滑坡体三维构造及稳定性分析

采用体元技术建立滑坡体真三维模型,通过基本三棱柱体构建具有复杂曲面结构的空间组合体,每个单元都赋予不同的属性,为滑坡体三维稳定性分析提供基本的前、后处理功能.以此为基础,并结合三维极限平衡分析计算方法,开发了相关的滑坡三维模拟与稳定性分析软件,并成功应用于清江库岸大型滑坡的三维仿真计算.     

海洋沉积物中的天然气水合物与海底滑坡

天然气水合物是一种由天然气和水形成的类似冰状的固体物质 ,主要存在于在低温高压背景下的海底沉积物和陆地永久冻土地带中。赋存于海底沉积物中的天然气水合物虽然本身能作为准稳定的胶结物对海底有建造作用 ,但由于其稳定性对特定温度和压力的严格依赖 ,海平面的下降、海底的连续沉积、地震等自然因素以及海洋钻探等人为因素造成的海底温压条件的改变会引起其分解 ,从而使海底沉积物失稳甚至导致海底滑坡。本文详细介绍了海底天然气水合物分解导致滑坡的机制、实例以及该种海底滑坡体的特征 ,并对以后的研究进行了展望     

Kalman最优平滑器在滑坡位移监测数据处理中的应用

针对传统方法中利用Kalman滤波器来处理物体的形变数据存在精度低的缺点,依据Kalman平滑比滤波的精度要高的原理,提出了将滑坡形变的估计问题视为Kalman平滑问题,而不仅仅是Kalman滤波问题;利用Kalman最优平滑器来处理滑坡位移监测数据,可使滑坡预测预报的精度得到较大提高,并在此基础上给出了一种固定区间平滑算法;最后,以龙羊峡龙西滑坡为例进行了实例分析,结果表明本文提出的方法是可行和有效的。此外,结论中针对实际运用中存在的问题提出了相应的建议。     

基于集对模型的地下工程塌方风险分析方法

为度量和监控地下工程塌方风险态势,提出一种基于集对模型的地下工程塌方风险分析方法。通过归纳地下工程塌方灾害因素,建立地下工程塌方风险的层次化结构,应用变异系数法确定风险指标的权重值;以集对分析(SPA)的同异反联系度和距离测度为基础,构建地下工程塌方风险态势监控机制及分析模型。给出地下工程塌方风险态势度量工作步骤,确定地下工程塌方灾害风险集对势、贴近度和次序关系。最后,通过对塌方风险分析样本的集对计算,为有效防范塌方灾害由潜伏性向灾变性转化提供防范重点。     

Influence of vacuum degree on the effect of gas explosion suppression by vacuum chamber

In order to study the influence of vacuum degree on gas explosion suppression by vacuum chamber, this study used the 0.2 mm thick polytetrafluoroethylene film as the diaphragm of vacuum chamber to carry out a series of experiments of gas explosion suppression by vacuum chamber with the vacuum degree from −0.01 MPa to −0.08 MPa. The experimental results show that: under the condition of any vacuum degree, vacuum chamber can effectively suppress the explosion flame and overpressure; as vacuum degree changes, the effect of gas explosion suppression using vacuum chamber is slightly different. Vacuum chamber has obvious influence on propagation characteristics of the explosion flame. After explosion flame passes by vacuum chamber, the flame signal weakens, the flame thickness becomes thicker, and the flame speed slows down. With the increase of the vacuum degree of vacuum chamber, the flame speed can be prevented from rising early by vacuum chamber. The higher the vacuum degree is, the more obviously the vacuum chamber attenuates the explosion overpressure, the smaller the average overpressure is, and the better effect of the gas explosion suppression is. Vacuum chamber can effectively weaken the explosion impulse under each vacuum degree. From the beginning of −0.01 MPa, the vacuum chamber can gradually weaken explosion impulse as the vacuum degree increases, and the effect of gas explosion suppression gradually becomes better. When the vacuum degree is greater than −0.04 MPa, the increase of vacuum degree can make the explosion overpressure decrease but have little influence on the explosion impulse. Therefore, the vacuum chamber has the preferable suppression effect with equal to or greater than −0.04 MPa vacuum degree.     

陕西省黄土崩塌隐患区宅基地选址方案研究

在对黄土崩塌所造成的伤亡、损失及灾害成因的调查的基础上,结合对黄土地形地貌、颗粒结构、岩土特征和力学特性的研究分析,提出了在黄土高原区内黄土崩塌隐患区居民宅基选址应注意的问题,变被动防灾为主动预防,这对地处黄土高原区山西、陕西、甘肃等省的居民宅基选址具有重要的指导意义和参考价值。     

陕西彬县百子沟滑坡预报的尝试

通过野外调查、形变监测,宏观前兆分析,对百子沟矿区滑坡蠕变规律和运动过程作了较全面的论述。为黄土高源滑坡、矿区滑坡临滑预报做出了范例。     

WIND GENERATED WAVES IN LAKE OKEECHOBEE1

ABSTRACT: The study of wind generated waves is important because waves affect sediment resuspension in lakes. Measurements of wind velocity and wave elevation were made at three different stations in Lake Okeechobee. Significant wave heights were computed using a direct count from the recorded data, and verified by the root-mean-square value approach. The correlation between wind stress and significant wave height also was analyzed. The data revealed a strong correlation. In addition to field measurements, a Boussinesq-type wind-wave model was developed to simulate wind-generated, long-propagating waves. This model included the effects of wind stress and bottom viscous dissipation. Wave elevation and velocity field were evaluated numerically. A six-day simulation using 1996 wind data was conducted. Simulated significant wave heights were found to agree reasonably well with measured values. A predictive wind-wave model provides information about wind generated waves, which is used to compute bottom shear stresses required for sediment resuspension studies.     

离心脉冲静电除尘模型的除尘性能实验研究

介绍了一种直筒式离心脉冲静电除尘器，研究了其除尘效率与入口风速，直流基础电压，入口粉尘浓度等操作因素的关系；测定了在不同入口风速，不同供电情况下除尘器的分级效率，结果表明，离心脉冲静电除尘器具有结构简单，阻力损失低，除尘效率高等优点；脉冲供电能显著提高除尘器的分级效率。对粒径小于2μm的粉尘的捕集，入口风速为6.97m/s至12.79m/s时，脉并非中供电与直流供电相比，其分级效率提高10%-23%；与旋风相比，其分级效率提高37%-66%。     

What is the lesson from the unprecedented event over antarctica in 2002

Varotsos (2002a,b), suggested that both the smaller-sized ozone hole over Antarctica and its splitting in two holes in September 2002 occurred due to an unprecedented major sudden stratospheric warming caused by very strong planetary waves propagated in the southern hemisphere. Subsequently, a NASA press release of December 6, 2002, also reported the prevalence of very strong planetary waves in Antarctica. The aim of this Letter is to further discuss the morphology of the Antarctic ozone hole, to detect the causes that allowed the Antarctic stratosphere to exhibit this exceptional warming and to examine what it denotes about its mechanisms. Concerning the morphology, among the principal findings is that the ozone hole split occurred not only in the stratosphere but extended in the lower altitudes (upper troposphere). As to the causes of the major sudden stratospheric warming of 2002, a comparison with the previous warmings in Antarctica since 1964 is made. The smaller-sized Antarctic ozone hole of 2002 is approximately equal to that of 1988 when a strong sudden stratospheric warming occurred. If only the destruction of ozone by chlorofluorocarbons resulted in the delayed sudden stratospheric warmings in Antarctica, then the early sudden stratospheric warmings of 1988 and 2002 would not have occurred, since chlorofluorocarbon loading of the stratosphere has remained relatively stable in recent years. Furthermore, it appears that the El Nino characteristics in 1988 and 2002 are not similar.