借助Matlab遗传算法反演火山区压力源参数

首先分析了Mogi模型的经典最小二乘反演由于出现矩阵奇异或接近奇异而发散的局限性,决定采用具有全局高效搜索性和优化计算时不需要求导的遗传算法来反演火山区压力源参数。反演程序调用Matlab7.0 Release14工具箱中的选择、交叉和变异等相关程序。最后应用该程序和长白山天池火山区水准和GPS观测资料联合反演火山区压力源参数,经过比较遗传算法和阻尼最小二乘方法的反演结果,可看出2种方法结果近似,可见此方法方便快捷地实现了目标函数的最小化。     

The harmonic decomposition reconstruction for the exponential radon transform

The exponential Radon transform, a generalization of the Radon transform, is defined and studied as a mapping of function spaces. It is represented in terms of Fourier transform of its domain and range, and this leads to the harmonic decomposition reconstruction. The results are similar results of Tretiak and Metz. Foundation item: Supported by the National Natural Science Foundation of China (No. 19971064), Key Project of Science and Technology of Hubei Province Education Committee. Biography: Wang Jin-ping (1963-), male, Ph.D. candidate, research direction: numberical solution of singular integral equation and integral transformation etc.     

面近正则外平面地图的色计数函数

首先给出了不可分离面近正则(除根面外,其它每个面的次均是常数k,其中k≥3)外平面地图的色数、根面次和边数3个参数的色计数函数所满足的方程,并给出了它的显式表达式.然后,给出了可分离面近正则外平面地图的色数、根面次和边数3个参数的色计数函数所满足的方程.     

层析成像的模糊-神经网络重建方法

考虑投影数据不足时，射线层析成像的离散重建算法难以取得较好效果的情况，利用模糊理论建立了表示物体衰减系数的连续函数，用神经网络学习算法确定该连续函数中的待定参数．提出了一种适于投影数据或投影方向不够时的CT图像重建算法．计算机仿真结果显示了该方法在投影数据严重缺少时的良好效果。     

矩阵范数的界和方阵的ρ-条件数

本文给出了长方矩阵的p-范数及更广一类矩阵范数的上、下界又给出了方阵的p-条件数等于1的条件。(1≤p≤ ∞)。文[1]则是p=2的情况。前三节讨论p-条件数,第四节讨论长方矩阵范数的界。     

基于量子微粒群优化算法的半透明介质光学参数反演

针对半透明介质光学参数估计问题,建立了脉冲激光辐照下半透明介质光学参数反演模型,采用量子微粒群优化(QPSO)算法反演了折射率和吸收系数,分析了测量误差、热物性参数对反演结果的影响,并利用敏感性分析揭示了反演精度与测量误差的关系.计算结果表明：建立的反演模型和采用的QPSO算法可以精确估计折射率和吸收系数,即使人为添加10%的测量误差,反演结果依然具有较强的鲁棒性和准确度.本研究可为半透明介质物性参数获取提供技术参考.     

波阻抗反演技术在孤东地区馆陶组薄储层描述中的应用

根据一维波动方程的拟合迭代法原理 ,给出了求解波阻抗σ(x)的算法。针对孤东地区馆陶组薄储层油藏存在的地层埋深浅、较疏松以及井径变化大泥岩中含有膨化矿物蒙脱石等引起的声波测井速度失真问题 ,采用分段函数法对其进行了校正。将校正后的声波资料进行反演 ,可得到高质量的资料 ,用该校正资料追踪描述的储层与录井结果吻合较好。应用结果表明 ,测井资料在反演中可以补充地震资料缺少的低频和高频分量 ,地震波阻抗反演技术是薄储层描述的有效方法     

Present-Day crustal deformation field in China continent inverted from GPS observations, earthquake moment tensor and quaternary fault slip rates

Based on the bi-cubic Bessel spline function method, we have inverted the present-day crustal horizontal velocity field and deformation field in China continent by combining with 410 GPS observations, 327 seismic moment tensors of earthquakes and fault slip rates in China and its neighboring areas, and considered the geological and geophysical parameters at the same time. The results reveal that the crustal movement mostly takes on compression in SN-NE direction and extension in EW-NW direction in China continent. The continent is rotating southeast and takes on a clockwise rotation image from the west to the east, particularly in the southeast of Tibet and Chuan-dian area. Different blocks have different deformation in China continent. The south China, Ordos and Northeast block have good integrity.The deformation in the western part of China is obviously stronger than that in the eastern part. The strong strains are focused on the Himalaya, east Tibet,west Tian Shan and Chuandian block etc. The deformation at the joint of blocks is stronger than that within the blocks. The China continent deformation not only has the strike-slip faulting and extrusion feature but also has the crustal shortening and thickening feature.     

An iterative algorithm in potential-field inversion

1　Principle and MethodAll the problems of potential- field inversioncan be concluded that of solving nonlinear functionas follows:b =f( x) ( 1 )where x =( x1,x2 ,… .xn) T,xj( j =1 ,2 ,… ,n)indicate geometricparameters and physical parame-ters of the object;b=( b1,b2 ,… ,bm) T,bi( i=1 ,2 ,… ,m) indicate potential- field measurements.Main algorithms for expression( 1 ) are leastsquare method ( include damping least squaremethod ) ,gradient method ( conjugate gradientmethod and variable met…     

重磁电震信息联合反演的随机建模技术

为了把目前的重磁反演从理论建模延伸到随机建模领域，本文从物理场、级数理论出发提出了重磁统计推断建模反演的方法．该方法在重磁场源分离的基础上，以断裂系统把研究区划分为一些独立的次级单元．在各单元内把要反演的地下界面深度作为其对应的极值重磁异常的二元复合逆函数，利用已知的重磁电震剖面资料，统计推断其逆函数的级数分布，以建立重磁电震联合反演的随机地质模型．应用该方法获得了合肥盆地的结晶基底构造图．该项技术探索．有潜能推进综合地球物理信息勘探技术发展．