三种探测煤层采空区的方法

采空区的存在对矿山生产和工程建设造成极大的安全隐患,采空区探测已成为重要研究课题。笔者结合参加过的工程项目,具体介绍3种探测煤层采空区的方法:井间地震、探地雷达和浅层地震反射波法,并分析比较了它们的优缺点。     

岩土层含水量分层监测系统的研究及应用

开发为地质灾害预测预报所需用的岩土层含水量和渗透力测试仪,并和气候雨量、地质灾害成灾规律联系起来,是我国地质灾害监测预报发展的趋势。岩土层含水量分层监测系统是采用TDR（Time Domain Refiectometry）技术原理、方法研制的仪器,通过波导棒探针发射的电磁波射入岩土层,测量电磁波脉冲从波导棒的起点传播到接收末端的反射电压值,此反射电压值与岩土体本身含水量介电常数有函数关系,经过计算转换为测点岩土体积含水量,实时测量和采集地质灾害岩土层含水量和渗透力参数。介绍了该监测系统的基本原理、主要技术参数、监测工艺技术方法以及现场应用情况。     

中国大陆社会与文化地理学研究领域综观

中国人文地理学的发展经历了一条充满艰辛而又曲折的道路。改革开放以来,中国人文地理学开始回暖,社会与文化地理研究重焕新生,但学科所占位置相对边缘。在“文化转向”的背景下,近年来社会与文化地理学开始呈现出欣欣向荣之势。从文化区、文化传播与文化整合,民族文化地理,文化景观与文化经济,地方和基于地方的政治,边缘群体研究五个方面对中国大陆社会与文化地理研究现状进行综观性的概述和批判性的反思。建立在西方学术话语霸权之上的社会与文化地理学,需要开展建设性的对话并加以研究。未来的社会与文化地理学研究应更加强调跨学科视角和对当前社会问题的关注。     

深地震反射剖面揭示嫩江断裂带中段的深部几何形态与地壳形变

嫩江断裂带对探讨松辽盆地的演化、 与大兴安岭的盆山耦合关系以及兴安地块与松嫩地块的归属问题具有重要研究意义。本文利用深地震反射剖面, 揭示了嫩江断裂带中段的深部几何形态, 表明它目前呈花状构造样式; 它也并非松辽盆地内部的拆离断层, 而是一条超壳断裂, 控制了大兴安岭的物质东移和松辽盆地的中生代沉积; 现今的嫩江断裂带同晚古生代兴安地块与松嫩地块拼合的嫩江构造拼贴带并没有继承性关系; 莫霍面可能在后期的演化过程中扮演了滑脱层的作用, 致使向西俯冲的地幔体向东位移。     

Bragg reflection of water waves by multiple submerged semi-circular breakwaters

This study examines the Bragg reflection of water waves by multiple submerged semi-circular breakwaters. The multipole expansions combined with the shift of polar coordinates are used to develop full linear potential solutions of the problem. In the full solutions, the obliquely and normally incident waves are independently considered. Experimental tests are carried out to measure the reflection and transmission coefficients of the breakwaters at different wave periods and body spacings. The analytical results are in reasonable agreement with the experimental data. The peak reflection coefficient of multiple submerged semi-circular breakwaters and the bandwidth of Bragg reflection are carefully examined by numerical examples. Some significant results for practical application are discussed.     

结合极化分解特征的SVM溢油检测研究

Marine oil spills have caused major threats to marine environment over the past few years.The early detection of the oil spill is of great significance for the prevention and control of marine disasters.At present,remote sensing is one of the major approaches for monitoring the oil spill.Full polarization synthetic aperture radarc SAR data are employed to extract polarization decomposition parameters including entropy(H) and reflection entropy(A).The characteristic spectrum of the entropy and reflection entropy combination has analyzed and the polarization characteristic spectrum of the oil spill has developed to support remote sensing of the oil spill.The findings show that the information extracted from(1–A)×(1–H) and(1–H)×A parameters is relatively evident effects.The results of extraction of the oil spill information based on H×A parameter are relatively not good.The combination of the two has something to do with H and A values.In general,when H0.7,A value is relatively small.Here,the extraction of the oil spill information using(1–A)×(1–H) and(1–H)×A parameters obtains evident effects.Whichever combined parameter is adopted,oil well data would cause certain false alarm to the extraction of the oil spill information.In particular the false alarm of the extracted oil spill information based on(1–A)×(1–H) is relatively high,while the false alarm based on(1–A)×H and(1–H)×A parameters is relatively small,but an image noise is relatively big.The oil spill detection employing polarization characteristic spectrum support vector machine can effectively identify the oil spill information with more accuracy than that of the detection method based on single polarization feature.     

深反射地震数据揭示的拉萨地体北部到羌塘地体南部地壳厚度的变化

由多个地体拼接而成的青藏高原,有着世界上最厚的地壳。在高原中部,从拉萨地体到羌塘地体,穿过班公湖—怒江缝合带(BNS)的地壳厚度变化长期存在争议。本文主要论述从拉萨地体北端横跨BNS到达羌塘地体的深地震反射剖面探测的结果。探测发现了清晰的Moho反射,揭示了拉萨地体—羌塘地体Moho深度和地壳厚度的变化。探测结果表明,在BNS下方Moho深度由南至北出现了6.2 km的急剧减小,并且与BNS向北28 km处的羌塘地体南部比较,地壳厚度变浅了12.5 km。否定了前人对BNS下方Moho存在20 km显著变化的认识。     

Seismic reflection traveltimes in two-dimensional statistically anisotropic random media

Velocity estimation remains one of the main problems when imaging the subsurface with seismic reflection data. Traveltime inversion enables us to obtain large-scale structures of the velocity field and the position of seismic reflectors. However, as the media currently under study are becoming more and more complex, we need to know the finer-scale structures. The problem is that below a certain range of velocity heterogeneities, deterministic methods become difficult to use, so we turn to a probabilistic approach. With this in view, we characterize the velocity field as a random field defined by its first and second statistical moments. Usually, a seismic random medium is defined as a homogeneous velocity background perturbed by a small random field that is assumed to be stationary. Thus, we make a link between such a random velocity medium (together with a simple reflector) and seismic reflection traveltimes. Assuming that the traveltimes are ergodic, we use 2-D seismic reflection geometry to study the decrease in the statistical traveltime fluctuations as a function of the offset (the source–receiver distance). Our formulae are based on the Rytov approximation and the parabolic approximation for acoustic waves. The validity and the limits are established for both of these approximations in statistically anisotropic random media. Finally, theoretical inversion procedures are developed for the horizontal correlation structure of the velocity heterogeneities for the simplest case of a horizontal reflector. Synthetic seismograms are then computed (on particular realizations of random media) by simulating scalar wave propagation via finite difference algorithms. There is good agreement between the theoretical and experimental results.