水平循环荷载引起的砂土沉陷-致密作用对刚性桩承载力的影响分析

为研究砂土中刚性桩基础在循环荷载作用下的承载力演化规律,提出了一种循环后单桩承载力的评估方法.首先,基于沉陷坑与致密区域土体的质量守恒原理,量化了由沉陷引起的土体参数变化;然后,根据API规范中的砂土水平土抗力-位移模型计算循环前后的单桩承载力;最后,提出了循环后单桩承载力的评估模型,并对沉陷坑尺寸、土体初始相对密实度和致密区域模式等因素进行对比分析.结果 表明:单桩承载力随沉陷坑的发展不断增大;对于松砂、中密砂和密砂,循环后的单桩承载力可分别提高约3.0、1.5、1.2倍,提高幅值随相对密实度的增大而降低;2种土体变形模式中,单锥模式相比于双锥模式更符合真实的致密区域形态.     

Dendrite growth and micromechanical properties of rapidly solidified ternary Ni-Fe-Ti alloy

The rapid solidification of undercooled liquid Ni_(45)Fe_(40)Ti_(15)alloy was realized by glass fluxing technique.The microstructure of this alloy consists of primaryγ-(Fe,Ni)phase and a small amount of interdendritic pseudobinary eutectic.The primaryγ-(Fe,Ni)phase transferred from coarse dendrite to fragmented dendrite and the lamellar eutectic became fractured with the increase of undercooling.The growth velocity ofγ-(Fe,Ni)dendrite increased following a power relation with the rise of undercooling.The addition of solute Ti suppressed the rapid growth ofγ-(Fe,Ni)dendrite,as compared with the calculation results of Fe-Ni alloy based on LKT model.The microhardness values of the alloy and the primaryγ-(Fe,Ni)phase increased by 1.5 times owing to the microstructural refinement caused by the rapid dendrite growth.The difference was enlarged as undercooling increases,resulting from the enhanced hardening effects on the alloy from the increased grain boundaries and the second phase.     

异质多智能体系统在固定拓扑下的分组一致性

研究了异质多智能体系统的分组一致性,针对固定通信拓扑情况,提出了一种基于邻接信息的分布式控制协议,并通过李雅普诺夫理论,推导出异质多智能体系统实现分组一致性的充分条件.最后利用数值仿真验证了理论分析的正确性.     

重申柏拉图——正义之城的美学问题

关于柏拉图美学已属老生常谈,但旧学可以新说.事实上,以"放逐诗人"闻名于世的这位哲人最初的人生志愿,是成为一位荷马那样的诗人.意识到这一点有助于我们重新认识柏拉图美学的价值所在.在某种意义上,他的政治哲学转型意味着一种以"正义论"为核心的伦理美学的奠基.所谓"正义之城的美学问题",也就是作为"美本身"的"终极善"的逻辑确定性何以认定的困惑.围绕这个问题展开的相关讨论,对于当下普遍缺乏真正的"问题意识"的中国式美学研究,无疑具有重要的启发意义.     

Gas Chromatography Determining BTEX in Water

随着国民经济的快速发展,工业产业得到了较大程度的发展,在创造经济效益的同时也带来了环境危害.其中,苯系物是水资源中最重要的污染物之一.文章就气相色谱法对饮用水中苯系物测定进行了分析.     

关于生物工程技术与水污染控制的思考

文章概括介绍生物工程技术的概念、特点、发展状况以及在废气处理和固体废物处理中的应用,重点介绍生物工程技术在污水处理中的应用。     

Atomic layer deposition on Pd nanocrystals for forming Pd-TiO2 interface toward enhanced CO oxidation

Pd typically exhibits relatively low catalytic activity in CO oxidation, as CO is apt to be adsorbed on Pd to poison the surface for O2 activation. In this Letter, we report that this limitation can be overcome by integrating Pd with TiO2. The TiO2 was coated on Pd nanocubes with a controllable thickness using atomic layer deposition (ALD) method. Given the different work functions of TiO2 and Pd, the electrons in TiO2 semiconductor will flow toward Pd. With the electron density increased on Pd, the adsorption of CO to Pd will be weakened while the oxygen activation can be facilitated. Meanwhile, the interface-confined sites at Pd-TiO2 may further enhance the oxygen activation. As the species adsorption and activation are strongly correlated with electron density, the performance of Pd-TiO2 in CO oxidation turns out to depend on the TiO2 thickness, which determines the number of transferred electrons, within a certain range (<1.8 nm). This work provides a new strategy for enhancing catalytic performance through tailoring charge densities in hybrid catalysts.     

基于混合DBN的海上编队通信链路威胁估计

针对海上编队通信链路威胁估计涉及因素多、知识表示与推理存在不确定性等问题,分析了海上编队通信链路威胁要素,依据要素间因果关系建立了通信链路威胁估计的混合动态贝叶斯网络(DBN)模型,提出了混合DBN模型中连续型网络节点变量的学习方法。仿真分析证实了该方法的有效性和可操作性。     

Tibetan plateau aridification linked to global cooling at the Eocene-Oligocene transition

Continental aridification and the intensification of the monsoons in Asia are generally attributed to uplift of the Tibetan plateau and to the land-sea redistributions associated with the continental collision of India and Asia, whereas some studies suggest that past changes in Asian environments are mainly governed by global climate. The most dramatic climate event since the onset of the collision of India and Asia is the Eocene-Oligocene transition, an abrupt cooling step associated with the onset of glaciation in Antarctica 34 million years ago. However, the influence of this global event on Asian environments is poorly understood. Here we use magnetostratigraphy and cyclostratigraphy to show that aridification, which is indicated by the disappearance of playa lake deposits in the northeastern Tibetan plateau, occurred precisely at the time of the Eocene-Oligocene transition. Our findings suggest that this global transition is linked to significant aridification and cooling in continental Asia recorded by palaeontological and palaeoenvironmental changes, and thus support the idea that global cooling is associated with the Eocene-Oligocene transition. We show that, with sufficient age control on the sedimentary records, global climate can be distinguished from tectonism and recognized as a major contributor to continental Asian environments.