油的储集岩类,在今后的勘探中,应提高对滨浅湖环境、易受大气淡水改造的岩石类型的重视程度。  相似文献   

四川盆地南部中二叠统茅口组碳酸盐岩岩溶特征:古大陆环境下层控型早成岩期岩溶实例   总被引：1，自引：0，他引：1       下载免费PDF全文

肖笛  谭秀成  郗爱华  刘宏  山述娇  夏吉文  程遥  连承波 《古地理学报》2015,17(4):457-476

综合钻井、录井、岩心、薄片等资料,研究四川盆地南部中二叠统茅口组碳酸盐岩的岩溶特征,并分析讨论其机理与模式。茅口组为开阔海台地沉积,以发育高能滩相颗粒灰岩与非滩相低能泥晶灰岩的不等厚互层为特征。岩溶主要发育在茅口组上部,表现为大量溶蚀缝洞发育,且多被离解的碳酸盐岩碎屑、方解石晶粒、碳质泥屑等不同来源的物质混合充填,但缺乏典型的岩溶角砾。茅口组岩溶属于大陆环境下早成岩期岩溶类型,一个显著特征是岩性与岩相对溶蚀-充填作用的控制:非滩相泥晶岩类岩性致密,岩溶欠发育;高能滩相颗粒岩类岩溶发育良好,并可以识别出基岩带、半离解带和混合充填带3种溶蚀-充填带。根据上述特征,认为泥晶灰岩致密层与颗粒灰岩高渗层在纵向上的多旋回叠置,以及先期的孔渗系统和断裂裂缝体系为岩溶水提供输导体系,导致形成了同期多层的颗粒滩相控岩溶系统,并在岩溶台地和斜坡岩溶型储集层皆较发育。该研究成果不仅可为相关研究提供补充与参考,还对研究区茅口组油气勘探具有一定的指导意义。  相似文献   

基于拟准检定的实时单站GPS提取同震速度的改进算法研究          下载免费PDF全文

刘腾  欧吉坤  袁运斌 《地球物理学报》2014,57(8):2507-2517

提出了一种基于拟准检定的实时单站GPS载波相位观测数据历元间差分提取同震速度的改进算法.改进算法将实时高频历元差分数据质量控制作为同震速度准确提取的重要保障,对原始高频数据中的小周跳和粗差十分敏感,且能够有效地估计小周跳和粗差,从而抵抗它们对同震速度估计的不良影响;另外,改进算法还简化了数据处理流程,也使得利用广播星历单站提取同震速度、监测地震形变的算法更为稳健.选取了2011年3月11日日本大地震距离震中140 km的MIZU站1 Hz高频GPS观测数据和广播星历来测试改进算法.结果表明：拟准检定法具有更好的小周跳与粗差自动定位和估计性能,改进算法利用广播星历求得的同震速度与事后动态精密单点定位结果表现出很好的一致性.  相似文献   

Modeling soil erosion using a spatially distributed model in a karst catchment of northwest Guangxi,China   总被引：2，自引：0，他引：2       下载免费PDF全文

Teng Feng  Hongsong Chen  Kelin Wang  Wei Zhang  Xiangkun Qi 《地球表面变化过程与地形》2014,39(15):2121-2130

Reliable assessment of the spatial distribution of soil erosion is important for making land management decisions, but it has not been thoroughly evaluated in karst geo‐environments. The objective of this study was to modify a physically based, spatially distributed erosion model, the revised Morgan, Morgan and Finney (RMMF) model, to estimate the superficial (as opposed to subsurface creep) soil erosion rates and their spatial patterns in a 1022 ha karst catchment in northwest Guangxi, China. Model parameters were calculated using local data in a raster geographic information system (GIS) framework. The cumulative runoff on each grid cell, as an input to the RMMF model for erosion computations, was computed using a combined flow algorithm that allowed for flow into multiple cells with a transfer grid considering infiltration and runoff seepage to the subsurface. The predicted spatial distributions of soil erosion rates were analyzed relative to land uses and slope zones. Results showed that the simulated effective runoff and annual soil erosion rates of hillslopes agreed well with the field observations and previous quantified redistribution rates with caesium‐137 (¹³⁷Cs). The estimated average effective runoff and annual erosion rate on hillslopes of the study catchment were 18 mm and 0.27 Mg ha^?1 yr^?1 during 2006–2007. Human disturbances played an important role in accelerating soil erosion rates with the average values ranged from 0.1 to 3.02 Mg ha^?1 yr^?1 for different land uses. The study indicated that the modified model was effective to predict superficial soil erosion rates in karst regions and the spatial distribution results could provide useful information for developing local soil and water conservation plans. Copyright © 2014 John Wiley & Sons, Ltd.  相似文献   

Control of differential tectonic evolution on petroleum occurrence in Bohai Bay Basin     

TENG ChangYu  ZOU HuaYao  HAO Fang 《中国科学:地球科学(英文版)》2014,57(5):1117-1128

The Bohai Bay Basin(BBB)is the most petroliferous Cenozoic basin in the east of China.It consists of seven depressions.Each depression has been subjected to different stress states and then has experienced varying faulting processes since the Neogene,especially during the Neotectonism(from the Pliocene to the present).On the basis of the investigation of fault patterns,fault densities and fault activity rates(FARs)for each depression,this paper demonstrates the discrepancy of faulting development and evolution across the BBB.The dynamic mechanism for the differences in faulting is also discussed by the analysis of the regional stress state.The Bozhong Depression is just situated in the transtensional zone induced by the two active strike-slip faults,namely Yingkou-Weifang and Beijing-Penglai.In this depression,the major faults which cut through the Paleogene or the Cenozoic have had higher than 10 m/Ma FARs since the Neogene,and the highest FARs have reached or exceeded 25 m/Ma during the Neotectonism.As a result,most of the petroleum has migrated along these major faults and accumulated within the Neogene.In contrast,in the other depressions of the BBB away from the Bozhong Depression,the FARs of the major faults were decreased to lower than 10 m/Ma since the Neogene,and tended to be zero during the Neotectonism.Therefore,the major faults could not serve as vertical conduits for petroleum migration,and the petroleum was entrapped in the Paleogene.Consequently,the faulting since the Neogene,especially during the Neotectonism,controlled the petroleum richness in vertical strata.  相似文献