FAST APPROXIMATE INVERSION OF MAGNETOTELLURIC(FAIMT) DATA FOR A HORIZONTALLY LAYERED EARTH WITH NEAR-SURFACE INHOMOGENEITIES

IwrRODUcrIONNearsurface2-Dand3-DinhomogeneousdistortionsinMTdatamakeitdimculttointerpretMTdataevenwhentheregionalorbasinstruCturescanbetreatalas1-dfornsionalnyohmann,l975,Weide1t,l975,Wannamakeretal.,l984,LaTormcaetal.,l986,Zhang,l987,TorresWhrdinetal.,l992).Inthelasttwentyyears,2-Dand3-DmodelinghavebeenaanmPlishedbyusingnumricalmethods.Afteranalyringthesefor-wardmodelingresultS,wenowdeariyunderstandthemaorphySica1meCanisrnsasultingfromthesedistortionsofnear6urfaceinhomogeneities(Pa…     

CALCULATION OF VARIABLE DRAG AND HEAT-TRANSFER COEFFICIENTS IN METEORIC PHYSICS EQUATIONS

The conservation of the ablation parameter is one of the main assumptions of the classical physical theory of meteors (PTM). But this value does vary dramatically on meteoroids trajectories for the most part of them. The drag and heat-transfer coefficients in the basic equations of PTM are considered from the gasdynamical point of view and mathematically modeled in the present paper. Analytical approximations of the drag and heat transfer coefficients valid for any flow regimes and separate approximation of the drag coefficient for free-molecule regime are offered and discussed. They use the Reynolds number as the main parameter characterizing flow regimes. The variations of coefficients result in the variation of the ablation parameter by 100% for meteoroids, passing all the flow regimes. The importance of correct calculation of the coefficients for meteoroids motion modeling was demonstrated by the numerical examples.     

Warm anisotropic inflation with bulk viscous pressure in intermediate era

The aim of this paper is to study the warm inflation during intermediate era in the framework of locally rotationally symmetric Bianchi type I universe model. We assume that the universe is composed of inflaton and imperfect fluid having radiation and bulk viscous pressure. To this end, dynamical equations (first model field equation and energy conservation equations) under slow-roll approximation and in high dissipative regime are constructed. A necessary condition is developed for the realization of this anisotropic model. We assume both dissipation and bulk viscous coefficients variable as well as constant. We evaluate entropy density, scalar (tensor) power spectra, their corresponding spectral indices, tensor–scalar ratio and running of spectral index in terms of inflaton. These cosmological parameters are constrained using recent Planck and WMAP7 probe.     

海洋条件下目标-背景对比度计算分析

推导了海洋条件下目标-背景对比度的计算公式,根据辐射传输方程,采用Eddington近似方法求解,建立了海洋条件下目标-背景对比度的表达公式。计算并分析了太阳高度、观测者角度、海水体衰减系数及目标所处深度对目标-背景对比度的影响。文中得出如下结论:垂直方向侦查时,太阳高度角在40°左右条件下的目标-背景对比度最大,最容易侦查到水下目标;目标-背景对比度随目标所在深度增大而减小,随海洋体衰减系数的增加而降低;太阳高度角为90°、观测者天顶角余弦在0.8~0.9范围时的目标-背景对比度存在较大尖峰值。研究结果为光学探测水下目标及水下航行器反光学探测提供理论支撑。     

基于直射线近似的一步法基准面校正方法研究

地形基准面校正算子（Topographic Datuming Operator,以下简称TDO）是一种基于直射线近似得到的基准面延拓算子.TDO可以视为是两步法波动方程基准面校正与常规静校正之间的一种过渡算法,该方法的最大特点在于它可以基于共炮点道集将炮点和检波点同时延拓到给定的水平基准面,因此相对于常规的两步法叠前波动方程基准面校正,TDO方法可以认为是一种更为高效的一步法基准面延拓方法.本文基于理论与实际数据论证了上述观点.     

Wave period distributions in non-Gaussian mixed sea states

The wave period probability densities in non-Gaussian mixed sea states are calculated by utilizing a transformed Gaussian process method. The transformation relating the non-Gaussian process and the original Gaussian process is obtained based on the equivalence of the level up-crossing rates of the two processes. A saddle point approximation procedure is applied for calculating the level up-crossing rates in this study. The accuracy and efficiency of the transformed Gaussian process method are validated by comparing the results predicted by using the method with those predicted by the Monte Carlo simulation method.     

“逐步逼近式”找水方法及其在缺水地区水文地质勘查中的应用

在缺水地区开展找水水文地质勘查工作,如何提高成井供水效率,科学的找水方法至关重要。笔者介绍近10年来在我国西部地区300多个缺水村镇找水水文地质勘查实践中,总结出＂逐步逼近式＂找水方法。主要包括利用前人调查成果通过预研究确定找水方向、应用遥感解译方法圈定找水靶区、辅以简易快速物探方法的中比例尺地面调查确定富水地段、详细地面调查与物探组合技术结合优化确定钻探孔位、不同含水层选择相应钻探方法和成井工艺5个步骤。以及针对不同找水区在遥感数据源选择、简易快速物探方法应用与多方法有效组合探测的技术要点。