RSM－16H动测仪在面波法岩土体检测中的应用

对在岩土体检测中推广应用的新技术──瑞雷面波法作了简述，介绍了ＲＳＭ－１６Ｈ型动测仪对稳态和瞬态面波资料的处理实例，并提出了对该仪器在面波测量中的软件改进建议。     

Steady- and transient-state inversion in hydrogeology by successive flux estimation

A calibration method to solve the groundwater inverse problem under steady- and transient-state conditions is presented. The method compares kriged and numerical head field gradients to modify hydraulic conductivity without the use of non-linear optimization techniques. The process is repeated iteratively until a close match with piezometric data is reached. The approach includes a damping factor to avoid divergence and oscillation of the solution in areas of low hydraulic gradient and a weighting factor to account for temporal head variation in transient simulations. The efficiency of the method in terms of computing time and calibration results is demonstrated with a synthetic field. It is shown that the proposed method provides parameter fields that reproduce both hydraulic conductivity and piezometric data in few forward model solutions. Stochastic numerical experiments are conducted to evaluate the sensitivity of the method to the damping function and to the head field estimation errors.     

瞬变电磁测深法在砂岩型铀矿找矿选区中的应用效果

本文以近几年来配合1∶25万带钻区调工作开展的瞬变电磁测深工作为基础,总结了该方法在铀矿区调阶段的应用效果。认为瞬变电磁测深资料有利于判断地下水动力条件及铀矿化的成矿有利区;大范围的瞬变电磁测深工作更适合于在戈壁沙漠区工作,有利于区调选区工作的进行,可达到缩小靶区和提供钻探设计依据的目的,在砂岩型铀矿找矿工作中有推广意义。     

中心回线瞬变电磁探测的一种快速解释方法

分析了中心回线装置激发的电磁场在晚期与平面电磁波的传播特征,通过时-频转换将TEM数据转换成平面波场数据,构建了关于反射函数的M×N阶欠定方程组。用线性规划法解出反射函数序列q_m,大量模型的反演结果与理论值误差很小。以q_m为参数绘制出电磁响应时间剖面图,从而实现了TEM快速成像解释。成像剖面清楚地反映了断面的地电特征。实测资料的处理结果说明了方法的实用性。     

瞬态瑞雷面波勘探技术在工程勘察评价中的应用

文章介绍了瞬态瑞雷面波勘探技术的理论基础和勘探原理、工作方法、资料的整理与解释，并结合工程实例说明瞬态面波勘探技术的应用效果。     

洞内瞬变电磁(TEM)探测技术研究

近年来,隧道超前探测、泄洪洞病害部位探测、矿洞内矿体方位及含水等地下洞体内的探测需求变得越来越迫切,但由于洞内工作面狭小、不是地表的1/2空间、潮湿、金属等低阻体干扰等的特殊工作条件,较难进行有效探测,从而使洞内探测成为一大难题;根据瞬变电磁(TEM)方法的特点,设计了适用于洞内探测的装置,开发了相应的包含数据组合滤波、弱信息增强处理、异常分离等数据预处理方法在内的处理程序,较好地解决了上述问题,并取得了良好的应用效果。     

综合物探解决黄土区煤田复杂地质问题

山西某矿位于构造堆积盆地，属黄土匠陵地貌，区内被第四系黄土覆盖，为解决该矿地质构造及水文地质问题，采用三维地震勘探与瞬变电磁法、直流电测深法相结合的勘探方案。利用三维地震勘探解决目的层赋存形态及其地质构造问题，再利用瞬变电磁法进行平面控制，以使平面及深度解释误差达到勘探要求；应用直流电测深法及瞬变电磁进行勘探，在正反演解释的基础上对其资料综合分析、对比，并结合三维地震资料，确定地质构造的富水及导水性。     

Western Pacific Jet Stream Anomalies at 200 hPa in Winter Associated with Oceanic Surface Heating and Transient Eddy Activity

The relationships between the 200-hPa westerly jet stream anomalies over the East Asian coastal water- western Pacific(WPJS),and the oceanic surface heating and synoptic-scale transient eddy(STE)activity anomalies over the North Pacific in wintertime are examined by using ERA-40 and NCEP/NCAR reanalysis data.The analysis demonstrates that the surface heating and the STE anomalies have different patterns, corresponding to the three WPJS anomalous modes,respectively.In the first WPJS anomalous mode,the WPJS main part shows no robust anomaly.The anomalous westerly wind,occurring over the mid-latitude central-eastern Pacific past the date line is associated with the anomalous heating presenting both in the tropical central-eastern Pacific past the date line and the center of the North Pacific basin.Meanwhile,the STE anomaly appears around the region of the anomalous zonal wind.The fluctuation in jet strength shown in the second WPJS mode is strongly related to the heating anomaly in the Kuroshio Current region and the STE anomaly in the jet exit region.The third mode demonstrates a northward/southward shift of the WPJS,which has a statistical connection with a south-north dipolar pattern of the heating anomaly in the western North Pacific separated at 35°N.Meanwhile,the STE spatial displacement is in conjunction with jet shifts in the same direction.The heating anomaly has a close connection with the atmospheric circulation, and thus changes the mid-latitude baroclinicity,leading to the STE anomaly,which then reinforces the WPJS anomaly via internal atmospheric dynamics.     

Identification method of weak seismic phases on the basis of wavelet packet transform

This paper describes a sort of new method identifying seismic phase by the name of wavelet packet transform. Perfectness and development of the wavelet packet transform is based upon the idea of its multiscale analysis. The method of wavelet packet transform can depict the anomalous changes information of transient spectra of seismic wave onset, and come true the target of identifying seismic phase especially weak seismic phase. Then this paper presents discriminating examples of simulating digital signals and actual seismic phase. Compared with conventional seismic phase discrimination, studied results show that the wavelet packet transform method is an available tool of weak signal analyses, and have unexampled merits and attractive application foreground. This research gets hold of Higher School Doctor Scientific Research Foundation (No. 157 WJ0704 9435611) and supported by the National Natural Science Foundation (No. 49474211).     

瞬变电磁法二维逆时偏移

本文简要介绍了电磁偏移的基本原理和低频滤波的偏移处理方法,并详细论述了最佳极值时刻T的求取方法。电磁偏移以斯特莱顿-朱型积分为理论基础,借助于无限均匀介质中的格林函数,描述了似稳电磁场在下半空间的传播过程。利用电磁偏移方法处理TEM资料,能够较准确地确定局部导电地质体的空间位置,处理速度快,解释结果形象。