利用BSTEM模型分析库岸边坡形态对其稳定性的影响

库岸稳定性取决于最大崩塌临界机制的驱动力和抵抗力的平衡,二者的平衡又取决于库岸边坡形态、岩土组成、水流浪涌特征、植被覆盖等.边坡形态是库岸稳定性的基本条件,主要指标有坡度、岸高及坡面形态.以三峡库区忠县石宝镇段为例,利用BSTEM模拟分析库岸边坡形态对其稳定性的影响,从而得到如下结论,研究库岸坡形形态对其稳定性的影响,...     

Comparison of theoretical and experimental wall pressure wavenumber-frequency spectra for axisymmetric and flat-plate turbulent boundary layers

The measurement and analysis of turbulent boundary layer wall pressure fluctuations using a wavenumber filter of sensors provide quantitative knowledge of turbulence physics. In addition, the sources of flow-induced noise and vibration for towed SONAR arrays can be determined. An axisymmetric turbulent boundary layer can have significantly different features than those of a comparable flat-plate boundary layer. Here, a detailed comparison of the distribution of wall pressure energy in both wavenumber and frequency between flat-plate and thick axisymmetric boundary layers is presented. The background theory of wavenumber-frequency spectra and state-of-the-art models for flat-plate boundary layers are discussed. The widely used model of Chase (1987), valid for flat-plate boundary layers over a wide range of Reynolds numbers, is used and combined with a sensor response function to allow the effects of spatial averaging to be considered. It is demonstrated that when measured boundary layer parameters for the axisymmetric case are used in the Chase flat-plate model, the results accurately predict the axisymmetric boundary layer wall pressure measurements.     

球面格网系统特征分析及比较

球面格网系统是一种新型栅格数据模型。在全面检索和分析前人相关研究成果的基础上,将球面格网系统分成4种类型:基于经纬线划分的格网系统、基于正多面体划分的格网系统、基于Voronoi划分的格网系统和混合格网系统;并针对各种不同类型的格网,分析了同级格网单元的空间几何特征及不同级别格网之间的层次嵌套等特性。通过对比分析,给出不同格网系统的优缺点及其适用领域,认为不存在满足所有需求的通用的格网系统,相关应用只能针对具体情况,选用最适宜的格网系统。     

主动铰接型盾构机自动导向系统测量与姿态精密解算方法

主动铰接型盾构机在曲线隧道开挖中应用广泛,其盾构姿态的精密解算是盾构机自动导向系统的核心功能,也是盾构掘进中进行盾构机实时纠偏的前提和基础。国内外盾构机自动导向系统提供商对自身盾构姿态计算原理和方法保密的现状,给盾构机姿态人工复核和盾构施工带来了较大困难。本文在研究两款国产盾构机和日本演算工坊棱镜法自动导向系统的基础上,利用立体几何和空间投影变换原理,提出了主动铰接型盾构机姿态精密解算方法,给出详细推导计算公式。通过对多台盾构机在不同隧道线型内多组姿态坐标数据的计算和对比,验证了该盾构姿态精密解算方法的正确性。     

无人机倾斜摄影铁路轨道线高精度自动重建

针对既有铁路测绘上线难、作业效率低及测量精度不足的问题,本文提出了一种基于无人机多视图几何原理的铁路轨道线高精度重建方法。首先从无人机影像上提取线特征;然后采用像方测度获得候选匹配线,基于物方距离测度进行Powell优化,获得精确的钢轨线匹配结果;最后,将影像钢轨线匹配结果作为观测值,以钢轨线反投影距离作为测度,最小二乘优化物方钢轨直线段坐标。试验结果表明,本文方法实现了影像轨道线自动匹配与高精度平差解算,像方反投影残差优于0.5像素,轨距和高程的内符合精度分别为0.006和0.005 m。解算成果的平面高程绝对定位精度可达到2 cm左右,平差模型收敛性良好,可以满足工程应用的需要。     

Regional flow perturbation folding within an exhumation channel: A case study from the Cycladic Blueschists

Kilometre-scale cylindrical folds and associated parasitic folds that trend at small angles to the transport lineation are analysed along a 100-km-long transport-normal segment of the Cycladic Blueschists in an attempt to reconstruct the 3D structural architecture within an exhumation channel. Reversals in the polarity of both fold vergence and the hinge/lineation obliquity occur in a flow-normal direction, defining transport-parallel culmination and depression surfaces that root downwards onto an underlying detachment. Fold patterns generated around culmination and depression surfaces support models of flow-perturbation folding where folds initiate at small angles or sub-parallel to transport in response to wrench-dominated differential shearing. Successive culmination and depression surfaces are separated from one another by along strike distances of ∼20 km, although atypical fold geometries developed in the flanks of major culmination and depressions follow their own patterns, revealing that smaller perturbations occur within the larger scheme. Major culminations are interpreted to reflect regions of surging flow marked by increased velocity during exhumation, whilst the opposite is true for depressions. This behaviour implies that on a regional scale, differential shear varies laterally in an irregular-sinusoidal manner defining areas of relative high and relative low displacement within the exhumation channel.     

岩溶热储井间连通性的示踪研究

岩溶热储储层的不均匀性强,采灌井之间的连通性不易确定。示踪技术可以将运移参数量化,有效刻画储层流体的特征,研究回灌井和开采井之间的水力联系,包括导水通道,流体流速等信息,对长期回灌可能引起的开采井的冷却进行预测,是岩溶热储井间连通性研究十分有效的技术。本文以华北牛驼镇地热田雄县地区为例,针对蓟县系雾迷山组岩溶热储,采用荧光素钠示踪剂,进行了1口井注入,10口井观测的群井示踪试验。采用裂隙介质溶质运移模型,对示踪试验数据进行了解释,得到优势通道的长度、渗透流速、纵向弥散度、回收率等储层性质,获得了试验区内采灌井之间的连通特征。对调整采灌井布局提出了建议。     

Relationship between the ionospheric conductance, field aligned current, and magnetopause geometry: Global MHD simulations

The role of the ionospheric conductance in the solar wind-magnetosphere coupling is studied using global MHD simulations. The simulations with varying conductance and a constant solar wind input show that the field-aligned currents, whose magnitude depends on the ionospheric conductance, affect the size of the magnetopause at the flanks by increasing the local magnetic pressure and thus altering the surface equilibrium at the magnetopause. A current system that generates the magnetic stresses required to account for the location and geometrical structure of the magnetosphere observed in the simulations is proposed.     

A Class of higher dimensional spherically symmetric cosmological model in Lyra geometry

Exact analytical solutions are obtained for a higher dimensional spherically symmetric inhomogeneous metric in presence of a mass-less scalar field with a flat potential within the framework of Lyra geometry. Assuming a homogeneous scalar field, we have shown that the metric can be reduced to a generalized FRW type.     

Three-dimensional Geometry and Kinematics of the Changning Anticline in the Southern Sichuan Basin

In this study, we aim to clarify the structural characteristics and deformation process of the Changning anticline. We carefully interpret 38 two-dimensional (2D) seismic profiles in the study area and establish three-dimensional (3D) geometric and quantitative kinematic models of the Changning anticline. This study shows that the basement fault controls the formation of the Changning anticline. The fault slope of the main fault in the basement shows ‘steep in the upper and gentle in the lower’ structural characteristics vertically, possessing obvious segmentary characteristics transversely and presents the overall characteristics of ‘steep in the east and gentle in the west’. Further analysis shows that the Changning anticline proceeds west and terminates at the boundary defined by current surface features but gradually disappears westward across the Mt. Huaying fault zone. Furthermore, we identified that deformation of the Changning anticline began during the early Yanshanian movement period. Under compressional stress from the southeast, the anticline slid forward along the basement fault until the end of the Yanshanian movement period, when the dominant WNW–ESE structure gradually emerged. Since the Himalayan movement period, a series of NE-trending structures have been formed in the anticline, owing to multi-directional compressive stress.