城市固体废弃物大直径三轴压缩试验研究

参照杭州天子岭填埋场城市固体废弃物（MSW）的主要成分，人工配制MSW试样，利用大型三轴剪力仪进行固结排水剪试验，研究MSW的剪切强度特性．由于MSW内部孔隙很大，导致固结过程中体变量非常大，固结时的体变与轴向应变基本成直线关系；当轴向应变达到15％时，剪切强度还在继续增长，MSW的应力应变关系表现为加工硬化型．破坏应变取值不同，MSW的强度参数c和φ差别很大．通过对比发现，现场静力触探试验得到的强度参数与室内大三轴试验破坏应变取为10％时得到的强度参数c和φ比较接近．     

火山灰沉积地区钻孔泥浆性能试验

水敏性火山灰沉积岩具有很强的吸水性和膨胀性,遇水后迅速软化崩解,钻孔施工时使用普通泥浆很难成孔。通过分析泥浆护壁性状,认为减少失水量和泥皮厚度是在水敏性土中成孔和提高桩侧摩擦阻力的关键。选取羧甲基纤维素(CMC)和纯碱(Na2CO3)作为减小失水量的添加剂,通过正交试验确定泥浆的最佳质量配比为:淡水∶膨润土∶CMC∶纯碱=100∶8∶0.1∶0.04。试验结果表明:膨润土质量分数越大,泥皮越厚,护壁效果越好,对桩侧摩擦阻力的消弱越大;CMC和纯碱对减少失水量和泥皮厚度效果明显;海水入浸会增加泥浆的失水量,造成泥浆恶化;铬铁木质素磺酸钠盐(FCL)对因海水入浸而恶化的泥浆改善效果不明显。     

固定化双菌串联发酵生产1，3-丙二醇

以葡萄糖为底物，利用分别固定化的酵母Candida krusei ICM-Y-05和肺炎杆菌Klebsiella pneumoniae ZJU 5205串联发酵生产1,3-丙二醇。实验结果表明，由C.krusei发酵而得粗甘油只需经简单离心后即可被K.pneumoniae所利用。将C.krusei包埋于NaCS/PDMDAAC生物微胶囊中，并于气升式反应器中发酵，所得发酵液直接流入固定床反应器，同时向固定床反应器补充微量元素，发酵培养经NaCS/PDMDAAC生物微胶囊包埋的K.pneumoniae，产物即为1,3-丙二醇。三批次发酵实验结果表明，1,3-丙二醇/葡萄糖的最终摩尔转化率为0.295。     

基于动态计量经济学模型的房地产周期研究

为正确判断房地产发展趋势,以动态计量经济学模型为基础,科学地识别并预测房地产市场周期。采用北京1989—2004年的时间序列数据,将先验经济理论与数据统计分析结合,建立自回归分布滞后的ARM AX模型。对变量进行单整ADF检验和多重协整JJ检验,求出误差修正序列。用包含误差修正项的模型来预测市场周期,弥补中国房地产市场广泛存在的非理性因素影响和统计数据的缺陷。研究表明:北京房地产市场的周期约为4~5 a;2005年的房地产市场正处于扩展阶段;2006年北京房地产市场仍将呈现稳步上升的态势。     

纺织服装院校物流人才培养绩效社会评价指标体系的构建

本文通过比较人才培养的传统评价模式和绩效评价模式，提出了以企业和竞争为标准的社会评价方式，并结合纺织服装院校专业特色，以此为基础构建了物流人才绩效社会评价指标体系，并利用模糊综合评价方法实现纺织服装物流人才培养绩效分析。     

E&AMode: 一种新的基于引擎粒子系统的图像渲染模式

本文分析了图像引擎粒子系统的传统实现方法的优劣，提出了一种称为发射源&影响者(E&AMode)的图像渲染模式，该模式实现了粒子系统模拟效果的多样性，粒子运动状态的动态性和结构设计的灵活性.本文介绍了新模式的基本结构、算法思想和实现方法.试验结果表明，发射源&影响者模式能够实现粒子属性的灵活设置，粒子运动状态的动态改变和模拟效果的多样性.     

Embryonic development and organogenesis of Chinese giant salamander, Andrias davidianus

The morphology and organogenesis of Chinese giant salamander, Andrias davidianus, in its different developmental periods and stages are described in detail, which provides an intact criterion for distinguishing different stages of its developmental process. Based on the external morphological and internal histological features, six periods including 20 stages of organogenesis of Chinese giant salamander are established, which are cleavage period, blastula period, gastrula period, neurula period, organogenesis stage and hatching stage. Generally, the embryonic development of Chinese giant salamander is consistent with those of Eastern newt, Cynops orientalis, and Black spots frog, R. nigromaculata. However, they have some differences in the early cleavage process and the development of digestive system. The cleavage of Chinese giant salamander, A. davidianus is not a discoidal division type, which is different from other species reported. And the first three cleavages being meridional and a retardant development of its digestive system without halter and sucker existing are the evident features of the embryonic development of Chinese giant salamander.     

Test of magnetic susceptibility and grain-size age models of loess

Ages of the stratigraphic boundary MIS1/2 and MIS3/4 of the Yuanbu loess section in Linxia are used as the basis of the nodal control age. The age of MIS1/2 and MIS3/4 are obtained from the latest international research result—the climatic events recorded in the stalagmite in the Hulu Cave in Nanjing, that MIS1/2 is 11.5 kaB.P. and MIS3/4 is 59.8 kaB.P.. The ages of the two climatic events contain three nodal age control models (Model 1: 0 kaB.P.—59.8 kaB.P.; Model 2: 0 kaB.P.—11.5 kaB.P. and 11.5 kaB.P.—59.8 kaB.P.; Model 3: 11.5 kaB.P.—59.8 kaB.P.), which are used as the nodal control age separately. The deposition times of various stratigraphic horizons are calculated by using the magnetic susceptibility age model and grain-size age model, and then compared with each other. In addition, the AMS14C age, OSL age and the ages of YD and H events are compared with the ages of the corresponding horizons calculated by the three models of nodal control ages. From the analyses of lithologic characters and climatic stages it has been found that both the magnetic susceptibility age model and the grain-size age model have some defects. Because the accurate control ages are selected as the nodal points of the glacial period or interglacial period, the stratigraphic deposition times determined by the high resolution of magnetic susceptibility age model and grain-size age model approximate to the actual ages. As for the relative accuracy of the two age models, the magnetic susceptibility age model is more accurate than the grain-size age model.     

降低密封催化消解法器械系统误差的方法

阐明了用密封催化消解法测量水样时可能带来系统误差的器械原因:当消解管生产加工的精度不高时会带来系统误差.分析了可能产生的误差大小,探讨了降低误差的方法.     

Test of magnetic susceptibility and grain-size age models of loess

Ages of the stratigraphic boundary MIS1/2 and MIS3/4 of the Yuanbu loess section in Linxia are used as the basis of the nodal control age. The age of MIS1/2 and MIS3/4 are obtained from the latest international research result—the climatic events recorded in the stalagmite in the Hulu Cave in Nanjing, that MIS1/2 is 11.5 kaB.P. and MIS3/4 is 59.8 kaB.P.. The ages of the two climatic events contain three nodal age control models (Model 1: 0 kaB.P.—59.8 kaB.P.; Model 2: 0 kaB.P.—11.5 kaB.P. and 11.5 kaB.P.—59.8 kaB.P.; Model 3: 11.5 kaB.P.—59.8 kaB.P.), which are used as the nodal control age separately. The deposition times of various stratigraphic horizons are calculated by using the magnetic susceptibility age model and grain-size age model, and then compared with each other. In addition, the AMS14C age, OSL age and the ages of YD and H events are compared with the ages of the corresponding horizons calculated by the three models of nodal control ages. From the analyses of lithologic characters and climatic stages it has been found that both the magnetic susceptibility age model and the grain-size age model have some defects. Because the accurate control ages are selected as the nodal points of the glacial period or interglacial period, the stratigraphic deposition times determined by the high resolution of magnetic susceptibility age model and grain-size age model approximate to the actual ages. As for the relative accuracy of the two age models, the magnetic susceptibility age model is more accurate than the grain-size age model.