溧阳体应变观测资料综合分析     

郑江蓉  李鸿宇  梁学萍  周健 《地震地磁观测与研究》2005,26(4):90-97

江苏省溧阳体应变自1994年开始观测以来，经历了1994年至2000年以整点值为主的模拟观测，和2001年至今以分钟值为主的数字化观测两个阶段，对这两个观测阶段观测资料变化形态、观测质量和观测精度、潮汐因子中误差、地震波记录能力等参数进行对比研究，同时采用固体潮汐残差矢量分析方法，对溧阳台1996年以来的观测资料进行了计算分析。结果表明：①溧阳台数字化观测和模拟观测资料的形态、观测精度、方差、潮汐因子中误差、相位滞后等参数无显著差异；影响观测资料精度的主要因素是仪器故障、水位、气压、气温等；②溧阳体应变固体潮汐残差矢量对1996年11月9日长江口6．1级地震异常特征明显，映震效果显著。  相似文献   

支持向量机在砂土液化预测中的应用研究   总被引：4，自引：0，他引：4  

陈荣淋  林建华  黄群贤 《中国地质灾害与防治学报》2005,16(2):15-18,23

介绍了人工智能领域最新的基于结构风险最小化原理的数据挖掘算法——支持向量机算法。根据支持向量机线性分类和可以具有不同核函数的非线性分类两种算法，建立了砂土液化预测模型，并且运用Matlab语言编写了程序。通过试算和分析比较得到了最佳模型，最佳模型的预测结果与实际液化情况基本上一致。认为支持向量机算法无论在学习或者预测精度方面都有很大的优越性，而基于支持向量机理论建立的砂土液化预测模型是可行的，且可以较为准确地实现砂土液化的预测。  相似文献   

处理非线性分类和回归问题的一种新方法 (Ⅱ)——支持向量机方法在天气预报中的应用   总被引：44，自引：5，他引：44       下载免费PDF全文

冯汉中  陈永义 《应用气象学报》2004,15(3):355-365

将SVM（Support Vector Machine）分类和回归方法首次应用于气象预报试验。利用1990~2000年4~9月ECMWF北半球的500 hPa高度、850 hPa温度、地面气压的00:00 UTC分析场资料，建立四川盆地分区面雨量有无大于15 mm的SVM分类推理模型、四川盆地内单站气温的SVM回归推理模型，进行相应的预报试验，试验结果显示对应的SVM推理模型具有良好的预报能力。  相似文献   

重力异常矢量的空间分布特征及其应用     

李九亮 《地质与勘探》1997,33(6):34-40

通过所研究地质体在剖面内产生的重力异常垂直分量ｇｚ和水平分量ｇｘ，求得了剖面内重力矢量强度ｇ及矢量轨迹线微分方程的表达式，进而求出了矢量轨迹线方程。较详细地论证了空间等值线和矢量轨迹线在这量解释中应用的基本方法－量扳法。  相似文献   

GPS phase accelerations for moving-base vector gravimetry   总被引：6，自引：1，他引：6  

C. Jekeli  R. Garcia 《Journal of Geodesy》1997,71(10):630-639

For airborne gravimetry using INS and GPS, the accelerations from both systems are differenced to yield the gravity acceleration. Usually, the GPS acceleration is determined by first solving for the position of the vehicle relative to a base station and subsequently taking two time derivatives of the vertical component. An alternative method is to time-differentiate the observed phases directly, thus avoiding the cycle ambiguity problem that must be solved for positioning and that is fraught with (certainly not insurmountable) difficulties in the event of a cycle slip. Due to the largely unpredictable receiver-clock errors and the imposition of the Selective Availability degradation, doubly differenced (in space) phase accelerations are used to obtain the relative vehicle accelerations. Test results for stationary receivers show that the acceleration vector can be determined from phase accelerations to an accuracy of 1 mgal for 40-s averages. The mathematical formulation of the acceleration determination also highlights certain other advantages over traditional methods, such as the avoidance of the E?tv?s correction, although a similar kind of velocity effect must be determined. Received: 9 September 1996 / Accepted: 14 April 1997  相似文献   

高斯平面上GPS工程网数据处理   总被引：2，自引：0，他引：2  

郑国宁  陈明剑 《测绘学院学报》1997,(2)

结合工程控制网的特点，给出高斯平面上GPS工程网数据处理的数学模型，对提高网的精度进行探讨，编写的软件对某GPS工程网进行数据处理与分析。  相似文献   

Spectral-finite-element approach to two-dimensional electromagnetic induction in a spherical earth     

Z. Martinec 《Geophysical Journal International》1997,130(3):583-594

We present a spectral-finite-element approach to the 2-D forward problem for electromagnetic induction in a spherical earth. It represents an alternative to a variety of numerical methods for 2-D global electromagnetic modelling introduced recently (e.g. the perturbation expansion approach, the finite difference scheme). It may be used to estimate the effect of a possible axisymmetric structure of electrical conductivity of the mantle on surface observations, or it may serve as a tool for testing methods and codes for 3-D global electromagnetic modelling. The ultimate goal of these electromagnetic studies is to learn about the Earth's 3-D electrical structure.
Since the spectral-finite-element approach comes from the variational formulation, we formulate the 2-D electromagnetic induction problem in a variational sense. The boundary data used in this formulation consist of the horizontal components of the total magnetic intensity measured on the Earth's surface. In this the variational approach differs from other methods, which usually use spherical harmonic coefficients of external magnetic sources as input data. We verify the assumptions of the Lax-Milgram theorem and show that the variational solution exists and is unique. The spectral-finite-element approach then means that the problem is parametrized by spherical harmonics in the angular direction, whereas finite elements span the radial direction. The solution is searched for by the Galerkin method, which leads to the solving of a system of linear algebraic equations. The method and code have been tested for Everett & Schultz's (1995) model of two eccentrically nested spheres, and good agreement has been obtained.  相似文献   

关于阵列的一点注记     

党诵诗 《武汉大学学报(信息科学版)》1988,(3)

本文对于阵列代数中的一个基本定理(阵列与矩阵乘积定理)用归纳方法给出较简的证明,此外,并建立k阶阵列与张量的一个关系。  相似文献   

Lunar and solar barometric tides at Rarotonga,Cook Islands     

J. W. Hutchings  J. W. Gellen 《Pure and Applied Geophysics》1988,126(1):141-151

Lunar and solar atmospheric tidal oscillations have been determined with reasonable accuracy from a ten-year record of hourly mercury-barometer readings, corrected to mean-sea-level, at Rarotonga (Cook Islands), 21.2°S. For the lunar semidiurnal tide, the annual determination shows an amplitude (56 b) slightly lower and a phase (51°) much smaller than the values (58 b, 72°) that would be derived, for the position of Rarotonga, from the spherical harmonic analysis given byHaurwitz andCowley (1969). The seasonal variation of this oscillation, as given by the monthly and J, E, D values, shows most of the characteristic features found in world-wide determinations. In particular, the near equality of the J, D amplitudes at Rarotonga tends to support theHaurwitz andCowley (1969) suggestion of negative J-D values in southern middle latitudes. For the solar tides, the semidiurnal and terdiurnal oscillations at Rarotonga are similar to those found at other stations in the south-west Pacific region. However, for the diurnal oscillation, the annual amplitude (232 b) is only about half the value (465 b) indicated for the position of Rarotonga by the world maps of theS ₁(p) annual harmonic coefficients given byHaurwitz (1965). It thus seems likely that the relatively small area of lowS ₁(p) annual amplitude in the eastern part of the south Pacific, as indicated by these maps, is much more extensive than formerly supposed.  相似文献   

Mg-Fe云母化学成分的解释和分类(Ⅰ)——基本置换和黑云母平面          下载免费PDF全文

孙世华  于洁 《地质科学》1989,(1):33

 中国东部花岗岩类141个Mg-Fe云母的化学成分将近90%的变化属于八面体层内的类质同象置换,置换矢量Mg ₁Fe⁺²和Fe_-3⁺²(R_Ⅵ⁺³)_-2□_Ⅵ组成了天然黑云母平面,大约80%的变化应当解释为基本置换8Mg ₁Fe⁺²+Fe_-3⁺²(R_Ⅵ⁺³)₂□_Ⅵ.这些是Mg-Fe云母在广泛的自然条件下表现出来的最主要的晶体化学关系。文中还提出了置换矢量的长度、分量和以及电价和三个参数,用以识别矿物化学成分变化的类质同象置换特征。  相似文献