p型自适应有限单元法及其在岩土工程中的应用

详细地介绍了p型自适应有限元的基本理论及其发展过程,总结了p型自适应有限元的误差估计方法、自适应升阶策略以及加速收敛技术,并将p型自适应有限元法应用于岩土工程的三维弹粘塑性分析、三维动力响应分析以及三维渗流分析中,最后提出了p型自适应有限单元法中亟待解决的问题及今后的研究方向。     

现浇混凝土薄壁管桩复合地基沉降简化计算研究

PCC桩是一种主要应用于软土地基处理的刚性桩。以PCC桩复合地基为研究对象,基于PCC桩-土-垫层所组成的一个工作体系,考虑桩-土-垫层体系的工作特性及相互影响,对PCC桩进行分析提出了一种PCC桩复合地基模量计算方法,进而推导出PCC桩复合地基的桩土应力比、沉降简化计算公式。同时,运用工程实例进行验证。计算结果说明提出的解答是合理的,能够满足实际要求。     

路基荷载下PCC刚性桩复合地基沉降简化计算

将路堤荷载作用下的刚性桩复合地基变形,简化为只有竖向变形,水平变形可以忽略,然后,应用土体的平衡、几何、物理方程,建立沉降计算的控制方程。桩土界面的接触条件按位移协调或产生滑移变形两种情况分别建立,采用有限差分法离散求解,可得桩、桩周土各自的沉降变形、桩土界面的摩擦力分布。与有限元分析和现场实测结果的对比表明,该简化方法具有较高的准确性,可以方便地应用到工程实际。     

Separation Technology of the World’s Only Chambersite Deposit Has Achieved A Big Breakthrough

<正>Chambersite is a rare mineral worldwide,a manganese chloride borate(Mn3B7O13Cl),which was first discovered in the recovered brine from a salt dome at Chambers,Texas,USA.This rare mineral has been proven to have a great utilization value in anti-nuclear radiation,hightemperature friction materials,medicine and stealth materials,and can be used in aerospace and     

How Depth is the Tibetan Chromite: Experimental Study

<正>Podiform chromitites are generally lenticular bodies of massive to disseminated chromite typically hosted in mantle peridotites in ophiolites.Most such chromitites are surrounded by envelopes of dunite,a few centimeters to a few meters wide.Based on their textures and compositions,podiform chromitites have been interpreted     

Introduction to “Metallogenesis of Continental Collision”

<正>There is a general consensus that Plate Tectonics can explain metallogenesis based on the collisions between oceanic and continental crust.For instance,the large-sized porphyry copper deposits that occur along the Cordillera of the Andes around the east coast of the Pacific,and in the Phillipines,Malaysia and Indonesia along the western coast of the Pacific that sit upon the massive Pacific plates.They are considered to be typical of deposits resulting from collision between the oceanic and continental crust.Many experts,however,have long held a negative view about whether the collision between     

China First Discovered Massive Available Hot Dry Rock Resources

<正>Hot Dry Rock(HDR)refers to those generally deeply buried impermeable metamorphic or crystallized biotite gneiss,granite and granodiorite rock bodies,with a burial depth greater than 2000 m,containing no water or vapor.HDR is as implied,hot and dry,with temperatures ranging from 150 to 650℃,and it can be utilized as a heat     

Super-Large Pb-Zn Deposits Discovered in Danaopo, Huayuan County, Hunan Province

<正>Geological Brigade 405 of Hunan Provincial Geology and Mineral Exploration and Development Bureau discovered the Danaopo and Yangjiazhai super-large PbZn deposits through 5 years(2009–2014)of exploration in Huayuan County,Hunan Province.These deposits contain208.4942 million tons of(332+333)class Pb+Zn ores and4.8746 million tons of metal amounts,of which metal amounts of 333 class zinc are 4.1198 million tons and metal amounts of lead are 0.7548 million tons,associated with useful components of Cd,Ag and Se.In addition,the Limei,Qingshuitang and Yutang Pb-Zn deposits were     

海温及海浪对台风眼墙中尺度涡的影响

本文利用包括海气耦合、气浪耦合及浪流耦合的完全耦合系统,着重研究了2006年“格美”(Kaemi)台风眼墙内的中尺度涡结构。中尺度涡作为影响台风眼墙非对称结构的内部因子,与风垂直切变密切相关,其发展过程受台风下垫面海洋状况的影响。在顺切变右侧,垂直气流逐渐增强,在顺切变左侧达到最大后逐渐减弱。当不考虑海表温度的冷涌反馈作用时,海气间的热通量输送较大,由此引起眼墙内的中尺度对流加强,但集中爆发区仍然位于顺切变方向,不受热通量输送变化的影响。当不考虑海浪对海表粗糙度的影响时,在较小的海表粗糙度条件下,眼墙非对称性减弱,使得中尺度对流涡在切向方向上的分布较为均匀。     

一次强对流天气及其中短时强降水的成因分析

利用常规地面、高空观测资料,自动站资料,NCEP再分析资料,多普勒雷达资料和WRF模式模拟资料等,对2009年6月初晋豫鲁皖苏5省的一次强对流天气及其中短时强降水的形成原因进行了分析。结果表明:本次过程是在高空东北冷涡不断引导冷空气南下,与低层低涡扰动形成冷暖空气汇合的有利天气形势下发生的。边界层内的强烈辐合抬升是触发对流发生和释放对流不稳定能量的主要原因之一。高空有明显的干侵入并叠加在低层高假相当位温的暖湿空气之上,这种较强的位势不稳定形势对本次过程中对流系统的触发提供了有利的条件。对流系统移动方向一侧有较强的风暴相对螺旋度,通过低层辐合上升气流的倾斜作用,使更多的水平涡度转化为垂直涡度,为本次过程的发展、维持以及其短时强降水的发生提供了有利的条件。