嗜酸乳杆菌亚油酸异构酶的结构与催化机理

对嗜酸乳杆菌亚油酸异构酶基因及其启动子进行了定位,采用多种软件分析了酶蛋白中α螺旋、β折叠等二级结构的组成以及酶蛋白中的糖基化位点、磷酸化位点的分布.证明了该蛋白具有肌凝蛋白交叉反应抗原、链状球菌的67 000肌凝蛋白交叉反应抗原、番茄红素脱氢酶相关蛋白和FAD结合蛋白等4个功能结构域,并首次提出其催化共轭亚油酸合成时可能存在氧化还原反应过程.     

甘肃小柳沟含矿隐伏花岗岩稀土元素地球化学特征

小柳沟W,Mo多金属矿床为复控型矿床,矿区内隐伏花岗岩属复式岩体,REE分布模式表明小柳沟隐伏复式岩体具有明显成因联系或同源演化特点,属同源岩浆岩,δEu强亏损与弱δCe亏损,REE分布型式为富集LREE的右倾式折线,LREE的分异程度明显高于HREE.早期花岗岩REE分布模式一致性好,w(La)N/w(Yb)N值大(远大于10),δEu强亏损为特征,是有利的成矿母岩;晚期花岗岩以REE分布模式一致性较差,LREE分异好而HREE分异差为特征,w(La)N/w(Yb)N值小(远小于10),δEu较强亏损为特征.晚期岩浆进一步分异,成矿物质在岩体中进一步富集、迁移、活化形成石英脉型W,Mo矿,寻找花岗岩型Mo矿应在晚期小岩体中寻找.     

基于Hoek-Brown准则的深部岩体力学参数及其应用

基于Hoek-Brown经验强度准则,采用最小二乘法拟合出岩体力学强度参数,并与H-B_02ed推荐的等面积拟合结果进行对比,结果发现两种拟合方法得出的岩体内摩擦角数值相差很小,但等面积拟合法得出的黏聚力强度远高于最小二乘拟合法。将两种强度参数拟合结果应用于深部矿体开采的数值模拟,发现采用最小二乘拟合法的岩体强度参数其模拟结果更接近工程实际。该方法对深部岩体力学参数的确定具有一定的借鉴意义。     

Electrical conductivity changes of bulk tin and Sn-3.0Ag-0.5Cu in bulk and in joints during isothermal aging

The changes of electrical conductivity(resistance) between Sn-3.0Ag-0.5Cu solder joints and printed circuit board(PCB) assembly during aging at 125℃were investigated by the four-point probe technique.The microstructural characterizations of interfacial layers between the solder matrix and the substrate were examined by optical microscopy and scanning electronic microscopy.Different types of specimens were designed to consider several factors.The experimental results indicate that electrical conductivitie...     

路基边坡面力学试验参数处理方法研究

介绍了半填半挖路基挖填交接面的形式分类以及相应的变形破坏形式,同时提出采用随机-模糊统计法处理路基稳定性。半挖半填式路基是高速公路施工中一种常见的修筑方式,其稳定性的好坏取决于挖填交接面的形式及其岩体力学性质。表明了模糊统计处理方法优于传统的随机处理方法,通过工程应用实例表明该方法可靠合理,具有广泛推广的价值。     

Failure mode and strength anisotropic characteristic of stratified rock mass under uniaxial compressive situation

A stratified rock mass model was founded by FLAC^3D. The failure mode and anisotropic characteristic of strength for stratified rock mass were analyzed. The analysis results show that the numerical simulation can visually reflect the failure modes of rock samples under different inclination angles β of structural plane. The stiffness of rock sample before peak strength changes in the compressive procedure. With the increase of β, the compressive strength σ _c of rock sample decreases firstly and then increases; when β is in the range of 20°–30° and 80°–90°, σ _c has the largest sensitivity to β; while β falls in the range of 30°–70°, σ _c varies little. When ϕ _j <β<90° (β _j is friction angle of structure plane), the results obtained from numerical simulation and theoretical analysis are in almost the same values; while β⩽ ϕ _j or β=90°, they are in great different values. The results obtained from theoretical analysis are obvious larger than those from numerical simulation; and the results from numerical simulation can reflect the difference of compressive strength of rock samples for the two situations of β⩾ ϕ _j and β=90°, which is in more accordance with the real situation. Foundation item: Project (50099620) supported by the National Natural Science Foundation of China     

Comprehensive assessment on dynamic roof instability under fractured rock mass conditions in the excavation disturbed zone

The damage process of fractured rock mass showed that the fracture in rocks induced roof collapse in Yangchangwan Coal Mine,China.The rock mass was particularly weak and fractured.There occurred 6 large-scale dynamical roof falls in the excavation disturbed zone (EDZ) with the collapsing volume of 216 m3.First,the field detailed geological environment,regional seismic dy-namics,and dynamic instability of roadways were generally investigated.Second,the field multiple-index monitoring measurements for detecting the deep delamination of the roof,convergence deformation,bolt-cable load,acoustic emission (AE) characteristic pa-rameters,total AE events,AE energy-releasing rate,rock mass fracture,and damage were arranged.Finally,according to the time-space-strength relations,a quantitative assessment of the influence of rock-mass damage on the dynamic roof instability was accomplished.     

恒定水头岩体混凝土裂纹水入浸过程分析

针对自然营造力作用下岩体或混凝土裂纹的水力劈裂特点,基于裂纹水流运动的立方定律建立了恒定水头作用下裂纹内水流入浸过程计算模型与迭代步骤.通过对不同裂纹张开宽度、裂纹表面起伏差、裂纹形状等因素变化,分别计算了水流入浸过程.计算结果表明,裂纹内水流入浸过程是先快后慢,随着时间的推移,裂纹内水压会发展为全水头.当裂纹张开宽度大于0.02 mm,水流入浸过程及其短暂,裂纹内水流很快就达到裂尖,而且水压基本就是全水头.当裂纹的张开宽度特别小,达到微米级,水流就很难进入,即产生不透水的现象.裂纹表面的起伏差对于裂纹张开宽度较小的裂纹影响程度要大于宽度较大的裂纹.     

震后裂缝危岩体诊断技术研究

震后山体结构破碎,崩塌频发,严重的制约着灾后重建工作。为此,从震后岩体实际结构状况出发,在分析诱发岩体崩塌的破坏性外力类型的基础上,借助断裂力学理论,通过合理建模,阐明了震后岩体崩塌的机理,给出了崩塌发生的条件,为震区可预知余震强度区的危岩体诊断和排查提供了技术支持。最后通过算例及分析表明：余震、降雨及其相互耦合作用是震后崩塌的根本动力;在特定外力下区内岩体裂缝发生扩展存在最小临界深度;外力耦合条件下裂缝失稳临界深度最小     

震后裂缝危岩体的失稳机理与诊断方法

震后山体结构破碎,崩塌频发,严重制约着灾后重建工作.从震后岩体实际结构状况出发,在分析诱发岩体崩塌的破坏性外力类型的基础上,借助断裂力学理论,通过合理建模,阐明了震后岩体崩塌的机理,给出了崩塌发生的条件,为町预知余震强度震区的危岩体诊断和排查提供了技术支持.最后通过算例分析表明:余震、降雨及其相互耦合作用是震后崩塌的根本动力;在特定外力下区内岩体裂缝发生扩展存在最小临界深度;外力耦合条件下裂缝失稳临界深度最小.