Fe3Al合金的高温变形行为

用载荷松弛法对Ｆｅ－２８Ａｌ－２Ｔｉ合金在较高温度下的变形行为进行了研究．测定了Ｆｅ－２８Ａｌ－２Ｔｉ合金在高温变形时的载荷松弛曲线、应力减小因子Ｙ及激活能值,并对试样进行了显微结构观察．结果表明,Ｆｅ－２８Ａｌ－２Ｔｉ合金的高温变形是一个亚晶界吸收位错,而且不断向大角晶界转变的过程．     

考虑空洞演化效应的金属超塑性变形理论

根据金属超塑性变形时一般出现严重空洞化的特点,对金属板料超塑性变形时的屈服准则、空洞长大模型、材料损伤动力学方程、起塑性极科的受拉（包括双向受拉）失稳过程和先稳时的成形极限计算方法,起塑性极科成形极限图的预测以及自由胀形和充模胀形等具体起塑成形工艺考虑空洞演化效应的工艺计算与分析等问题进行了系统全面的研究．从而形成了考虑空洞演化效应的金属起塑性变形理论体系。对考虑空洞演化效应的金属起塑性变形理论中的基本问题作了扼要介绍。     

Thermal Deformation Measurement and Stress Analysis of PQFP Assembly during Power Cycling

ＴｈｅｒｍａｌＤｅｆｏｒｍａｔｉｏｎＭｅａｓｕｒｅｍｅｎｔａｎｄＳｔｒｅｓｓＡｎａｌｙｓｉｓｏｆＰＱＦＰＡｓｅｍｂｌｙｄｕｒｉｎｇＰｏｗｅｒＣｙｃｌｉｎｇＤａｉＦｕｌｏｎｇ（戴福隆）,ＳｈｉＬｉｎｇ（石玲）,ＷｅｎＸｉｕｍｅｉ（温秀梅）Ｄｅｐａｒｔｍ...     

复合采动影响下地表变形预测与危险区划分方法

矿山岩体工程开挖将改变原岩应力状态,由此引起岩体本身及周围一定区域的移动和变形,地下与露天复合开采的矿山更是如此,其变形速率之大、范围之广、时间之长已严重地影响周边环境的安全。通过对地下与露天复合采动影响下地表变形规律进行研究,建立了相应的移动模型。在此基础上,对移动参数的计算方法及地面变形区的划分方法等问题进行了研究。然后,依据当前形量和后续变形量大小,对矿山继续开采可能产生的破坏范围进行了划分     

水库二维水流泥沙数学模型及应用

建立水库坝区平面二维水流泥沙数学模型,考虑了悬移质非均匀,非饱和输沙特性,采用正交曲线坐标拟合复杂边界、ＳＩＭＰＬＥＣ程式离散求解及动边界技术。用该模型对白沙水库流场和河床变形进行了数值验证,计算了典型年条件下,水库取水口附近流场和河床局部形态。结果表明,坝前取水口漏斗基本保持稳定状态。     

膨胀土的浸水规律

根据土体浸水速率（导水库）与土体结构的理论关系和膨胀土结构的分形模型,导出了膨胀土的浸水速率与含水量,吸力、时间和上覆荷载的相关关系。理论和试验结果表明：膨胀土的浸水速率与含水量、吸力和时间在双对数坐标上呈直线相关,随着含水量增加、吸力减小,浸水速率增大、浸水速率随时间延长而减小;浸水速率的对数与上覆荷载呈直线相关,上覆荷载越大,浸水速率越小。     

冲击波作用下粉末颗粒效应及其形成过程

采用两种颗粒尺寸相差悬珠的高速钢粉末进行爆炸烧结机制的研究,发现了明显的“颗粒效应”,烧结过程首先在小颗粒变形量最大的尖角处发生熔化,在冲击波作用下使液体流激烈运动,加速了颗粒的熔化,最后使颗粒相互粘结在一起,达到烧结的目的。     

STUDY ON THE DUCTILE DEFORMATION DOMAIN OF THE SIMPLE SHEAR IN ROCKS——TAKING BRITTLE FAULTS OF THE COVERING STRATA IN THE SOUTHERN JIANGSU AREA AS AN EXAMPLE

A study on the ductile deformation domain of the brittle fault in the shallow level ofthe crust is a new probe field for the modern structural geology. Taking the southern Jiang-su Province area as an example the orientation measurement of quartz crystals, the com-positional texture observation of three pressure sensitive minerals and the rheological param-eter determination of dislocation densities, etc. have been demonstrated and analysed basedon typical samples in the present paper. In addition, their generation mechanisms arealso discussed from the cataclastic rheology, the dynamic differentiation and the simpleshearing, specially, from the Ode strength theory. Finally, a generative relationship betweenthe ductile deformation domain of the brittle fault system, in the regional layer--slip andthe formation of the stratabound ore deposit is shown as well.     

Molecular structure of ethynylbenzene from electron diffraction and ab initio molecular orbital calculations

The molecular structure and benzene ring distortions of ethynylbenzene have been investigated by gas-phase electron diffraction and ab initio MO calculations at the HF/6-31G^* and 6-3G^** levels. Least-squares refinement of a model withC _2v, symmetry, with constraints from the MO calculations, yielded the following important bond distances and angles:r _g(C _i -C _o )=1.407±0.003 Å,r _g(C _o -C _m )=1.397±0.003 Å,r _g(C _m -C _p )=1.400±0.003 Å,r _g(Cr _i -CCH)=1.436 ±0.004 Å,r _g(C=C)=1.205±0.005 Å, C _o -C _i -C _o =119.8±0.4°. The deformation of the benzene ring of ethynylbenzene given by the MO calculations, including o-C_i-C_o=119.4°, is insensitive to the basis set used and agrees with that obtained by low-temperature X-ray crystallography for the phenylethynyl fragment, C₆H₅-CC-, in two different crystal environments. The partial substitution structure of ethynylbenzene from microwave spectroscopy is shown to be inaccurate in the ipso region of the benzene ring.     

Plastic deformation kinetics for glassy polymers and blends

Measurements of the plastic deformation kinetics for several glassy (PS, PC, PI-polyimide, PET, epoxy-amine network), semi crystalline polymers (PBT, PET) and blends (ABS, PC:ABS, PC: PBT) were performed for the unidirectional compression loading conditions by using constant temperature deformation calorimetry. The experiments have permitted us to follow the changes of the mechanical work (A), the heat of deformation (Q) and differences between these quantities, i.e., internal energy (U) stored in samples during their loading and unloading. Experiments have shown that the large portion (45–85%) of the mechanical work of deformation (A) is converted to heat (Q). The rest ofA is converted to internal energy (U) stored in deformed samples. U is quite high as compared with metals [1,2]. After complete unloading of plastically deformed samples, i.e., samples carrying irreversible atT _def plastic deformation ( _irr ), some amount (U) of stored energy disappeared. The amount of (U and (U) are different for different polymers. All data are analyzed in the framework of the model proposed in [3,4]. The experiments support the deformation model where the plasticity of glassy polymers is the process of nucleation and development of so-called PDs-plastic local shear defects of nonconformational and nondilatational nature.Dedicated to Prof. Dr. W. Pechhold on the occasion of his 60th birthday