共查询到20条相似文献,搜索用时 15 毫秒
1.
利用反问题新算法—时间域正演反演法研究非线性抛物型方程的逆时反问题。该方法处理反问题的主要思路是先求解相对应的正问题,获得解在特定时间网格处的近似值;然后构造一个合适的全纯映射,在象空间中获得解在时间网格对应点处的近似值;最后利用解析函数的唯一延拓性质实现反问题的逆时间反演。数值模拟例子说明了方法的有效性。 相似文献
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讨论了一类二阶抛物型方程反问题的数值解法。应用拟解法的思想,把原问题分解为一系列适定的正问题和一个不适定的线性代数方程组。对于相应的正问题,证明了解连续依赖于初始分布,由此得到了在时刻的稳定性估计。使用古典欧拉差分格式求解正问题和用截断奇异值分解法求解病态方程组。数值结果显示数值解与理论解吻合很好。 相似文献
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Jef Caers 《Mathematical Geology》2007,39(1):27-52
Inverse problems are ubiquitous in the Earth Sciences. Many such problems are ill-posed in the sense that multiple solutions can be found that match the data to be inverted. To impose restrictions on these solutions, a prior distribution of the model parameters is required. In a spatial context this prior model can be as simple as a Multi-Gaussian law with prior covariance matrix, or could come in the form of a complex training image describing the prior statistics of the model parameters. In this paper, two methods for generating inverse solutions constrained to such prior model are compared. The gradual deformation method treats the problem of finding inverse solution as an optimization problem. Using a perturbation mechanism, the gradual deformation method searches (optimizes) in the prior model space for those solutions that match the data to be inverted. The perturbation mechanism guarantees that the prior model statistics are honored. However, it is shown with a simple example that this perturbation method does not necessarily draw accurately samples from a given posterior distribution when the inverse problem is framed within a Bayesian context. On the other hand, the probability perturbation method approaches the inverse problem as a data integration problem. This method explicitly deals with the problem of combining prior probabilities with pre-posterior probabilities derived from the data. It is shown that the sampling properties of the probability perturbation method approach the accuracy of well-known Markov chain Monte Carlo samplers such as the rejection sampler. The paper uses simple examples to illustrate the clear differences between these two methods 相似文献
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Juan L. Fernández Martínez César O. Menéndez Pérez Luis M. Pedruelo González José P. Fernández Alvarez Pablo Cienfuegos Suárez 《Mathematical Geology》2003,35(8):953-969
In this article we present a geostatistical approach to the transmission tomographic inverse problem, which is based on consideration of the inverse problem variables (velocity and traveltime errors) as regionalized variables (R.V.). Their structural analysis provides us with a new method to study the geophysical anisotropy of the rock, an important source of a priori information in order to design the anisotropic corrections. The underlying idea is that the geophysical structure can be deduced from the spatial structure of the regionalized variables which result from solving the tomographic problem with an isotropic algorithm. Also, the application of the structural analysis technique to the anisotropic corrected velocity field allows us to characterize the reliability of these corrections (model quality analysis). Geostatistical formalism also provides us with different techniques (parametric and non-parametric) to estimate and even simulate the velocity in the areas where this field has been considered anomalous based on field studies and on geophysical and statistical criteria. The kriging acts as a low-pass smoothing filter for the anomalous model parameters (velocities), but is not a substitute for an adequate filtering of the outliers before the inversion. This methodology opens the possibility of considering the inverse problem variables as stochastic processes, an important feature in cases where the tomogram is to be used as a tool of assessment to quantify the rock heterogeneities. 相似文献
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用非线性遗传反演方法进行自动静校正 总被引:4,自引:0,他引:4
静校正处理是消除近地层影响的一个重要地震资料数字处理方法,在近地表层纵,横向变化复杂,静校正量变化较大的地区,常规静校正方法和线性反演方法均不能解决问题,遗传算法是近年发展起来的一种模拟生物生化过程的较先进的非线性反演方法,对用遗传算法进行静校正的若干问题进行了讨论,说明它是可以解决表层情况复杂地区静校正问题的一个有效方法。 相似文献
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Numerical computations concerning geochemical processes in porous media require a knowledge of the values of the macroscopic
parameters. In the context of the interpretation of leaching tests one such parameter is the apparent macroscopic diffusivity.
In this paper, a mathematical model for dissolution in the presence of diffusion is considered. It is shown that the constant
diffusion coefficient can be identifiable when the time integral of the flux is known. Moreover, a practical algorithm for
computing the diffusion coefficient is proposed.
This revised version was published online in August 2006 with corrections to the Cover Date. 相似文献
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Juan L. Fernández Martínez José P. Fernández Alvarez Luis M. Pedruelo González 《Mathematical Geology》2006,38(3):343-374
Transmission tomography methods show a great sensibility to data variability, which eventually includes data errors, often present in field experiments. Local optimization methods, traditionally used to solve this inverse problem, are very sensitive to these difficulties, failing to converge properly in the presence of spurious data. Regularization methods partially cope with these weaknesses, damping the instabilities.A complementary approach, adopted here, is to perform a structured analysis of data variability before the inversion, oriented to discriminate the contribution of errors from that of true geological heterogeneities. The key concept of mean traveltime curves ( and ) is introduced and described. Their analytical equations are deduced for isotropic homogeneous media and any recording geometry. Empirical mean traveltime curves can be inferred based solely on traveltime data, using the corresponding discrete estimators. The methodology proposed here proceeds through a user-defined subdivision of the domain of interest into isotropic homogeneous areas. Least squares velocity estimations and associated data misfits are used to scrutinize the behaviour of the implied source-receiver sets and of the ray-swept part of the geologic medium. Data are considered suspicious if zonal estimated velocities are non-consistent with a priori information. Also, independent fitting of both empirical curves helps to classify the genesis of the residuals: some situations are illustrated.Finally, we show the application of this technique to a data set from the Grimsel test site in Switzerland. Using this methodology, we detect some anomalous gathers, which may be responsible for the large range of velocities found in the initial imaging with this data set. Also, we give some indications of the possible sources of these anomalies. This approach offers a quick data variability analysis in the pre-processing stage, which, even if no data editing algorithms are finally used, always improves the understanding of the data structure. 相似文献
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A GCV based method for nonlinear ill-posed problems 总被引:5,自引:0,他引:5
This paper discusses the inversion of nonlinear ill-posed problems. Such problems are solved through regularization and iteration
and a major computational problem arises because the regularization parameter is not known a priori. In this paper we show
that the regularization should be made up of two parts. A global regularization parameter is required to deal with the measurement
noise, and a local regularization is needed to deal with the nonlinearity. We suggest the generalized cross validation (GCV)
as a method to estimate the global regularization parameter and the damped Gauss-Newton to impose local regularization. Our
algorithm is tested on the magnetotelluric problem.
In the second part of this paper we develop a methodology to implement our algorithm on large-scale problems. We show that
hybrid regularization methods can successfully estimate the global regularization parameter. Our algorithm is tested on a
large gravimetric problem.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
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环境水力学反问题研究进展 总被引:3,自引:0,他引:3
反问题广泛存在于环境水力学的各个研究领域,通过环境水力学反问题研究可以实现对水流及伴随水流系统的污染物质迁移、输运过程的识别和控制,促进水资源的可持续利用。近年来,环境水力学反问题研究内容逐渐丰富,其重要性日渐突出。基于反问题理念阐述了环境水力学反问题的内涵,从不同的角度对环境水力学反问题进行了分类,强调了环境水力学反问题研究的重要意义。从参数反问题、源项反问题、边界条件反问题、初始条件反问题和形状反问题5个方面分析评述了环境水力学反问题的研究现状和研究成果。在此基础上,讨论了研究现状存在的问题并对该领域未来研究方向进行了展望。 相似文献
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区间入流是影响水动力模型精度的重要因素,实际的区间径流情况复杂难以量化。从反问题的角度出发,由基本方程导出区间入流校正量的解析表达式,应用数值离散方法,得到节点水位与区间入流的响应函数,根据实测的潮位资料建立区间入流的迭代求解方法。数值实验验证了方法的可行性,反问题的计算值与真值非常接近,模拟的确定性系数达到0.996。该方法应用于长江下游大通至镇江河段的水动力模型实例计算,得出了概化的区间入流过程,提高了模拟精度,验证了方法的有效性。 相似文献
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Accurate identification of interactions of reactive solutes with porous media constituents is necessary for reliable risk
assessment studies and the development of efficient sanitation strategies. Standard parameter estimation procedures bear a
number of unsolved problems with respect to uniqueness and identifiability. This paper presents a new approach for the identification
of nonlinear interaction parameters of column outflow experiments. The procedure requires no a priori assumptions on the shape
of the underlying interaction process functions. Employing experimental data sets on cadmium and anthracene breakthrough as
case studies, possible applications of the new approach will be shown, and its features will be discussed. Error analysis
based on singular value decomposition of the sensitivity matrix quantifies the identification error. Identification procedures
without a priori shape information are superior to fixed parametrizations in diagnostic investigations, especially in cases
without reliable a priori knowledge on the sorptive interactions. 相似文献
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We consider the inverse problem of permeability estimation for two-phase porous-media flow. The novel approach is based on
regularization by zonation, where the geometry and size of the regions are chosen adaptively during the optimization procedure.
To achieve this, we have utilized level-set functions to represent the permeability. The available data are sparsely distributed
in space; hence, it is reasonable to confine the estimation to coarse-scale structures. The level-set approach is able to
alter the boundaries between regions of different permeability without strict restrictions on their shape; however, when the
data are sparse, a reasonable initial guess for the permeability is required. For this task, we use adaptive multiscale permeability
estimation, which has the potential of identifying main permeability variations. These are described by a piecewise constant
function, where the constant values are attained on rectangular zones. In the current work, we develop a level-set corrector
strategy, assuming adaptive multiscale permeability estimation as a predictor. 相似文献
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Pranav M. Karve Arash Fathi Babak Poursartip Loukas F. Kallivokas 《国际地质力学数值与分析法杂志》2017,41(7):1016-1037
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This paper is devoted to the numerical reliability and time requirements of the Mixed Finite Element (MFE) and Mixed-Hybrid Finite Element (MHFE) methods. The behavior of these methods is investigated under the influence of two factors: the mesh discretization and the medium heterogeneity. We show that, unlike the MFE, the MHFE suffers with the presence of badly shaped discretized elements. Thereat, a numerical reliability analyzing software (Aquarels) is used to detect the instability of a matrix-inversion code generated automatically by a symbolic manipulator. We also show that the spectral condition number of the algebraic systems furnished by both methods in heterogeneous media grows up linearly according to the smoothness of the hydraulic conductivity. Furthermore, it is found that the MHFE could accumulate numerical errors if large jumps in the tensor of conductivity take place. Finally, we compare running-times for both algorithms by giving various numerical experiments. 相似文献
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In this paper, the deterministic parameter identification procedure proposed in a companion paper is applied to suction‐dependent elasto‐plasticity problems. A mathematical model for such type of problems is firstly presented, then it is applied to the parameter identification using laboratory data. The identification procedure is applied in a second example to exploitation of a gas reservoir. The effects of the extraction of underground fluids appear during and after quite long periods of time and strongly condition the decision to profit or not of the natural resources. Identification procedures can be very useful tools for reliable long‐term predictions. Copyright © 2001 John Wiley & Sons, Ltd. 相似文献
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抛物型方程和Poisson方程参数控制反问题的求解及其应用 总被引:1,自引:1,他引:0
提出用脉冲谱技术(PST)求解抛物型方程参数控制反问题和边界元-优化法求解Poisson方程参数控制反问题;推导了算式,给出了计算程式,并分别用这两种方法反演了非均质矩形土坝的渗透系数和新安江大坝坝基帷幕区补强前后的渗透系数.计算结果表明,用脉冲谱法和边界元-优化法求解参数控制反问题是行之有效的,应用于坝工渗流计算,可基本解决坝体和地基渗透系数的反演问题,其优点是,所需附加信息量少,无需大面积的钻孔取样工作,可节省大量投资. 相似文献
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This paper is devoted to the formulation of the direct differentiation method and adjoint state method in quasi‐static linear poroelasticity. We derive the strong and weak formulation of both methods and discuss their solutions using the finite element method. The techniques are illustrated and tested on two numerical examples for the case of isotropic and homogeneous material. The presented formulations can be extended to more complex behaviour in poromechanics. Copyright © 2004 John Wiley & Sons, Ltd. 相似文献