贵州省盘县陇英大地金矿床成矿地质特征及找矿评价

通过对贵州省盘县陇英大地金矿床金矿矿区地层、构造、矿体特征、矿石特征等方面的研究,初步认为该区金矿体主要产于峨眉山玄武岩组一段及二段玄武质熔岩底部,受断层旁侧的节理、裂隙控制金矿体在断层破碎带内呈顺层和穿层两种状态产出。此外,通过对贵州省盘县地区峨眉山玄武岩底部和玄武岩之间的凝灰岩中的微细粒浸染型金矿床的研究,认为此类金矿的区域分布受控于峨眉山玄武岩及其边缘凝灰岩分布区;区域性控矿构造如扬子陆块西南缘的深部构造和区域性深大断裂,控制了金矿成矿及矿体的形成和分布,局部性构造决定了矿体的空间分布及产出特征。最后提出在该区寻找相同类型金矿的找矿标志及找矿远景。     

地平式跟踪系统过顶问题研究

地平式光电系统过顶跟踪时需要很大的方位角速度,在目标通过天顶瞬间方位角速度达到无穷大,导致地平式系统在天顶附近存在跟踪盲区。为此,对天顶跟踪盲区进行了分析,提出盲区范围计算公式,并分析了天顶附近目标图像旋转问题。从软硬件两种角度提出过天顶跟踪目标的方法,即倾斜方位轴方法和程序引导方法,通过比较二者的优缺点给出具体应用范围。     

基于神经网络的面波迭代反演应用研究

根据滩浅海近地表结构特征,尝试利用地震记录中的面波进行近地表结构研究,以便了解滩浅海地区的近地表地层介质结构变化,为深层油气勘探提供准确的低降速带资料.针对面波频散反演已有方法存在的不足,引入一种基于BP神经网络的迭代反演方法对面波的频散曲线进行拟合迭代,用于反演预测滩浅海低降速带地层参数.由于神经网络具有很强的自学习、自适应、自组织和容错能力,它的反演预测能力非常强大,能够较精确地预测出所要求解的目标数据,同时结合传统迭代反演方法的优点,增强了该方法的反演预测能力.通过对滩浅海近地表结构模型试算,获得好的效果,同时进一步对实际记录进行了计算,也取得了比较满意的结果.     

由平方剩余差集与差集偶构造二元ZCZ序列偶集

提出了一种利用平方剩余差集(4t-1,2t-1,t-1) DS和差集偶(N,p,q,e,λ) DS
P构造二元零相关区(ZCZ)序列偶集的方法. 由平方剩余差集获得其二元特征序列,并由差集
偶获得其特征二元序列偶,将二者进行交织构造生成一类新的二元ZCZ序列偶集. 该方法解
决了现有二元ZCZ序列偶集构造中含有少量非二元元素的问题,通过选择适当的差集偶可使构造的二元ZCZ序列偶集在失配滤波检测中获
得较高的能量效率,从而提高了通信性能.     

高精度磁测在圈定旅游开发区中的应用

随着新测量方法的开发和利用,以及新的数据处理和资料解释技术[1]的提高,使得高精度磁法勘探的应用范围越来越广,本文利用磁异常研究岩脉的赋存状态[2],确定了溶洞存在的范围,为圈定旅游开发区提供了重要依据。     

快硬硫铝酸盐水泥浆体-矾土集料界面的微结构

用XRD层析技术、SEM/EDAX和DTA等手段测定了矾土集料-硬化硫铝酸盐水泥浆体界面区的组成、微结构及形貌,同时用XRD线宽法测定了界面区中AFt晶体尺寸及其分布。研究发现,在矾土界面区中,AFt主要以胶体形态富集,C(?)H_2以晶体形态富集,界面区的厚度为70μm左右。为此,提出了矾土集料界面区微结构的形成机理。     

ANALYTICAL SOLUTIONS FOR PEELING USING BEAM-ON-FOUNDATION MODEL AND COHESIVE ZONE

When fibrillation occurs during peeling, the normal stress in the adhesive may gradually reduce to zero at the peel front. The shear stress also reduces to zero. Classical beam-spring (or beam-on-elastic-foundation) models do not yield solutions that have these properties. With the use of a beam-on-foundation model combined with a cohesive zone in the neighborhood of the peel front, these properties can be satisfied. In order to obtain analytical solutions, peel tests are considered in which the backing has a small slope and is linearly elastic in the adhered region, and the traction law is assumed to be piecewise linear. Cases are considered with only normal stresses in the adhesive (mode I), only shear stresses (mode II), and both stresses coupled (mixed-mode behavior). Analytical solutions are obtained for displacements of the backing, forces in the backing, and stresses between the adhesive and the backing.     

广州地区大型办公类公共建筑能耗调查与分析

通过对广州市有代表性的写字楼进行3个年度全年能耗抽样调查,分析了2栋大型办公类公共建筑全年的建筑能耗组成和变化规律。指出此两栋大型办公类建筑按实际使用面积计算的全年平均总能耗为149.3 kWh/m2和115 kWh/m2,全年空调能耗占建筑总能耗的比例分别为49.2%和38.5%。由于所使用的能耗调查方法详细,调查对象具有代表性,因此,能耗分析结果可作为广州地区办公类公共建筑能耗数据库的一部分或为其提供参考。此外,通过和其他相关文献研究结果的对比,指出了夏热冬暖气候区建筑节能的途径。     

Micro-computed tomography scanning approaches to quantify,parameterize and visualize bioturbation activity in clogged streambeds: A proof of concept

Fine particle clogging and faunal bioturbation are two key processes co-occurring in the hyporheic zone that potentially affect hyporheic exchange through modifications in the sediment structure of streambeds. Clogging results from excessive fine sediment infiltration and deposition in rivers, and it is known to decrease matrix porosity and potentially reduce permeability. Faunal bioturbation activity may compensate for the negative effect of clogging by reworking the sediment, increasing porosity, and preventing further infiltration of fines. Although both processes of clogging and bioturbation have received significant attention in the literature separately, their combined effects on streambed sediment structure are not well understood, mostly due to the lack of a standard methodology for their assessment. Here, we illustrate a novel methodology using X-ray computed tomography (CT), as proof of concept, to investigate how, together, clogging and bioturbation affect streambed porosity in a controlled flow-through flume. By visualising gallery formations of an upward conveyor macroinvertebrate; Lumbriculus variegatus as a model species, we quantified bioturbation activity in a clogged streambed, focusing on orientation, depth, and volume at downwelling and upwelling areas of the flume. Gallery creation increased the porosity of the streambed sediment, suggesting a potential improvement in permeability and a possible offset of clogging effects. We illustrate the promising use of X-ray CT as a tool to assess bioturbation in clogged streambeds, and the potential role of bioturbation activity supporting hyporheic exchange processes in streambeds, warranting further studies to understand the extent of bioturbation impacts in natural systems.     

存在高渗透区的黏土心墙土石坝渗流稳定性分析

黏土心墙土石坝是重要的挡水建筑物,心墙的低渗透性可以大幅降低坝体水力梯度,减少坝体发生渗透破坏的风险。然而心墙的质量问题（如局部高渗透区）会影响坝体的渗透稳定性,甚至酿成管涌溃坝等严重后果。以瀑布沟心墙土石坝为原型开展坝体渗流大型水槽模型试验,并结合有限元数值模拟方法研究高渗透区对坝体内部渗流场和渗流稳定性的影响。试验表明高渗透区域将改变心墙的渗流场,成为优势渗流通道,导致高渗透区域附近孔压值大幅上升,同时高渗透区域的存在将显著提升坝体渗漏速率。试验与模拟结果一致表明,随着高渗透区域逐步上移,高渗透区所在位置处的孔隙水压力增大,坝体渗漏量减小。高渗透区和心墙的渗透系数增加都会使心墙孔压值和渗漏量增加;随着高渗透区的渗透系数的增大,心墙坝渗流稳定性系数降低,导致坝体稳定性下降;随着心墙渗透系数的增大,高渗透区水力梯度略微减小,但心墙整体临界水力梯度下降,坝体稳定性降低。所得结论可为基于监测数据反演分析心墙的质量问题和评估坝体的安全性能提供依据。