降雨条件下考虑非饱和渗流的黄土滑坡灾变分析

采用滤纸法测试,并根据SWCC理论模型Van Genuchten方程拟合,得到非饱和土-水特征曲线,同时根据Van Genuchten统计传导模型估计渗透系数曲线.针对降雨诱发型黄土滑坡,建立边坡二维分析模型,以Mohr-Coulomb准则作为滑坡破坏依据,以非饱和土渗流理论为依托,进行渗流分析和稳定性分析.通过分析降雨不同持时坡体内部孔隙水压力的变化规律,揭示降雨入渗机理.结果表明,随降雨时长增加,滑坡土体由非饱和状态向饱和状态过渡,坡体孔隙水压力不断增加,水位线不断向上抬升.稳定性分析结果表明,降雨持续时间越长,滑坡稳定系数越低,降雨开始前滑坡稳定系数为1.005,滑坡处于蠕动变形阶段,与现状滑坡体上裂缝发生发展相符合;雨强120 mm/d持续降雨48 h时稳定系数为0.978,滑坡为不稳定状态;降雨持续2.5 h时,滑坡由欠稳定状态转为不稳定状态,由蠕动变形阶段进入滑动阶段,反映了滑坡稳定状态对降雨极为敏感.     

不饱和类卡宾H_2C＝CNaX(X=F,Cl,Br)的密度泛函理论研究

采用密度泛函理论方法,在B3LYP/6-311+G(d,p)水平上研究了不饱和类卡宾H2C=CNa X(X=F,Cl,Br)的结构.结果表明,不饱和类卡宾H2C=CNa X(X=F,Cl,Br)各有2种平衡构型,其中具有三元环结构的构型能量低,是其存在的主要构型.预言了最稳定构型的振动频率和红外强度.计算得到了最稳定构型分子内氢迁移反应的过渡态.讨论了卤原子对不饱和类卡宾H2C=CNa X的影响.     

高陡横坡段桩柱式桥梁双桩基础受力分析

基于高陡横坡段桩柱式桥梁双桩基础承载特性,提出了一种改进有限杆单元计算分析方法.分析了高陡横坡段桩柱式桥梁双桩基础承载机理及受力特性,建立了双桩基础计算分析模型.其次,根据前、后桩与边坡相对位置关系,给出了后桩所受剩余下滑力与前桩所受土压力的比例关系.在传统有限杆单元分析方法基础上,结合陡坡桩受力特征,导得了考虑桩土共同作用与"P-Δ"效应的单元刚度矩阵修正方法,并在此基础上编制了适用于高陡横坡段桩柱式桥梁双桩基础的有限杆单元分析MATLAB计算程序.采用室内模型试验对本文计算方法进行验证,给出了适用于陡坡段桥梁桩基的设计流程图.研究结果表明:本文理论计算值与模型试验实测结果吻合良好,表明本文计算方法正确可行,可为同类工程设计提供参考.     

一个包含Smarandache Ceil函数的对偶函数的方程

利用初等方法研究了一个包含Smarandache Ceil函数Sk(n)的对偶函数-Sk(n),给出了当k=6时方程-S6(1)+-S6(2)+…+-S6(n)=6Ω(n)的具体正整数解。     

疏松砂岩油藏大孔道定性识别新方法研究

疏松砂岩油藏在长期注水开发过程中,往往伴随着大孔道的出现,这严重影响了油藏水驱开发效果,制约了采出程度的进一步提高,因此,大孔道识别及有效封堵成为该类油藏急需解决的关键问题.通过研究分析,确定了影响大孔道从形成到发展的7种主要静态因素,以及标志大孔道形成的6种主要动态因素.将层次分析法及灰色关联法相结合,分别计算静态及动态因素的权重,建立了全新的大孔道定性识别模型.示踪剂监测结果验证了该方法的实用性和有效性.     

Crystallization of Poly(ethylene adipate) within γ-Phase Poly(vinylidene fluoride) Matrix

The effects of PEA on the γ-phase PVDF crystal structure and the crystallization of PEA within the pre-existing γ-phase PVDF spherulites have been investigated by optical microscopy(OM), infrared spectroscopy(IR) and scanning electron microscopy(SEM). The results demonstrate that the γ-phase PVDF spherulites consist of the lamellae exhibiting a highly curved scroll-like morphology and develop preferentially in PEA-rich blend. With increasing PEA concentration, the scroll diameter increases and the scrolls are better separated from each other. PEA crystallizes first in the interspherulitic region and transcrystalline layer develops. Subsequently, the transcrystalline layer of PEA continues to grow within the γ-phase PVDF spherulites, e.g., in the region between the scrolls, until impinging on other PEA transcrystalline layers or spherulites. The crystallization kinetics results indicate that the growth rate of PEA crystals in the intraspherulitic region of γ-phase PVDF shows a positive correlation with content of PEA, but a negative one with the crystallization temperature of γ-phase PVDF.     

(2+1)维KD方程组的一类非亚纯行波解

通过行波变换将(2+1)维KD方程组转变为复域中的常微分方程,给出复合的(2+1)维KD方程组2(wk-3l2+3ak2 C1)u=2k4 u″-k2 a2 u3+(6k2b-3kal)u2+C2,v=lku+C1的一类非亚纯解的结构.     

Mass and isotopic concentrations of water-insoluble refractory carbon in total suspended particulates at Mt.Waliguan Observatory(China)

Mass concentration and isotopic values δ¹³C and ¹⁴C are presented for the water-insoluble refractory carbon（WIRC） component of total suspended particulates（TSP）,collected weekly during 2003,as well as from October 2005 to May 2006 at the WMO-GAW Mt.Waliguan（WLG） site.The overall average WIRC mass concentration was（1183±120）ng/m³（n = 79）,while seasonal averages were 2081 ±1707（spring）,454±205（summer）,650±411（autumn）,and 1019±703（winter） ng/m3.Seasonal variations in WIRC mass concentrations were consistent with black carbon measurements from an aethalometer,although WIRC concentrations were typically higher,especially in winter and spring.The δ¹³C PDB value（-25.3 ± 0.8）%.determined for WIRC suggests that its sources are C₃ biomass or fossil fuel combustion.No seasonal change in δ¹³C PDB was evident.The average percent Modern Carbon（pMC） for ¹⁴C in WIRC for winter and spring was（67.2 ± 7.7）%（n = 29）.Lower pMC values were associated with air masses transported from the area east of WLG,while higher pMC values were associated with air masses from the Tibetan Plateau,southwest of WLG.Elevated pMC values with abnormally high mass concentrations of TSP and WIRC were measured during a dust storm event.