基于零立体像对立体匹配的配后质量控制   总被引：1，自引：0，他引：1  

万志龙 《测绘学院学报》1994,(4)

立体匹配的质量控制对数字摄影测量产品的质量起着关键的作用。本文首先分析了现有的各种质量控制策略，然后根据正射影像同ＤＴＭ及匹配点位存在的固有关系，提出了用零立体像对再匹配作为立体匹配的配后质量控制方案，为立体匹配质量控制开辟了崭新的途径。  相似文献   

Waveform response to the morphology of 2-D subducted slabs     

Hua-wei Zhou  Genmeng Chen 《Geophysical Journal International》1995,121(2):511-522

  相似文献   

The Canada-Ontario-industry rockburst project     

D. G. F. Hedley  J. E. Udd 《Pure and Applied Geophysics》1989,129(3-4):661-672

This project was started in 1985, after a particularly extensive period of rockburst activity in several Ontario mines. Three parties participated in the project: the Government of Canada, through CANMET, the Ontario Ministries of Labour and Northern Development and Mines, and the Ontario Mining Association.The first two years of the project have been mainly devoted to the design and installation of new seismic monitoring systems. It is intended to install three different types of monitoring systems at the four mining camps experiencing rockbursts (Red Lake, Elliot Lake, Sudbury, and Kirkland Lake). Seismograph units will be installed at each mining camp to obtain permanent records of the larger seismic events and their magnitude. Macroseismic systems are being installed around five mines (Campbell, Quirke, Strathcona, Creighton and Macassa). These systems consist of triaxial, strong-motion geophones with processing units for event detection and data digitization. Complete waveforms are captured to study first motion, peak particle velocity, seismic energy and spectral frequency. At present 13 mines in Ontario operate their own microseismic systems which are used exclusively for real time source location of seismic events.The instrumentation already installed and the present research activities at the mines are described in the paper.Presented at the Fred Leighton Memorial Workshop on Mining Induced Seismicity, Montreal 1987.  相似文献   

基于二进小波变换的遥感影像镶嵌方法     

李军  林宗坚 《武汉大学学报(信息科学版)》1995,(4)

提出了一种新的影像镶嵌方法。通过与经典的直方图色调匹配方法实验结果比较，证明该方法克服了相邻影像中局部灰度差异大的问题，保证了接缝邻域处的图像清晰度和光滑度两个方面的要求。  相似文献   

用于运动估计的高效三步法的VLSI实现   总被引：1，自引：0，他引：1  

丁锐  邝继顺  谭论正 《武汉大学学报(信息科学版)》2006,31(9):842-845

根据高效三步法的特点，提出了有效的数据流和相应的VLSI结构。该数据流充分利用参考帧搜索点之间数据重叠的特征，以减少数据存储器访问的次数，从而减少了运动估计中功率消耗最大部分的操作。通过对各种测试序列的仿真证明，该VLSI结构有效地实现了高效三步法，适合MPEG-4和HDTV应用。  相似文献   

A multiscale method for distributed parameter estimation with application to reservoir history matching     

Sigurd Ivar Aanonsen  Dmitry Eydinov 《Computational Geosciences》2006,10(1):97-117

A method for multiscale parameter estimation with application to reservoir history matching is presented. Starting from a given fine-scale model, coarser models are generated using a global upscaling technique where the coarse models are tuned to match the solution of the fine model. Conditioning to dynamic data is done by history-matching the coarse model. Using consistently the same resolution both for the forward and inverse problems, this model is successively refined using a combination of downscaling and history matching until model-matching dynamic data are obtained at the finest scale. Large-scale corrections are obtained using fast models, which, combined with a downscaling procedure, provide a better initial model for the final adjustment on the fine scale. The result is thus a series of models with different resolution, all matching history as good as possible with this grid. Numerical examples show that this method may significantly reduce the computational effort and/or improve the quality of the solution when achieving a fine-scale match as compared to history-matching directly on the fine scale.  相似文献   

黄河下游河道输沙水量及计算方法研究   总被引：15，自引：0，他引：15       下载免费PDF全文

申冠卿  姜乃迁  李勇  尚红霞  李小平 《水科学进展》2006,17(3):407-413

根据黄河下游1950年以来的水沙、河道冲淤及洪水观测资料,系统分析了黄河下游主要控制站输沙水量与来沙量、洪水量级、水沙搭配、区间引水引沙及河道允许淤积度等因子间的相互关系。在探讨泥沙输移规律和机理的基础上,引入水沙搭配参数,建立了适用于黄河下游主要控制站汛期及洪水期计算输沙水量的数学表达式,量化了水沙条件及河道允许淤积度变化对河道输沙水量的影响程度。该研究对维持黄河健康生命及黄河水资源的规划利用具有重要的理论和实际意义。  相似文献   

Another look at the 1993 and 1995 Gulf of Aqaba earthquakes from the analysis of teleseismic waveforms   总被引：3，自引：0，他引：3  

Ali K. Abdel-Fattah  H. M. Hussein  S. El-Hady 《Acta Geophysica》2006,54(3):260-279

In this work we estimated the source process and the source parameters of the 1993 and 1995 Gulf of Aqaba earthquakes. To investigate the source process of both events, we inverted the teleseismic P- and SH-waveform data using an iterative technique in which the rupture is modeled as a series of point source subevents with varying mechanisms. The main source process of the 1993 event can be explained by two subevents with essentially the same mechanism. These two subevents had different focal depths. The second subevent was about 5 s later than the first one and about 70% of the moment rate released with the second one. The total rupture duration time was about 12 s. Our solution for the 1995 Gulf of Aqaba earthquake indicated that the event consists of three subevents with various fault geometries and about 60% of the moment released by the second subevent. The first subevent occurred at a depth of 13 km, and was followed after 9 s by the second one at a depth of 11 km; the third subevent, at a depth of 9 km occurred 19 s after the second one. The total duration of the earthquake rupture process was about 18.7 s. The obtained mechanisms for the 1993 and 1995 Gulf of Aqaba earthquakes are well correlated with the structural setting of the Gulf of Aqaba.  相似文献   

The effectiveness of spectral similarity measures for the analysis of hyperspectral imagery     

Freek van der Meer 《International Journal of Applied Earth Observation and Geoinformation》2006

In geological imaging spectrometry (i.e., hyperspectral remote sensing), surface compositional information (e.g., mineralogy and subsequently chemistry) is obtained by statistical comparison (by means of spectral matching algorithms) of known field- or library spectra to unknown image spectra. Though these algorithms are readily used, little emphasis has been given to comparison of the performance of the various spectral matching algorithms. Four spectral measures are presented: three that calculate the angle (spectral angle measure, SAM), the vector distance (Euclidean distance measure, ED) or the vector cross-correlation (spectral correlation measure, SCM), between a known reference and unknown target spectrum and a fourth measure that measures the discrepancy of probability distributions between two pixel vectors (the spectral information divergence, SID). The performance of these spectral similarity measures is compared using synthetic hyperspectral and real (i.e., Airborne Visible Infrared Imaging Spectrometer, AVIRIS) hyperspectral data of a (artificial or real) hydrothermal alteration system characterised by the minerals alunite, kaolinite, montmorillonite and quartz. Two statistics are used to assess the performance of the spectral similarity measures: the probability of spectral discrimination (PSD) and the power of spectral discrimination (PWSD). The first relates to the ability of the selected set of spectral endmembers to map a target spectrum, whereas the second expresses the capability of a spectral measure to separate two classes relative to a reference class. Analysis of the synthetic data set (i.e., simulated alteration zones with crisp boundaries at 1–2 nm spectral resolution) shows that (1) the SID outperforms the classical empirical spectral matching techniques (SAM, SCM and ED), (2) that SCM (SID, SAM and ED do not) exploits the overall shape of the reflectance curve and hence its outcomes are (positively and negatively) affected by the spectral range selected, (3) SAM and ED give nearly similar results and (4) for the same reason as in (2), the SCM is also more sensitive (again in positive and negative sense) to the spectral noise added. Results from the study of AVIRIS data show that SAM yields more spectral confusion (i.e., class overlap) than SID and SCM. In turn, SID is more effective in mapping the four target minerals than SCM as it clearly outperforms SCM when the target mineral coincides with the mineral phase on the ground.  相似文献   

On the effects of petrographic composition on coalbed methane sorption     

Gareth R.L. Chalmers  R. Marc Bustin 《International Journal of Coal Geology》2007,69(4):288-304

The effect of petrographic composition on the methane sorption capacity has been determined for a suite of coals and organic-rich shales. Subbituminous and bituminous coals were separated into bright and dull lithotypes by hand-picking. The methane sorption capacities range between 0.5 and 23.9 cm³/g at a pressure of 6 MPa. The low volatile bituminous Canmore coal and the anthracite sample have the highest capacities with the “natural coke” having the lowest. For low-rank coals there is no significant difference between bright and dull samples except for one coal with the dull sample having a greater sorption capacity than its bright equivalent. For higher-rank coals, the bright samples have a greater methane capacity than the dull samples and the difference between sample pairs increases with rank. The boghead coal samples have the highest sorption capacities in the liptinite-rich coals suite and are higher than subbituminous to medium volatile bituminous samples. Pore size distribution indicates that methane is held as solution gas in liptinite-rich coals and by physical sorption in micropores in liptinite-poor coals. These contrasting processes illustrate that liptinite-rich samples need to be independently assessed. The positive relationship between reactive inertinite content and methane sorption capacity occurs within the subbituminous to medium volatile bituminous coals because the reactive inertinite is structurally similar to vitrinite and have a higher microporosity than non-reactive inertinite. Reactivity of inertinite should be assessed in CBM studies of dull coals to provide a better understanding of petrographic composition effects on methane capacity.  相似文献