露天矿运输道路生态型抑尘因子的选择

根据露天矿汽车运输土质路面特征及扬尘的发生机理,从环境本底条件出发,建立了黏结凝并、吸湿、保水等抑尘因子的选择原则.对蔗糖、可溶性淀粉、丙三醇、碳酸钠、硅酸钠等因子进行了粘度、吸湿、高温抗蒸发及研磨抗辗压等实验模拟研究,并与纯水进行了对比.结果表明,由可溶性淀粉、硅酸钠和丙三醇组成的抑尘剂,粘度可达510 mPa·s,粉尘的饱和吸剂率达到65.3%,恒高温(45℃)下单位面积的抗蒸发速率为0.03g·cm-2·h-1,抗蒸发时间达65.17h,具有强的黏结、凝并、吸湿、保水、抗高温和固结路面等性能,而且吸附性强,不产生喷洒时的二次扬尘,对矿石加工与冶炼无任何副作用,环境友好.     

用信息聚类方法研究蛋白质的氨基酸组成和二级结构含量的关系

从蛋白质的氨基酸组成出发，用信息聚类方法给出了蛋白质的聚类树状图，发现树状图的分支与蛋白质二级结构的含量有较强的相关性．     

钝体回流区二次风掺混实验研究

针对装有钝体燃烧器的燃煤粉锅炉，就其二次风对一次风喷口内回流区的掺混影响进行了一系列冷态实验研究．结果表明，二次风对回流区的影响主要表现在：限制了大空间卷吸进来的质量，加强了一次风内回流作用，使一次风主流轴线向内弯曲，使回流区缩短，同时对回流区尾部产生一定的掺混影响．这些影响的强弱程度与喷口间的相对距离和二次风的流速有关．研究结果将对实际煤粉锅炉一、二次风喷口距离和一次风量的选择有一定参考价值．     

工艺氩精制的模拟计算

用改进的Ｓｏａｖｅ状态方程作为数学模型，首次对工艺氩的精制流程进行计算，即用收敛单元法对高纯氩工艺流程进行模拟计算，并对精氩塔用设计型算法进行精馏计算，计算结果令人满意，为工艺氮精制优化设计提供了可靠的技术依据。     

用超塑性预处理原理细化低碳钢晶粒的研究

利用超塑性预处理细化晶粒原理 ,在低碳钢中加入不同体积分数的第二相粒子ZrC和ZrO2 ,研究了ZrC和ZrO2 粒子体积分数及轧后不同冷却方式对低碳钢组织和力学性能的影响。研究结果表明 ,轧制变形量为 84 %时 ,加入 0 .8%的ZrC粒子 ,采用轧后水冷方式可获得超细组织 ,晶粒尺寸可达到 9.8μm ;加入 0 .2 %的ZrO2 粒子时 ,晶粒尺寸可达 7.8μm。轧后水冷比轧后空冷方式能获得更为细小的晶粒     

Genetic mechanism and prediction of Paleozoic clastic eureservoirs in platform of Tarim Basin

Based on the pore cast and cathodolumines-cence thin sections, diagenesis process, source rock matura-tion history, structural evolution and reservoir qualitycharacteristics, the points of view that the porosities of Pa-leozoic clastic eureservoirs in the platform of the Tarim Ba-sin are mainly secondary, and the dissolution plays anunignorable role in the formation of eureservoirs, are putforward. In this paper, a series of criteria for the recognitionof the secondary porosities, the occurrence extent and classi-fication of secondary porosity are introduced, and threekinds of dissolution mechanism—the aluminosilicate dis-solution, the silicon dioxide dissolution and the carbonatedissolution—to generate the secondary porosity are comeup with. The formation, distribution, preservation and dis-appearance of eureservoirs are controlled by the paleo-structural framework and evolution, and hydrocarbon fillingand discharging. Paleostructural framework manipulate themigration path and direction of the acid fluid so as to deter-mine the position and extent of the dissolution. Paleostruc-ture highs and continuous paleouplifts are in favor of devel-oping the secondary porosity. The hydrocarbon filling madethe secondary porosities preserved and the hydrocarbondischarging let the secondary porosities filled by later calciteor quartz overgrowth cements. Paleostructure highs andcontinuous paleouplifts during the maturation period ofCambrian, Ordovician and Carboniferous source rocks(corresponding to S, P and K) are main areas for eureservoirs developing.     

微量元素对CuZnAl形状记忆合金晶粒细化和晶粒生长的影响

研究了添加 Ｚｒ，Ｔｉ，Ｂ和 Ｆｅ元素，对 ＣｕＡｎＡｌ形状记忆合金晶粒细化和 晶粒生长的影响；探讨了合金晶粒细化与晶粒生长的机制。试验结果表明：合 金中添加Ｚｒ，Ｔｉ，Ｂ，Ｆｅ元素，晶粒得到显著细化，晶粒生长受到抑制；晶粒 生长受到抑制最大的添加元素为 Ｚｒ，其余顺序为 Ｂ，Ｔｉ，Ｆｅ；添加 Ｚｒ，Ｔｉ的 合金，在９００℃上发生异常晶粒长大现象，这是由于晶界结构的变化，固溶 Ｚｒ，Ｔｉ原子对晶界的作用在高温时削弱及第二相粒子的溶解。添加 Ｂ的合 金，当ＣＢ＜０．０１（ｗｔ％）时，晶粒尺寸随含Ｂ量增多急剧减小；当ｃＢ＞０．０１ （Ｗｔ％）时，晶粒尺寸变化不大，该合金晶粒细化主要是固溶于基体中的硼的 作用。     

Raman spectroscopy study of zinc finger ZNF191（243-368）

The structure of ZNF191(243-368), the zinc finger region protein of zinc finger protein ZNF191, and its structural change upon thermal and EDTA-induced denaturation were investigated by the Raman spectroscopy. It was demonstrated that the coordination between Zn^2 and His/Cys in ZNF191(243-368) is the essential factor to the stability of zinc finger, which plays an important role in maintaining the hydrophobic core and the secondary structure in zinc finger, and the Raman spectroscopy is a powerful tool for investigating the structure of ZNF191(243-368).