Part II. Discontinuous Galerkin method applied to a single phase flow in porous media     

Béatrice Riviè;re  Mary F. Wheeler  Krzysztof Banaś 《Computational Geosciences》2000,4(4):337-349

Discontinuous Galerkin numerical simulations of single phase flow problem are described in this paper. The simulations show the advantages of using discontinuous approximation spaces. hp convergence results are obtained for smooth solutions. Unstructured meshes and unsmooth solutions are also considered.  相似文献   

高精度恒误差数字频率计设计   总被引：2，自引：0，他引：2  

周欣 《南京气象学院学报》2000,23(3):435-439

基于高精度恒误差测频原理,采用Ｌａｔｔｉｃｅ的在系统可编程器件（ｉｓｐＬＳＩ）进行数字频率计设计。结果表明,高精度恒误差测频原理是合理的,并对所采用的高精度恒误差测频原理作了深入的理论分析,给出了依据此原理实现的硬件电路。  相似文献   

国外测绘机构大地测量的新动向   总被引：2，自引：1，他引：1  

胡明城 《测绘科学》2000,25(3):51-55

本文概述国外测绘机构大地测量的动向 ,目的在于了解全球大地测量的发展趋势 ,作为借鉴。综观各国的大地测量动向可以看出 ,高精度国家大地控制网的建立 ,都是采用 GPS,无一例外 ,而且它们之间只是细节上的差异。从各国建立高精度大地控制网的目的来看 ,都是为多学科服务的。面对这样的总趋势 ,大地测量工作者必须拓宽知识面 ,迎接新的挑战。  相似文献   

广域差分GPS系统完备性监测   总被引：4，自引：2，他引：2  

秘金钟  李毓麟 《测绘科学》2000,25(1):28

广域差分 GPS系统完备性监测技术是广域差分的关键和核心。本文全面介绍了完备性监测技术的定义 ,完备性监测系统的构成 ,以及各个部分的监测方法 ,包括监测站和用户站的监测技术 ,最后给出了完备性监测的一般步骤。  相似文献   

昌平地震台地温前兆特征分析   总被引：2，自引：1，他引：1       下载免费PDF全文

王勇  张国红  代建华  段立新 《地震工程学报》2000,22(3):236-240

介绍了昌平地震台地温测点的基本情况及地温正常变化特征。分析了该测点记到的一些地震前的地地温异常变化特征。自１９９５年以来该测点观测到１１次异常,其中有９次与发生在该台附近（３００ｋｍ范围内）的地震相对应,有２次异常没有对应地震。距离该测点较近的地震的异常形态为趋势下降－回升型;距离该测点较远的地震的异常形态为跳型,震前异常幅度越大,平静时间越长,未来地震的震级越大,反之则小,以分为间隔的测值的异常  相似文献   

天水地震台最大振幅面波与初至波到时差和震中距的关系          下载免费PDF全文

吴启民  毛森林  刘东声  缑亚江  陈兰新 《地震工程学报》2000,22(3):348-350

根据天水地震台ＳＫ地震仪近年来记录的３３８个震例的资料,用最小二乘法求出最大振幅面波与初至波至时差同震中距的关系式,并与Ｊ－Ｂ表进行了对比,结果表明,用Ｊ－Ｂ表计算出的震中距与实际震中距的偏差较大,用本给出的关系式和走时表估算震中距可以缩小误差,提高定位精度。  相似文献   

地质标准物质中痕量元素量值溯源性探讨   总被引：10，自引：4，他引：6  

凌进中 《岩矿测试》2000,19(3):188-193

标准物质的特性量值应该具备溯源性。然而地质标准物质溯源性的建立往往是很困难的。对痕量元素量值溯源的若干难点进行了讨论;提出了建立标准物质研制的质量体系的建议并就相关问题进行了阐述;应重视量值的信息反馈,提高定值的质量。  相似文献   

Octahedral cation ordering in olivine at high temperature. I: in situ neutron single-crystal diffraction studies on natural mantle olivines (Fa12 and Fa10)     

R. Rinaldi  G. Artioli  C. C. Wilson  G. McIntyre 《Physics and Chemistry of Minerals》2000,27(9):623-629

Crystallographic determinations on natural olivine single crystals of mantle composition and origin, carried out by in situ neutron diffraction at high temperature, show that the octahedrally co-ordinated Fe²⁺ and Mg cations undergo two successive trends of cation ordering with increasing temperature. An initial slight preference of Fe²⁺ for site M1, up to a temperature of about 850?°C, is followed by a reverse-ordering reaction with a site preference exchange between the two cations. The cross-over between the two regimes of ordering, corresponding to a situation of complete disorder, occurs at about 900?°C. Above this temperature Fe²⁺ progressively and strongly segregates into site M2 up to 1300?°C, the practical limit of the experimental setup utilized in the experiments. Care was taken to ensure that no chemical changes occurred in the crystals (i.e. oxidation), as testified by Mössbauer spectroscopy determinations carried out before and after the heat treatment. The cation-ordering behaviour is reflected in temperature-dependent changes of geometrical and atomic displacement parameters occurring in the octahedral sites M1 and M2. A thermodynamical explanation of this behaviour is proposed in terms of a prevailing vibrational contribution to entropy.  相似文献   

Determination of High Field Strength Elements, Rb, Sr, Mo, Sb, Cs, Tl and Bi at ng g⁻¹ Levels in Geological Reference Materials by Magnetic Sector ICP-MS after HF/HClO₄ High Pressure Digestion     

Zongshou Yu  Philip Robinson  Ashley T. Townsend  Carsten Mnker  Anthony J. Crawford 《Geostandards and Geoanalytical Research》2000,24(1):39-50

Six low abundance rock reference materials (basalt BIR-1, dunite DTS-1, dolerite DNC-1, peridotite PCC-1, serpentine UB-N and basalt TAFAHI) have been analysed for high field strength elements (Zr, Nb, Hf, Ta, Th and U), Rb, Sr, Mo, Sb, Cs, Tl and Bi at ng g⁻¹ levels (in rock) by magnetic sector inductively coupled plasma-mass spectrometry after HF/HClO₄ high pressure decomposition. The adopted method uses only indium as an internal standard. Detection limits were found to be in the range of 0.08 to 16.2 pg ml⁻¹ in solution (equivalent to 0.08 to 16.2 ng g⁻¹ in rock). Our data for high field strength elements, Rb, Sr, Mo, Sb, Cs, Tl and Bi for the six selected low abundance geological reference materials show general agreement with previously published data. Our Ta values in DTS-1 and PCC-1 (1.3 and 0.5 ng g⁻¹) are lower than in previously published studies, providing smooth primitive mantle distribution patterns. Lower values were also found for Tl in BIR-1, DTS-1 and PCC-1 (2, 0.4 and 0.8 ng g⁻¹). Compared with quadrupole ICP-MS studies, the proposed magnetic sector ICP-MS method can generally provide better detection limits, so that the measurement of high field strength elements, Rb, Sr, Mo, Sb, Cs, Tl and Bi at ng g⁻¹ levels can be achieved without pre-concentration, ion exchange separation or other specialised techniques.  相似文献   

Determination of Trace Elements in Twenty Six Chinese Geochemistry Reference Materials by Inductively Coupled Plasma-Mass Spectrometry   总被引：20，自引：0，他引：20  

Qi Liang  D. Conrad Grégoire 《Geostandards and Geoanalytical Research》2000,24(1):51-63

We report new data for thirty seven elements determined in twenty six Chinese geochemistry reference materials using inductively coupled plasma-mass spectrometry and a reliable and simple dissolution technique. One hundred milligrams of sample were digested with 1 ml of HF and 0.5 ml of HNO₃ in PTFE-lined stainless steel bombs heated to 200 °C for 12 hours. Insoluble residues were dissolved using 6 ml of 40% v/v HNO₃ heated to 140 C for 3 hours. Analytical calibration was accomplished using aqueous standard solutions. Rhodium was used as an internal standard to correct for matrix effects and instrument drift. Precisions were typically better than 5% RSD. Most of the data presented here agree well with the published certified values. For the elements Zr, Hf and most other trace elements, the measured values were less than 10% in error when compared to certified values.  相似文献