层状地基任意形状刚性基础动力响应求解

提出了基于积分变换、对偶方程与精细积分算法求解多层地基任意形状刚性基础的动力刚度问题. 首先在频率波数域内圆柱坐标体系中利用圆形微元的对称与反对称特性建立多层地基中格林影响函数的波动方程,然后将应力和位移关系表示成对偶形式进行精细积分求解以提高计算精度和稳定性. 再将任意形状刚性基础与地基的交界面离散化为一系列圆形微元,利用格林影响函数建立其平动与转动动力刚度的矩阵方程. 该求解方法高效、准确并且计算稳定,适于任意复杂多层地基任意形状基础动力刚度的计算.      

Certifying algorithms for recognizing proper circular-arc graphs and unit circular-arc graphs

We give two new linear-time algorithms, one for recognizing proper circular-arc graphs and the other for recognizing unit circular-arc graphs. Both algorithms provide either a model for the input graph, or a certificate that proves that such a model does not exist and can be authenticated in O(n) time. No other previous algorithm for each of these two graph classes provides a certificate for its result.     

Macro-performance of multilayered thermoelectric medium

The effective properties of thermoelectric composites are well known to depend on boundary conditions, which causes the macro performance of thermoelectric composite to be difficult to assess. The overall macro-performance of multilayered thermoelectric medium is discussed in this paper. The analytical solutions are obtained, including the heat flux, temperature,electric potential, and the overall energy conversion efficiency. The results show that there are unique relationships between the temperature/electric potential and the electric current/energy flux in the material, and whether the material is independent of or embedded in thermoelectric composites. Besides, the Peltier effect at the interface can significantly improve the overall energy conversion efficiency of thermoelectric composites. These results provide a powerful tool to analyze the effective behaviors of thermoelectric composites.     

遗传算法设计多层微波吸收材料的结构

本文用遗传算法优化设计多层结构的电磁波吸收材料,通过优化设计和数值计算给出了材料的结构参数,并对优化结果的多种约束条件（总厚度、吸收带宽、反射率大小）进行了加权评估,从而得到了多种介质材料匹配后具有优良吸波特性的吸波材料．     

A Hyperspectral Image Classification Approach Based on Feature Fusion and Multi-Layered Gradient Boosting Decision Trees

At present, many Deep Neural Network (DNN) methods have been widely used for hyperspectral image classification. Promising classification results have been obtained by utilizing such models. However, due to the complexity and depth of the model, increasing the number of model parameters may lead to an overfitting of the model, especially when training data are insufficient. As the performance of the model mainly depends on sufficient data and a large network with reasonably optimized hyperparameters, using DNNs for classification requires better hardware conditions and sufficient training time. This paper proposes a feature fusion and multi-layered gradient boosting decision tree model (FF-DT) for hyperspectral image classification. First, we fuse extended morphology profiles (EMPs), linear multi-scale spatial characteristics, and nonlinear multi-scale spatial characteristics as final features to extract both special and spectral features. Furthermore, a multi-layered gradient boosting decision tree model is constructed for classification. We conduct experiments based on three datasets, which in this paper are referred to as the Pavia University, Indiana Pines, and Salinas datasets. It is shown that the proposed FF-DT achieves better performance in classification accuracy, training conditions, and time consumption than other current classical hyperspectral image classification methods.     

层状填土主动土压力计算方法的改进

针对现有层状填土主动土压力计算方法中存在的局限性和不合理性,对原有计算方法进行了拓展和改进.在平面滑裂面假设下,充分考虑墙后分层填土的滑动变形协调条件以及墙背倾斜、填土表面有附加荷载、填土黏聚力、填土与挡土墙墙背接触面上的黏着力等一般情况,建立分层填土的主动土压力关于滑裂面倾角的计算表达式,有效地改进了分层法,增加了实用性,为工程中挡土墙土压力设计提供了更为合理、有效的方法.     

渗透各向异性可压缩地基固结的平面应变分析

对多层地基的平面应变固结问题进行了研究,并同时考虑了土体的渗透各向异性和孔隙流体的可压缩性.从平而应变Biot固结的控制方程出发,对时间t,坐标z和x进行Laplace和Fourier变换,建立了地基表面(z=O)和任意深度z处的基本量在Laplauce-Fourier变换域内的传递矩阵关系.利用传递矩阵法,结合土层连续条件和边界条件,并应用Laplace-Fourier逆变换技术,推导出渗透各向异性可压缩多层地基平面应变固结的理论解.基于该解,编制了计算程序,并进行了数值计算.讨论了土体的渗透各向异性、孔隙流体的可压缩性以及地基的分层特性对地基同结的影响,分析结果表明:土体的渗透各向异性、孔隙流体的可压缩性,以及地基的分层特性对地基的固结行为有着重要的影响.     

半覆水相变V形峡谷场地P波入射下的空间地震动散射频域理论解、验证及特征

克服介质相变、峡谷分层且局部地形覆水导致的固有边界值难题,首次推导并得到了半覆水相变V形峡谷场地对P波激励下的散射理论解,验证理论解的正确性,探究了相变界面的有无、入射波频率和入射角对地表位移的显著影响,突出并重点强调了覆水因素对结果影响的不可忽视性。分析结果表明,(1)以经典算例为标准,对比验证了本文理论解的正确性,解释并澄清了峡谷局部可预测性的微小偏差的来源。(2)与未覆水部位相比,峡谷覆水部位表面位移显著增大;与峡谷满水状态相比,相变面的存在使位移增大的初始位置向峡谷中间移动;不同的入射波频率和入射角下,地面运动情况存在显著差异,随着入射角的增大,水平方向的位移逐渐增大,竖直方向的位移逐渐减小。本文研究可为覆水V形峡谷的长大结构多点地震动的合理输入提供基础性研究依据,兼有理论意义与应用价值。     

Effect of the open roof on low frequency acoustic propagation in street canyons

This paper presents an experimental, numerical and analytical study of the open roof effect on acoustic propagation along a 3D urban canyon. The experimental study is led by means of a street scale model. The numerical results are performed with a 2D-Finite Difference in Time Domain approach adapted to take into account the acoustic radiation losses due to the street open roof. An analytical model, based on the modal decomposition of the pressure field in the street width mixed with a 2D image sources model including the reflection by the open roof, is also presented. Results are given for several frequencies in the low frequency domain. The comparison of these approaches shows a quite good agreement until f = 100 Hz at full scale. For higher frequency, experimental results show that the leakage, due to the street open roof, is not anymore uniformly distributed on all modes of the street. The notion of leaky modes must be introduced to model the acoustic propagation in a street canyon.     

The clique operator on circular-arc graphs

A circular-arc graphG is the intersection graph of a collection of arcs on the circle and such a collection is called a model of G. Say that the model is proper when no arc of the collection contains another one, it is Helly when the arcs satisfy the Helly Property, while the model is proper Helly when it is simultaneously proper and Helly. A graph admitting a Helly (resp. proper Helly) model is called a Helly (resp. proper Helly) circular-arc graph. The clique graphK(G) of a graph G is the intersection graph of its cliques. The iterated clique graphKⁱ(G) of G is defined by K⁰(G)=G and Kⁱ⁺¹(G)=K(Kⁱ(G)). In this paper, we consider two problems on clique graphs of circular-arc graphs. The first is to characterize clique graphs of Helly circular-arc graphs and proper Helly circular-arc graphs. The second is to characterize the graph to which a general circular-arc graph K-converges, if it is K-convergent. We propose complete solutions to both problems, extending the partial results known so far. The methods lead to linear time recognition algorithms, for both problems.